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Claims for the world’s deepest earthquake challenged by new analysis

seismogram

The magnitude 7.9 Bonin Islands earthquake sequence, which ruptured deep within the earth near the base of the upper mantle, did not include an aftershock that extended to record depths into the lower mantle, according to a study in The Seismic Record.

When Hao Zhang of the University of Southern California and colleagues re-examined the aftershock sequence of the May 2015 earthquake, they did not find evidence for a 751-kilometer-deep aftershock as reported by previous researchers. This aftershock has been called the deepest earthquake ever recorded.

Instead, their study found a distribution of aftershocks that is compatible with a 12-kilometer sliver of a mantle mineral called olivine that could shed light on how deep earthquakes can occur.

The Bonin Islands earthquake, which ruptured 1000 kilometers offshore of Japan in a remote part of the Pacific Ocean, is one of the deepest and largest earthquakes ever recorded. The earthquake took place within the Izu-Bonin subduction zone 680 kilometers below the Earth’s surface.

The mechanisms behind deep earthquakes — those occurring 500 kilometers or deeper — are something of a mystery to seismologists. Extremely high pressures and temperatures at these depths make rock more likely to bend or deform plastically, rather than break in the brittle fashion that causes earthquake rupture at shallower depths.

These earthquakes also typically produce few aftershocks, Zhang noted, which could provide useful data to understand how these deep events are generated at subduction zones.

Plastic deformation “limits the formation of extensive fracture networks that would typically generate aftershocks,” he said. “Additionally, the high confining pressures promote efficient redistribution of stress following the mainshock, further reducing the likelihood of subsequent seismic events.”

One previous study of the Bonin Islands earthquake reported a foreshock sequence for the event, while a second study detected a potentially record-breaking deep aftershock in the lower mantle.

“Both findings could significantly advance our understanding of deep earthquakes, if accurate,” said Zhang. “However, these two catalogs are inconsistent, and both have methodological limitations. Therefore, it is essential to re-examine the aftershock sequence using improved techniques.”

To gain a better look at the deep and remote earthquake, Zhang and colleagues turned to data collected by a dense seismic array in Japan called Hi-Net, using a combination of techniques to precisely locate seismic signals coming from the event.

Their new analysis detected no foreshocks but identified 14 aftershocks in the upper mantle within a 150-kilometer radius of the earthquake’s hypocenter. One set of aftershocks aligned with the rupture plane of the earthquake one week after the mainshock, with a second set dispersing over a wider area during the second week.

“While it remains challenging to definitely reject the existence of seismicity initiated in the lower mantle and its associated mechanisms, our results do reject the most compelling lower mantle seismicity claim to date,” the researchers write in their paper.

The aftershock pattern is compatible with the presence of a metastable olivine wedge or MOW, the researchers suggested. In a subducting slab, olivine can delay its transition into other mineral states under high temperature and pressure. “This delayed transformation may generate stress and release energy, potentially triggering deep earthquakes,” Zhang said.

With MOWs as potential earthquake nucleation sites, some researchers have proposed this mechanism of transformational faulting as one of the main ways that deep earthquakes occur, he added.

“Furthermore, MOWs offer insights into the thermal structure and behavior of subducting slabs, with colder slabs being more likely to preserve metastable olivine at greater depths,” Zhang added. “By studying MOWs, we can refine models of deep earthquake generation and improve our understanding of the dynamic processes in Earth’s interior.”

Reference:
Hao Zhang, John E. Vidale, Wei Wang. Aftershocks on the Planar Rupture Surface of the Deep-Focus Mw 7.9 Bonin Islands Earthquake. The Seismic Record, 2025; 5 (1): 35 DOI: 10.1785/0320240035

Note: The above post is reprinted from materials provided by Seismological Society of America.

Eclogite Folds in Nordfjord, Norway: A Geomorphological Perspective

Eclogite Folds in Nordfjord, Norway: A Geomorphological Perspective
Eclogite Folds in Nordfjord, Norway: A Geomorphological Perspective

Introduction to Eclogite Folds in Nordfjord

Eclogite is a dense, mafic metamorphic rock characterized by a striking assemblage of red garnet (pyrope) and green clinopyroxene (omphacite). Its formation occurs under high-pressure and moderate-temperature conditions, typically exceeding 1.2 GPa and ranging between 400–600°C, corresponding to depths greater than 40 kilometers within subduction zones. The Nordfjord region in western Norway is renowned for its well-preserved eclogite exposures, particularly those exhibiting intricate folding patterns. These eclogite folds offer valuable insights into the tectonometamorphic history of the Scandinavian Caledonides and the dynamic processes that have shaped the Earth’s lithosphere.


Geological Formation of Eclogite

Eclogite forms through the metamorphism of basaltic rocks subjected to high-pressure conditions, typically within subduction zones where oceanic crust is forced deep into the mantle. The protoliths of eclogite are often mid-ocean ridge basalts (MORB) or similar mafic compositions. During subduction, these rocks undergo significant mineralogical transformations:

  • Plagioclase transforms into omphacite (a sodium-rich clinopyroxene).
  • Pyroxenes and amphiboles recrystallize into garnet (almandine-pyrope series).

This metamorphic process results in the distinctive mineralogy and high density of eclogite, which plays a crucial role in geodynamic processes such as slab pull during subduction.


Tectonic History of the Nordfjord Region

The Nordfjord area is part of the Western Gneiss Region (WGR) of Norway, which experienced significant tectonometamorphic events during the Caledonian orogeny (~490–390 million years ago). This orogeny resulted from the collision between the Laurentian and Baltican continents, leading to the closure of the Iapetus Ocean. The intense compressional forces during this period caused deep subduction of continental and oceanic crust, facilitating the formation of high-pressure and ultrahigh-pressure metamorphic rocks, including eclogite. Subsequent extensional tectonics and exhumation processes brought these deep-seated rocks back to the surface, where they are now exposed in regions like Nordfjord.


Structural Characteristics of Eclogite Folds

In Nordfjord, eclogite bodies often display complex folding patterns indicative of the intense deformation they have undergone. These folds vary in scale from microscopic to several meters and exhibit diverse geometries, including:

  • Isoclinal folds: Tight folds with parallel limbs.
  • Chevron folds: Characterized by sharp hinges and straight limbs.
  • Recumbent folds: Folds with horizontal axial planes, suggesting significant horizontal compressive forces.

The study of these folds provides insights into the deformation mechanisms, rheological properties of the rocks, and the stress regimes during metamorphism.

Metamorphic Conditions and Facies

Eclogite formation occurs under high-pressure (HP) and ultrahigh-pressure (UHP) conditions, with pressures exceeding 1.2 GPa (equivalent to depths greater than 40 km) and temperatures ranging from 400–800°C. In Nordfjord, eclogite facies metamorphism is a direct result of the deep subduction of the Baltican crust during the Caledonian orogeny.

Key Metamorphic Facies in Nordfjord:

  • Eclogite Facies: Defined by garnet + omphacite + kyanite mineral assemblages.
  • Granulite Facies: Represents the transition to lower-pressure, high-temperature conditions during exhumation.
  • Amphibolite Facies: Marks retrograde metamorphism as the rocks returned to shallower crustal levels.

Petrological studies of eclogites in Nordfjord suggest that these rocks were subjected to pressures as high as 3.0 GPa (equivalent to ~100 km depth) before being rapidly exhumed.


Petrography and Mineralogy of Nordfjord Eclogites

Nordfjord’s eclogites are characterized by their distinctive mineralogy, which provides valuable information on their pressure-temperature (P-T) history.

Primary Minerals in Eclogite:

  • Garnet (Almandine-Pyrope Series): Forms large, well-developed crystals with inclusion-rich cores.
  • Omphacite (Clinopyroxene): A Na-rich pyroxene, crucial for defining eclogite facies.
  • Kyanite: An indicator of high-pressure metamorphism.
  • Coesite: Found in ultrahigh-pressure (UHP) eclogites, indicating deep burial.

Retrograde Minerals (Lower Pressure Phases):

  • Amphibole (e.g., hornblende) forms during decompression.
  • Plagioclase replaces omphacite as pressure decreases.
  • Chlorite and Epidote are common signs of hydrothermal alteration.

The mineralogy of these eclogites provides crucial evidence of subduction zone processes and crustal recycling in deep Earth environments.


Geochronology and Age Determination of Eclogite Folds

To understand the timing and duration of eclogite metamorphism, geologists use various radiometric dating techniques:

Key Dating Methods:

  • U-Pb Dating on Zircon & Monazite: Provides precise ages of peak metamorphism.
  • Lu-Hf and Sm-Nd Isotopic Systems: Used to date garnet growth and determine the duration of high-pressure metamorphism.
  • Ar-Ar Dating on Micas: Useful for dating retrogression and exhumation.

Age of Eclogite Metamorphism in Nordfjord:

  • Peak eclogite metamorphism: 430–400 Ma (Caledonian orogeny).
  • Exhumation to crustal levels: 390–370 Ma.
  • Final cooling below ~300°C: 350 Ma.

These dates align with the subduction and exhumation cycles of the Baltican continental crust during the closure of the Iapetus Ocean.


Exhumation Processes of High-Pressure Rocks

One of the most intriguing geological questions is: How do eclogites, formed at depths of ~100 km, return to the surface?

In Nordfjord, exhumation occurred through a combination of:

  1. Tectonic Uplift: Driven by buoyancy forces acting on subducted crust.
  2. Extensional Faulting: Linked to the Nordfjord-Sogn Detachment Zone (NSDZ), a major low-angle normal fault that facilitated crustal thinning.
  3. Erosion and Surface Denudation: Helped expose high-pressure rocks at Earth’s surface.

The Nordfjord-Sogn Detachment Zone played a key role in the exhumation of high-pressure metamorphic rocks, allowing geologists to study deep crustal processes in an accessible field setting.


Field Studies and Mapping of Eclogite Folds

Nordfjord is one of the best locations worldwide for studying eclogite folds in situ. Field geologists utilize structural mapping, petrography, and geochemical analysis to understand fold dynamics.

Key Localities for Eclogite Folds in Nordfjord:

  • Stadtlandet Peninsula: Displays spectacular recumbent folds in eclogite-bearing gneisses.
  • Hornelen Basin: Features large-scale synclinal and anticlinal folds in high-pressure rocks.
  • Western Gneiss Region: Contains some of the largest and best-preserved eclogite bodies in the world.

These field exposures provide natural laboratories for studying deep-crustal processes and tectonic evolution.


Geochemical Signatures and Provenance

Geochemical studies of eclogites in Nordfjord help determine their protolith origin and tectonic history.

Key Geochemical Techniques Used:

  • Major & Trace Element Analysis: Determines the original rock composition.
  • Isotopic Studies (Sr-Nd-Pb-Hf): Traces the sources of eclogite-forming material.
  • Rare Earth Element (REE) Patterns: Distinguishes between oceanic and continental sources.

Results indicate that Nordfjord eclogites were originally mafic rocks derived from an oceanic crustal setting, later subducted and metamorphosed during the Caledonian orogeny.


Comparison with Other Eclogite-Bearing Terranes

The Nordfjord eclogite folds are part of a global network of high-pressure terranes. Comparing them to other regions helps geologists understand subduction-exhumation processes worldwide.

Comparison with Other Eclogite Occurrences:

Region Tectonic Setting Key Features
Nordfjord, Norway Caledonian Orogeny Large-scale eclogite folds, extensive UHP metamorphism
Western Alps, France-Italy Alpine Orogeny UHP eclogites with coesite and diamond inclusions
Dabie-Sulu, China Triassic Orogeny World’s largest UHP terrane, with deep subduction evidence
Franciscan Complex, USA Subduction Zone Eclogite blocks in a mélange setting

These comparisons show that Nordfjord is unique due to its large-scale fold structures and strong association with extensional detachment faults.


Economic and Industrial Significance of Eclogite

Although not a major economic resource, eclogite has several industrial applications:

  • Crushed rock for road construction (due to its hardness and durability).
  • Dimension stone in decorative applications.
  • Source of garnet for use as an abrasive material.

Additionally, the study of eclogite-hosted mineral deposits can provide insights into deep-seated ore-forming processes.


Environmental and Geohazard Considerations

Eclogite-bearing terrains can present geohazards due to their brittle deformation history. Some key concerns in Nordfjord include:

  • Rockslides and Slope Instabilities: Due to the presence of highly deformed rocks.
  • Seismic Activity: Associated with past and present fault movements.

Proper geological assessments are crucial for land use planning and infrastructure development in these regions.


Conservation and Educational Value

Nordfjord’s eclogite folds serve as natural geological archives that should be preserved for scientific research and education. Universities and research institutions frequently conduct field excursions to these sites, allowing students and professionals to study high-pressure metamorphism in a real-world setting.


Future Research Directions in Nordfjord Eclogite Studies

Emerging techniques such as AI-based mineral mapping, high-resolution geochemical analysis, and geodynamic modeling are expected to revolutionize our understanding of eclogite formation and exhumation.

Future research may focus on:

  • The role of fluids in metamorphic reactions.
  • The kinematics of eclogite folding using 3D structural analysis.
  • Deep-Earth drilling to study eclogite-hosted mineral deposits.

The Velodrome Recumbent Fold

The Velodrome Recumbent Fold
The Velodrome Recumbent Fold

Introduction to The Velodrome Recumbent Fold

The Velodrome Recumbent Fold is a remarkable geological structure that exemplifies the extreme forces acting within the Earth’s crust. It is classified as a recumbent fold, meaning that its axial plane is nearly horizontal, causing its limbs to lie parallel to each other. Such folds are crucial in understanding compressional tectonic environments, where intense horizontal stress deforms rock layers over geological time scales.

This article explores the formation, structure, significance, and implications of the Velodrome Recumbent Fold, providing insights into its role in Earth’s tectonic history and resource potential.


What is a Recumbent Fold?

A recumbent fold is a specific type of fold where the axial plane is nearly horizontal, and the limbs are overturned to an extreme degree. This structure forms under intense compressional forces, which cause rock layers to deform plastically rather than fracturing.

Key Features of Recumbent Folds:

  • Axial Plane: Nearly horizontal
  • Fold Limbs: Overturned and lying subparallel
  • Formation Process: Result of prolonged compression and shearing forces
  • Common Location: Found in mountain belts and regions of strong tectonic deformation

Recumbent folds are often associated with thrust faulting and nappe structures, where large rock masses are displaced over long distances due to tectonic movement.


The Geological Context of The Velodrome Recumbent Fold

The Velodrome Recumbent Fold is situated in a highly deformed tectonic region, characterized by compressional stress and crustal thickening. The surrounding geology suggests that this fold developed during a major orogenic event, which involved the collision of tectonic plates.

Tectonic Setting:

  • Found in a convergent plate boundary where subduction and collision occurred.
  • Associated with high-pressure metamorphic rocks.
  • Frequently occurs within fold-and-thrust belts.

Structural Characteristics of The Velodrome Recumbent Fold

The Velodrome Recumbent Fold exhibits:

  • A horizontal axial plane, indicating extreme tectonic stress.
  • Highly deformed syncline and anticline structures.
  • A relationship with thrust faults, showing nappe formation.

Field observations and structural analysis reveal that this fold likely formed due to ductile deformation of sedimentary and metamorphic layers, which accommodated the intense pressure without fracturing.


Tectonic Forces Behind The Velodrome Recumbent Fold

The formation of this fold is attributed to:

  • Plate Convergence: Collision of tectonic plates led to intense crustal shortening.
  • Shear Stress: Lateral movements of crustal blocks contributed to its recumbent shape.
  • High-Temperature Deformation: Rocks underwent metamorphism, enhancing their ability to fold rather than break.

Dating and Age Determination

To determine the age of the Velodrome Recumbent Fold, geologists use:

  • Radiometric dating (U-Pb, Ar-Ar) on minerals such as zircon.
  • Fossil evidence within folded strata.
  • Relative dating techniques comparing cross-cutting relationships.

Results indicate that this fold formed during a significant orogenic event, correlating with major tectonic plate interactions.


Economic and Environmental Importance

The Velodrome Recumbent Fold holds geological significance due to:

  • Rich mineral deposits, including gold, copper, and rare earth elements.
  • Potential oil and gas reservoirs, trapped within its structural folds.
  • Environmental considerations, as regions with extreme folds can be prone to landslides and seismic activity.

Conclusion

The Velodrome Recumbent Fold serves as a testament to the powerful forces shaping our planet. Its intricate structure provides valuable insights into tectonics, resource distribution, and geological evolution. As new technologies emerge, further studies will enhance our understanding of such complex geological phenomena.


Frequently Asked Questions (FAQs)

  1. What causes a recumbent fold?
    • Extreme compressional forces cause rock layers to fold horizontally.
  2. Where are recumbent folds commonly found?
    • In orogenic belts, where tectonic collisions have deformed the crust.
  3. What is the significance of the Velodrome Recumbent Fold?
    • It provides insights into tectonic evolution and resource distribution.
  4. How do geologists study recumbent folds?
    • Using field mapping, seismic data, and petrographic analysis.
  5. Can recumbent folds lead to earthquakes?
    • Yes, especially if associated with thrust faults and active tectonic zones.
  6. Are recumbent folds important for mining?
    • Yes, as they often contain valuable ore deposits.

World’s oldest mammalian ancestor discovered in Mallorca

Reconstruction of the appearance in life of a gorgonopsian in a floodplain of the Permian of Mallorca. Credit: Henry Sutherland Sharpe
Reconstruction of the appearance in life of a gorgonopsian in a floodplain of the Permian of Mallorca. Credit: Henry Sutherland Sharpe

An international research team led by the Institut Català de Paleontologia Miquel Crusafont (ICP) and the Museu Balear de Ciències Naturals (MUCBO | MBCN) have described a fossil animal that lived between 270 and 280 million years ago in present-day Mallorca.

The discovery is exceptional, not only because of the number of fossil remains found, but also because it is the oldest known gorgonopsian on the planet, the lineage of saber-toothed predators that would eventually give rise to mammals. The research has been published in the journal Nature Communications.

Gorgonopsians are an extinct group of synapsids that lived during the Permian, between 270 and 250 million years ago. They belong to the evolutionary lineage that would give rise to the first mammals 50 million years later.

They were warm-blooded animals like modern mammals, but, unlike most of them, they laid eggs. They were carnivorous and were the first animals to develop the characteristic saber teeth. They were often the superpredators of the ecosystems in which they lived, and their appearance would be similar to a dog, but without ears or fur.

The remains recovered in Mallorca belong to a small to medium-sized animal, approximately one meter in length, and come from a site located in the municipality of Banyalbufar (Serra de Tramuntana, Mallorca). Excavations were carried out in three different campaigns during which a large quantity of material was recovered.

“The large number of bone remains is surprising. We have found everything from fragments of skull, vertebrae, and ribs to a very well-preserved femur. In fact, when we started this excavation, we never thought we would find so many remains of an animal of this type in Mallorca,” explains Rafel Matamales, curator of the Museu Balear de Ciències Naturals (MUCBO | MBCN), research associate at the ICP, and first author of the article.

Its location in the Balearic Islands is an unusual fact in itself. The known remains of gorgonopsians prior to this discovery belonged to very high latitudes such as Russia or South Africa. Its age has also surprised the researchers who conducted the study.

“It is most likely the oldest gorgonopsian on the planet. The one we found in Mallorca is at least 270 million years old, and the other records of this group worldwide are, at the very least, slightly younger,” points out Josep Fortuny, senior author of the article and head of the Computational Biomechanics and Evolution of Life History group at the Institut Català de Paleontologia Miquel Crusafont (ICP).

Among the excavated fossil remains, a nearly complete leg stands out, which has allowed researchers to study how the animal moved. Unlike reptiles, which have a more ancestral locomotion with their legs more spread out, gorgonopsians had their legs positioned more vertically and, therefore, moved in a way that was intermediate between reptiles and mammals. This system is more efficient for walking and especially for running.

The recovered saber teeth confirm its diet. “We know that this is a carnivorous animal, a characteristic shared by all gorgonopsians worldwide. The saber teeth are a common feature in large predators of ecosystems, and what we have found was likely one in the environment in which it lived,” emphasizes Àngel Galobart, researcher at the ICP and director of the Museu de la Conca Dellà.

When Mallorca was not an island

During the Permian, approximately 270 million years ago, Mallorca was not an island but was part of the supercontinent Pangea. It was located at an equatorial latitude, where countries like Congo or Guinea can be found today. The climate was monsoonal, alternating between wet and very dry seasons.

It has been found that the site where the fossils were found was a floodplain with temporary ponds where gorgonopsians and other fauna drank. Among the animals that cohabited in this ecosystem were moradisaurine captorhinids, an ancient group of herbivorous reptiles to which the Tramuntanasaurus tiai belongs, which may have been part of the gorgonopsians’ diet.

Despite the small area that they occupy, the Balearic Islands have an exceptional fossil record. The most studied and well-known fossils are from the Pleistocene and Holocene.

However, the fossil record from other periods is considerably less known. Nonetheless, remarkable fossils have been found, such as the world’s oldest mosquito, nearly a thousand species of ammonoids (cephalopods related to squids), ancestors of horses and hippos, giant sharks, and large coral reefs.

Reference:
Matamales-Andreu, R., et al. Early–middle Permian Mediterranean gorgonopsian suggests an equatorial origin of therapsids. Nature Communications. DOI: 10.1038/s41467-024-54425-5

Note: The above post is reprinted from materials provided by Miquel Crusafont Catalan Institute of Paleontology.

Mysterious plant fossil belongs to a family that no longer exists

An strange, extinct plant once thought to be related to modern ginseng is now considered the lone representative of an unknown family. Credit: Florida Museum of Natural History / Jeff Gage
An strange, extinct plant once thought to be related to modern ginseng is now considered the lone representative of an unknown family. Credit: Florida Museum of Natural History / Jeff Gage

In 1969, fossilized leaves of the species Othniophyton elongatum—which translates to “alien plant”—were identified in eastern Utah. Initially, scientists theorized the extinct species may have belonged to the ginseng family (Araliaceae). However, a case once closed is now being revisited. New fossil specimens show that Othniophyton elongatum is even stranger than scientists first thought.

Steven Manchester, curator of paleobotany at the Florida Museum of Natural History, has studied 47-million-year-old fossils from Utah for several years. While visiting the University of California, Berkeley, paleobotany collection, he came across an unidentified and unusually well-preserved plant fossil collected from the same area as the leaves of Othniophyton elongatum.

Manchester is the co-author of a new study in which he and his colleagues showed that the leaves in question belonged to a unique plant, with unusual flowers and fruits. The findings are published in the journal Annals of Botany.

Close observation revealed that the 1969 fossils and those later studied by Manchester at UC Berkeley were from the same plant species. But the leaves, fruits and flowers attached to the woody stem of the Berkeley fossils were nothing like those of the other plants in the ginseng family, to which that species had been originally assigned.

“This fossil is rare in having the twig with attached fruits and leaves. Usually those are found separately,” Manchester said.

The authors extensively analyzed physical features of the old and new fossils, then methodically searched for any living plant family to which they could belong. There are over 400 diverse families of flowering plants alive today, but the authors couldn’t match the fossils’ strange assortment of features with any of them.

Resisting the urge to tidily lump the obscure specimen in with a living group, the team then searched for extinct families it might have belonged to but came up empty-handed once again.

The authors say their results underscore what may be a pervasive problem in paleobotany. In many cases, extinct plants that existed less than 65 million years ago are placed within modern families, or genera—the taxonomic groups directly above the level of individual species. This can create a skewed estimate of biodiversity in ancient ecosystems.

“There are many things for which we have good evidence to put in a modern family or genus, but you can’t always shoehorn these things,” Manchester said.

The species does not belong to any living family or genus

The fossils were discovered in the Green River Formation near the ghost town of Rainbow in eastern Utah. Roughly 47 million years ago, the area was a tectonically active, massive inland lake system that provided the perfect conditions for fossil preservation. Low-oxygen lake sediments and showers of volcanic ash slowed the decomposition of many fish, reptiles, birds, invertebrates and plants, allowing some of them to be preserved in amazing detail.

Researchers who had studied the original leaf fossils of this species had very little to work with. Without flowers, fruits or branches, they were limited to analyzing the shape and vein patterns of the leaves. Based on the arrangement, researchers thought it might be a single leaf made up of multiple smaller leaflets. This type of compound leaf is a defining feature of several plants in the ginseng family.

But the new fossils had leaves that were directly attached to stems, which painted a very different picture of what the plant once looked like.

“The two twigs we found show the same kind of leaf attached, but they’re not compound. They’re simple, which eliminates the possibility of it being anything in that family,” Manchester said.

The fossil’s berries ruled out families like the grasses and magnolias. The flowers did resemble some modern groups, but other features ruled those out, too. Even with such a pristine fossil in their repertoire, researchers were left with more questions than before.

Researchers see the fossil in a new light

Stumped, the team set the fossil aside for several years. Then the Florida Museum hired a curator of artificial intelligence who established a new microscopy workstation. When viewed through the digital microscope’s powerful lens and computer-enhanced shadow effect illumination, the authors could see subtle peculiarities they’d missed during prior observations.

When they focused on the fossil’s minute fruits, they could see micro-impressions left behind by their internal anatomy, including features of the small, developing seeds.

“Normally we don’t expect to see that preserved in these types of fossils, but maybe we’ve been overlooking it because our equipment didn’t pick up that kind of topographic relief,” Manchester said.

One of the plant’s strangest newly seen features was its stamens, the male reproductive organs of the flower. In most plant species, once the flower is fertilized, the stamens detach along with petals and the rest of the flower parts, which are no longer needed for reproduction.

“Usually, stamens will fall away as the fruit develops. And this thing seems unusual in that it’s retaining the stamens at the time it has mature fruits with seeds ready to disperse. We haven’t seen that in anything modern,” Manchester said.

With all modern families ruled out, they compared the traits to extinct families. Once again, there was no match to be found.

Julian Correa-Narvaez, the lead author of the study and a doctoral student at the University of Florida, played a major role in gathering information to identify the fossils. “It’s important because it gives us a little bit of a clue about how these organisms were evolving and adapting in different places,” he said.

Plant families can contain astonishing amounts of diversity. Seemingly disparate plants like poison ivy, cashews and mangoes are all in the same family, along with over 800 other species. It’s unclear how much diversity in this mysterious extinct group has been lost to time.

This isn’t the only enigmatic species that has come out of the Green River Formation. Similar situations have unfolded when plant fossils from the locality surprised researchers, leading to the discovery of other extinct groups. “The book published in 1969 has all these interesting mysteries that remain,” Manchester said.

With digital access to museum specimens through tools like iDigBio, researchers can continue to study and understand the natural history of plant evolution.

Walter Judd of the Florida Museum of Natural History is also a co-author of the study.

Reference:
Steven R Manchester et al, Vegetative and reproductive morphology of Othniophyton elongatum (MacGinitie) gen. et comb. nov., an extinct angiosperm of possible caryophyllalean affinity from the Eocene of Colorado and Utah, USA, Annals of Botany (2024). DOI: 10.1093/aob/mcae196

Note: The above post is reprinted from materials provided by Florida Museum of Natural History

Insect fossil find ‘extremely rare’

A close-up of two tiny, whitefly puparia.
A close-up of two tiny, whitefly puparia.

Newly discovered insect fossils are so small they can barely be seen by the human eye but have been preserved in an “extraordinary” way.

Published in the journal Palaeobiodiversity and Palaeoenvironments, a new study reveals rare whitefly insect fossils have been found in Miocene age crater lake sediments at Hindon Maar, near Dunedin.

Adult whiteflies are tiny insects about 3mm in size, smaller if they are immature.

The fossils found at Hindon Maar are about 1.5mm by 1.25mm and have been preserved in the position they lived and died, attached to the underside of a fossil leaf.

Black with an oval-shaped body, they have some similarities to modern-day whiteflies — such as the shape and colour — but differ in that all the segments of the body are distinctly defined by deep sutures.

Co-author Dr Uwe Kaulfuss, of the University of Göttingen in Germany and former postdoctoral fellow in the University of Otago’s Department of Geology, discovered the tiny fossils during an excavation at Hindon earlier this year.

“Fossils of adult whitefly insects are not uncommon, but it takes extraordinary circumstances for the puparia — the protective shell the insect emerges from — to become fossilised,” Dr Kaulfuss says.

“Some 15 million years ago, the leaf with the puparia must have become detached from a tree, blown into the small lake and sank to the deep lake floor to be covered by sediment and become fossilised. It must have happened in rapid succession as the tiny insect fossils are exquisitely preserved.

“The new genus and species described in our study reveals for the first time that whitefly insects were an ecological component in ancient forests on the South Island.”

Study co-author Emeritus Professor Daphne Lee, of Otago’s Department of Geology, says they add to the expanding insect fauna revealed in the maar.

“It was difficult to see much with the naked eye but once the fossils were under a microscope, we could see the amazing detail,” she says.

“The fact that they are still in life position on the leaf is incredible and extremely rare. These little fossils are the first of their kind to be found in New Zealand and only the third example of such fossil puparia known globally.

“Until about 20 years ago, the total number of insects in the country older than the Ice Ages was seven and now we have 750. Almost all are housed in the Otago Geology Department collections.

“New discoveries such as these from fossil sites in Otago mean we’ve gone from knowing almost nothing about the role played by insects to a new appreciation of their importance in understanding New Zealand’s past biodiversity and the history of our forest ecosystems.”

Professor Lee says while most people are interested in big fossils — large charismatic ones — most animals in forests are insects.

“There are 14,000 insects in New Zealand and 90 per cent are found nowhere else in the world,” she says.

“Discovery of these minute fossils tells us this group of insects has been in Aotearoa New Zealand for at least 15 million years. This provides a well-dated calibration point for molecular phylogenetic studies.”

Other small fossils new to science have also been found at Otago sites this year, including the first dancefly, cranefly, phantom midge and marsh beetle fossils from New Zealand. These studies show the extent of Otago’s scientific collaborations around the world with co-authors of these papers coming from Germany, France, Spain, Poland and the USA.

Reference:

Jowita Drohojowska, Gregory A. Evans, Uwe Kaulfuss, Daphne E. Lee, Jacek Szwedo. First Miocene whiteflies and psyllids (Hemiptera: Sternorrhyncha: Aleyrodoidea and Psylloidea) from Aotearoa New Zealand. Palaeobiodiversity and Palaeoenvironments, 2024; DOI: 10.1007/s12549-024-00628-z

Note: The above post is reprinted from materials provided by University of Otago.

Chart of life extended by nearly 1.5 billion years

Geobiologist Shuhai Xiao (at left) and colleague in the field in Canada. Photo courtesy of Danielle Fitzgerald.
Geobiologist Shuhai Xiao (at left) and colleague in the field in Canada. Photo courtesy of Danielle Fitzgerald.

Ancient species may have evolved slower and lasted longer, but the pace of evolution accelerated after global ice ages, according to a new Virginia Tech analysis. The study, published in the journal Science, maps the rise and fall of ancient life many times older than the dinosaurs.

If all the world’s a stage and all the species merely players, then their exits and entrances can be found in the rock record.

Fossilized skeletons and shells clearly show how evolution and extinction unfolded over the past half a billion years, but anew Virginia Tech analysis extends the chart of life to nearly 2 billion years ago.

The chart shows the relative ups and downs in species counts, telling scientists about the origin, diversification, and extinction of ancient life.

With this new study, the chart of life now includes life forms from the Proterozoic Eon, 2,500 million to 539 million years ago. Proterozoic life was generally smaller and squishier — like sea sponges that didn’t develop mineral skeletons — and left fewer traces to fossilize in the first place.

Virginia Tech geobiologist Shuhai Xiao and collaborators published a high-resolution analysis of the global diversity of Proterozoic life based on a global compilation of fossil data, which was released Dec. 20 in the journal Science.

Xiao and his team looked specifically at records of ancient marine eukaryotes — organisms whose cells contain a nucleus. Early eukaryotes later evolved into the multicellular organisms credited for ushering in a whole new era for life on Earth, including animals, plants, and fungi.

“This is the most comprehensive and up-to-date analysis of this period to date,” said Xiao who recently was inducted into the National Academy of Sciences. “And more importantly, we’ve used a graphic correlation program that allowed us to achieve greater temporal resolution.”

The choreography of species offers critical insights into the parallel paths of the evolution of life and Earth.

Observed patterns and insights suggested by the analysis:

  • The first eukaryotes arose no later than 1.8 billion years ago and gradually evolved to a stable level of diversity from about 1,450 million to 720 million years ago, a period aptly known as the “boring billion,” when species turnover rates were remarkably low.
  • Eukaryotic species in the “boring billion” may have evolved slower and lasted longer than those came later.
  • Then cataclysm: Snowball Earth, a spiral of plunging temperatures, sealed the planet in ice at least twice between 720 million and 635 million years ago. When the ice eventually thawed, evolutionary activity picked up, and things weren’t so boring anymore.

“The ice ages were a major factor that reset the evolutionary path in terms of diversity and dynamics,” Xiao said. “We see rapid turnover of eukaryotic species immediately after glaciation. That’s a major finding.”

The patterns, Xiao said, raise a lot of interesting questions, including:

  • Why was eukaryotic evolution sluggish during the “boring billion”?
  • What factors contributed to the increased pace of evolution after snowball ice ages?
  • Was it environmental, such as climate changes and increases in atmospheric oxygen level?
  • Was it an evolutionary arms race between different organisms that could drive creatures to evolve quickly?

Future scientists can use the quantified pattern to answer these questions and better understand the complex interplay of life on Earth and the Earth itself.

Study collaborators include:

  • Qing Tang, first author, former graduate student and postdoctoral researcher, now at Nanjing University, as well as former graduate students Drew Muscente, now at Princeton Consultants, and Natalia Bykova, now at the University of Missouri, who worked in Xiao’s lab in the past decade
  • Researchers from the University of Hong Kong; University of California, Santa Barbara; Princeton Consultants; University of Missouri; Russian Academy of Sciences; University of California, Riverside; Chinese Academy of Sciences; and Northwest University (China)

Reference:
Qing Tang, Wentao Zheng, Shuhan Zhang, Junxuan Fan, Leigh Anne Riedman, Xudong Hou, A. D. Muscente, Natalia Bykova, Peter M. Sadler, Xiangdong Wang, Feifei Zhang, Xunlai Yuan, Chuanming Zhou, Bin Wan, Ke Pang, Qing Ouyang, N. Ryan McKenzie, Guochun Zhao, Shuzhong Shen, Shuhai Xiao. Quantifying the global biodiversity of Proterozoic eukaryotes. Science, 2024; 386 (6728) DOI: 10.1126/science.adm9137

Note: The above post is reprinted from materials provided by Virginia Tech. Original written by Kelly Izlar.

Researchers identify a mysterious fossil seed to reveal new chapters in climate history of Los Angeles

Fluorescent and scanning electron microscopy (SEM) of fossil and modern juniper leaves. (a, b) Fluorescent microscope imagery of fossil juniper branchlet (LACMHC 1469B). (b) Close-up of leaf scale with smooth leaf margins and acute-slightly obtuse apical shape. (c) SEM image of entire fossil leaf scale from adaxial (dorsal) perspective. (d–g) Close-up imagery of abaxial (ventral) side of modern (d) J. blancoi, (e) J. scopulorum, (f) J. virginiana, and (g) fossil juniper leaf (P23-47594).
Fluorescent and scanning electron microscopy (SEM) of fossil and modern juniper leaves. (a, b) Fluorescent microscope imagery of fossil juniper branchlet (LACMHC 1469B). (b) Close-up of leaf scale with smooth leaf margins and acute-slightly obtuse apical shape. (c) SEM image of entire fossil leaf scale from adaxial (dorsal) perspective. (d–g) Close-up imagery of abaxial (ventral) side of modern (d) J. blancoi, (e) J. scopulorum, (f) J. virginiana, and (g) fossil juniper leaf (P23-47594).

La Brea Tar Pits scientists have identified a previously unknown juniper species to the La Brea Tar Pits as Juniperus scopulorum, commonly known as the Rocky Mountain juniper. The successful identification, along with the first-ever radiocarbon dating of these fossil plants in Southern California, expands our ability to track past environmental changes and highlights the vulnerability of junipers and the environments they shape in the face of modern climate change. Published in the journal New Phytologist, the study unlocks a key finding to understanding the megafaunal extinction at the Tar Pits and better understanding our own climate future.

The mammoths and saber-toothed cats that shape our imagination of Ice Age Los Angeles browsed, grazed, and hunted in juniper woodlands. More than just a source of food for giant herbivores, junipers were keystone trees and shrubs in the region, in turn shaping the landscape for at least 47,000 years before completely vanishing from the region in the same extinction event that erased most of the megafauna.

Researchers have long known that there are two different species of juniper found at the Tar Pits — the large-seeded J. californica (California juniper), and the small-seeded, mystery juniper. With distinct tolerances for temperature and drought, fossil junipers play a crucial role in understanding the changing climate of the last Ice Age, and how junipers can survive our climate future, but the identity of the mystery seed remained uncertain — until now.

“We set out to identify this mystery juniper, and in the process, we found a number of exciting things,” says Dr. Jessie George, postdoctoral researcher at La Brea Tar Pits, and lead author on the study. “Number one, we identified this juniper as Rocky Mountain juniper, and it is one of the most extreme examples of a plant going extinct locally. It’s not present anywhere in California today.”

As part of the study, George and the other Tar Pits researchers radiocarbon dated the two species of juniper, which led to the second exciting finding: “In the process of radiocarbon dating these juniper species, we found this really interesting pattern of reciprocal presence — either California juniper only or Rocky Mountain juniper only.”

Because each plant survives in specific conditions, its presence acts as a proxy for climate. George and her colleagues found that this dance between the two junipers coincided with long periods of drought and warm, dry weather that would otherwise be hidden in the fossil record. “California juniper is a much more drought tolerant species. It withstands moisture deficit way better than Rocky Mountain juniper,” says George. “Through these back-and-forth occurrences of the two species from the Tar Pits, we have this really fascinating record of aridity and drought that was previously undetected.”

The small size of the unknown juniper seed — about as big as Lincoln’s forehead on a penny — made it a difficult subject, especially since DNA has yet to be extracted from Tar Pits fossils. Instead, George compared the structure of seeds and branchlets to other juniper species — the only way to uncover its identity. It required careful comparison using advanced microscopy, image analysis, and species distribution modeling (SDM) until the team reached a definitive answer.

While climate definitely played an important role in their local extinction, the team thinks that the abrupt disappearance of Ice Age megafauna and fires started by humans may have also contributed, much like in the case of those iconic giant mammals. In a hotter, drier climate, even plants well-adapted to drought couldn’t survive the extra stress of human fires. This is especially true for plants that are not adapted to wildfire-unlike many other conifer species, juniper has little tolerance for surviving or re-growing following fires. The finding highlights the threat junipers continue to face from human-caused climate change and could inform conservation efforts going forward.

“We’re seeing events of really dramatic decline of these trees in the southwest today because of warming temperatures and increased wildfire caused by modern climate change. So a direct record of how this might have occurred in the past, what factors were at play, and where those boundaries occurred is incredibly important,” says George. “It gives us a better framework to understand a baseline of climate and environment to contextualize changes in other plant life and the fauna that we see during these periods of significant change in the past. As our ability to precisely date fossils improves, better and more detailed information is revealed from ancient life at La Brea.”

“Identification of fossil juniper seeds from Rancho La Brea (California, USA): drought and extirpation in the Late Pleistocene” was authored by Jessie George, Monica Dimson, Regan E. Dunn, Emily L. Lindsey, Aisling B. Farrell, Brenda Paola Aguilar, Glen M. MacDonald and was published in New Phytologist on December 10, 2024.

Reference:
Jessie George, Monica Dimson, Regan E. Dunn, Emily L. Lindsey, Aisling B. Farrell, Brenda Paola Aguilar, Glen M. MacDonald. Identification of fossil juniper seeds from Rancho La Brea (California, USA): drought and extirpation in the Late Pleistocene. New Phytologist, 2024; DOI: 10.1111/nph.20324

Note: The above post is reprinted from materials provided by Natural History Museum of Los Angeles County.

A festive flying reptile family reunion 150 million years in the making

UV photography of Pterodactylus. Ultraviolet light reveals remarkable details of the fossil invisible under normal lighting. This famous specimen showcases preserved soft tissues, including the delicate wing membranes, which fluoresce vividly under UV illumination.
UV photography of Pterodactylus. Ultraviolet light reveals remarkable details of the fossil invisible under normal lighting. This famous specimen showcases preserved soft tissues, including the delicate wing membranes, which fluoresce vividly under UV illumination.

Christmas is the time for families to come together, and in the midst of the festive season University of Leicester paleontologists have announced that they have reunited a family that have been separated for 150 million years.

A new study published this week has found nearly 50 ‘hidden’ relatives of Pterodactylus, the first pterosaur, that will allow scientists to reconstruct this flying reptile’s life history from hatchling to adulthood.

Nearly 250 years ago, the very first pterosaur fossil was found in a quarry in northern Bavaria. Dubbed Pterodactylus, this 150-million-year-old fossil provided the first evidence for an extraordinary group of flying reptiles that filled the skies of the Mesozoic, soaring over the heads of dinosaurs on wings that could span up to 10 metres or more. While this first pterosaur was only the size of a turtle dove, it completely reshaped our understanding of prehistoric life.

Despite being the original ‘pterodactyl’, Pterodactylus was soon quite literally overshadowed in the public consciousness by more dramatic, giant pterosaurs like Pteranodon and Quetzalcoatlus, whichstole the spotlight. But Pterodactylus remained a favourite among pterosaur scientists.

Over the centuries, Pterodactylus and other similar pterosaurs from Bavaria have been central to ongoing scientific study, helping shape much of what we know about pterosaurs, from the shape of their wings and how they flew, to their diet and how they grew. But one question has always lingered: which of these many pterosaurs are truly Pterodactylus and which belong to completely different species? This confusion has persisted for centuries… until now. Thanks to a new study that analysed dozens of specimens of Pterodactylus in museums around the world, the mystery has been solved, and the true identity of these fossils has finally been uncovered.

Shining powerful UV torches on fossil bones to make them fluoresce, University of Leicester paleontologists Robert Smyth and Dr Dave Unwin were able to bring to light tiny near-invisible bony details that distinguish one kind of pterosaur from another. Using Pterodactylus’ unique features, found in the head, hips, hands and feet, Smyth and Unwin systematically checked other fossils from the same deposits and to their surprise discovered many other examples of Pterodactylus ‘hiding’ in among what were thought to be other species of pterosaur.

Lead author Robert Smyth, a doctoral researcher in the in the Centre for Palaeobiology and Biosphere Evolution (School of Geography, Geology and the Environment at the University of Leicester), explained: “By examining lots of fossils in collections across Europe we were able to reidentify more than forty specimens as Pterodactylus. UV stimulated fluorescence is astonishing in the amount of detail it can reveal. Features that were once hidden were glowing in plain sight.”

In an eyeblink the entire concept of Pterodactylus changed dramatically. With nearly 50 examples recognised so far, our knowledge of this most important of pterosaur has exploded. As co-author Dr David Unwin from the University of Leicester explained: “We can now construct a complete and highly detailed skeletal anatomy for this key pterosaur. Soft tissues are fossilised in more than twenty examples so we can also reconstruct head crests, body shape, foot webs and even the wings.”

The result? A sprawling family portrait of Pterodactylus, providing a unique opportunity to reconstruct its full life history. This spans from robin-sized hatchlings (affectionately dubbed ‘flaplings’) to ‘teenage’ Pterodactylus, all the way to raven-sized adults with wingspans nearly ten times larger.

Dr Unwin added: “UV stimulated fluorescence is a well-known technique, but the difference in this case is that we have been able to combine new high quality light sources with a systematic ‘catch-all’ approach, and it’s going to have a revolutionary impact on our understanding of pterosaurs.”

Reference:
Robert S. H. Smyth, David M. Unwin. Re-evaluation of Pterodactylus antiquus and Diopecephalus kochi two troublesome taxonomic concepts. Journal of Systematic Palaeontology, 2024; 22 (1) DOI: 10.1080/14772019.2024.2421845

Note: The above post is reprinted from materials provided by University of Leicester.

Denali Fault tore apart ancient joining of two landmasses

Monazite crystals from samples associate professor Sean Regan gathered in the Coast Mountains near Juneau. Images courtesy of Sean Regan
Monazite crystals from samples associate professor Sean Regan gathered in the Coast Mountains near Juneau. Images courtesy of Sean Regan

New research shows that three sites spread along an approximately 620-mile portion of today’s Denali Fault were once a smaller united geologic feature indicative of the final joining of two land masses. That feature was then torn apart by millions of years of tectonic activity.

The work, led by associate professor Sean Regan at the University of Alaska Fairbanks Geophysical Institute and UAF College of Natural Science and Mathematics, is featured on the cover of the December edition of Geology, the journal of The Geological Society of America.

Regan is the research paper’s lead author. UAF co-authors include doctoral student McKenzie Miller, recent master’s graduate Sean Marble and research assistant professor Florian Hofmann. Other co-authors are from St. Lawrence University, South Dakota School of Mines and Technology and the University of California, Santa Barbara.

“Our understanding of lithospheric growth, or plate growth, along the western margin in North America is becoming clearer, and a big part of that is related to reconstruction of strike-slip faults such as the Denali Fault,” Regan said. “We’re starting to recognize those primary features involved in the stitching, or the suturing, of once-distant land masses to the North American plate.”

The research focused on formations at three locations: the Clearwater Mountains of Southcentral Alaska, the Kluane Lake region of Canada’s southwestern Yukon, and the Coast Mountains near Juneau. Previous thinking among geologists is mixed, with some suggesting the three locations formed individually.

Regan’s historical reconstruction of 300 miles of horizontal movement on the Denali Fault over millions of years found that the three locations at one time formed a terminal suture zone. A terminal suture zone represents the final integration of tectonic plates or crustal fragments into a larger mass.

Regan’s work defines one of several places where the Wrangellia Composite Terrane, an oceanic plate that originated far from its current position, accreted to the western edge of North America between 72 million and 56 million years ago.

“When you think about geologists crawling around Earth’s surface trying to understand what the heck happened, it makes some sense that they might not link things that are so far apart,” Regan said of the three sites he studied. “With different geologists working in different areas, the dots don’t really get connected until you can reconstruct deformation on the Denali Fault.”

Regan’s reconstruction focused on the three sites’ inverted metamorphism, a geological phenomenon where rocks formed under higher temperatures and pressures are found overlying rocks formed under lower temperatures and pressures. This is the reverse of the typical sequence observed in regional metamorphism, where temperature and pressure generally increase with depth.

Inverted metamorphism is a key indicator of tectonic complexity and helps geologists reconstruct the processes of crustal deformation and mountain building.

“We showed that each of these three independent inverted metamorphic belts all formed at the same time under similar conditions,” Regan said. “And all occupy a very similar structural setting. Not only are they the same age, they all behaved in a similar fashion. They decrease in age, structurally, downward.”

Regan connected the three locations by analyzing their monazite, which consists of the rare earth elements lanthanum, cerium, neodymium and sometimes yttrium. He collected monazite from the two Alaska locations and used Kluane data published earlier in the year by another scientist.

“It is just the most special little mineral,” Regan said. “It can participate in a lot of reactions, so we can use it as a way to track the mineralogical evolution of a rock.”

Regan began his quest after reading a 1993 paper by researchers at the University of Alberta and University British Columbia and published in Geology. That paper asserted similarities in the Denali Fault region later studied by Regan, but only went as far as labeling them as a single metamorphic-plutonic belt.

A metamorphic-plutonic belt is a region characterized by the close association of metamorphic rocks and plutonic rocks that form as a result of intense tectonic activity, typically during mountain-building processes. These belts are commonly found in areas where tectonic plates converge.

“It was amazing to me that the 1993 paper hadn’t caught more attention back in the day,” Regan said. “I had this paper hung up on my wall for the last four years, because I thought it was really ahead of its time.”

Reference:
Sean P. Regan, Mark E. Holland, Trevor S. Waldien, McKenzie Miller, Peter Taylor, Andrew Kylander-Clark, Sean Marble, Florian Hofmann. Orogen-scale inverted metamorphism during Cretaceous–Paleogene terminal suturing along the North American Cordillera, Alaska, USA. Geology, 2024; 52 (12): 933 DOI: 10.1130/G52614.1

Note: The above post is reprinted from materials provided by University of Alaska Fairbanks. Original written by Rod Boyce.

Prehistoric rock in Japan reveals clues to major ocean anoxic event

Representative image: Hand holding a rock
Representative image: Hand holding a rock

By studying prehistoric rocks and fossils emerging from the side of Mount Ashibetsu in Japan, researchers have precisely refined the timing and duration of Ocean Anoxic Event 1a (OAE 1a), an extreme environmental disruption that choked oxygen from Earth’s oceans to cause significant extinction, especially among plankton.

Researchers have long suspected that massive volcanic eruptions undersea caused carbon dioxide (CO2) increases, global warming and depleted oxygen (called anoxia) in the ocean during the Mesozoic Period. Now, an international team of researchers, including Northwestern University Earth scientists, determined the precise timing of the volcanic eruption and OAE1a, which started 119.5 million years ago. The work adds to a growing volume of evidence that volcanic CO2 emissions directly triggered the anoxic event.

The new study also determined that OAE 1a lasted for just over 1.1 million years. This new information helps scientists better understand how the Earth’s climate and ocean system operates and responds to stress — especially as it relates to current warming.

The study was published late last month in the journal Science Advances. It marks the most detailed and highly resolved dating of an ocean anoxic event ever achieved.

“Ocean anoxic events occur in part as a consequence of climatic warming in a greenhouse world,” said Northwestern’s Brad Sageman, a senior author of the study. “If we want to make accurate predictions about what we will see in the decades ahead with human-caused warming, this information is invaluable. The best way to understand the future is to look at data from the past.”

An expert on ancient climates, Sageman is a professor of Earth, Environmental and Planetary Sciences at Northwestern’s Weinberg College of Arts and Sciences and a co-director of the Paula M. Trienens Institute for Sustainability and Energy.

A Northwestern connection

The Cretaceous Period experienced two major and several minor ocean anoxic events, with OAE 1a as one of the two largest. The most likely cause: volcanic eruptions rapidly injected massive amounts of CO2 into the ocean and atmosphere. These aren’t ordinary volcanoes but large igneous provinces that erupt up to a million cubic kilometers of basalt over several millions of years. When CO2 reacts with seawater, it forms a weak carbonic acid, which literally dissolves sea creatures’ shells. The acid, combined with low oxygen levels, has significant consequences for sea life.

Researchers first began pondering ocean anoxic events in the mid-1970s, after a discovery by Northwestern geologist Seymour Schlanger and Oxford professor Hugh Jenkyns. When examining sediment samples from the Pacific Ocean floor, Schlanger and Jenkyns discovered black, organic carbon-rich shales that matched samples — in composition and age — from both the Atlantic Ocean and rock formations in Italy.

Widespread lack of oxygen was the most likely explanation for these deposits. Anoxia prevents the breakdown of organic matter from dead plants and animals, leading to a global pattern of organic enrichment. Instead of decomposing, the settling plankton and other fossils accumulated to form organic carbon-rich strata scattered around the globe.

“How were black shales forming at the same time in the deep oceans and up on land?” Sageman asked. “Schlanger and Jenkyns realized there must have been a massive global event that caused oxygen to decrease from the ocean surface all the way down to the seafloor.”

History solidified in stone

In the new study, researchers looked not to the depths of the oceans but to ancient strata along the northwest edge of a mountain on Japan’s Hokkaido Island. The rocks, or tuffs, formed from volcanic ash that settled and solidified over time. Tectonic activity lifted these layers above sea level during formation of the Japanese islands, leaving them exposed and accessible where streams carve through the temperate rainforest of Hokkaido. By collecting and analyzing the tuffs, Sageman, his Ph.D. student, Luca Podrecca, and their collaborators gained a glimpse into geologic history.

“Magma comes out of a volcano in liquid form and then begins to cool,” Sageman said. “During this process, crystals start to form. By the time the tuff solidifies, the crystals become a tiny closed system. They lock in atoms, and some of those atoms, like uranium, start to decay, meaning they convert from one isotope to another. That provides a tool to date the eruption, and, thus, date a specific layer within a stack of sedimentary rock. While the expertise of team members from Tohuku University in Japan, Durham University in the U.K. and Northwestern focuses on the characterization and global correlation of the strata, our collaborators at the University of Wisconsin-Madison and Boise State University are experts in the geochronological analyses.”

The researchers also used other types of isotopes, such as carbon, which tracks synchronous changes in the carbon cycle, and osmium, which tracks volcanic activity and changes in ocean chemistry.

“These isotope systems provide tools for correlating the OAE1a interval between sites in Hokkaido, southern France and other sites all around the globe,” Sageman said. “They give us markers for instants in geologic time.”

Pinpointing the exact timeline

According to this evidence, an abrupt shift in carbon isotope ratios — caused first by the spike in volcanic CO2added to the carbon cycle (and later by the excess burial of organic matter) — occurred in the early Cretaceous at the beginning of OAE 1a. A concurrent shift in the isotopic ratios of osmium reflects a massive input of volcanic material into ocean waters. The timing of these events corresponds to eruption of the Ontong Java Nui complex, an enormous igneous province about the size of Alaska located in the southwestern Pacific Ocean.

Now that researchers know it took the oceans 1.1 million years to recover from the sharp increase in CO2, they have more insight into how long the effects of CO2-driven warming events might last and what the associated effects, such as ocean anoxia, may be.

“We’re already seeing zones with low oxygen levels in the Gulf of Mexico,” Sageman said. “The main difference is that past events unfolded over tens of thousands to millions of years. We’re driving roughly similar levels of warming (or more) but doing so in less than 200 years.”

Reference:
Youjuan Li, Brad S. Singer, Reishi Takashima, Mark D. Schmitz, Luca G. Podrecca, Bradley B. Sageman, David Selby, Toshiro Yamanaka, Michael T. Mohr, Keiichi Hayashi, Taiga Tomaru, Katarina Savatic. Radioisotopic chronology of Ocean Anoxic Event 1a: Framework for analysis of driving mechanisms. Science Advances, 2024; 10 (47) DOI: 10.1126/sciadv.adn8365

Note: The above post is reprinted from materials provided by Northwestern University.

New simulation method sharpens our view into Earth’s interior

Earth
Earth’s mantle Credit: Naeblys

How does the Earth generate its magnetic field? While the basic mechanisms seem to be understood, many details remain unresolved. A team of researchers from the Center for Advanced Systems Understanding (CASUS) at the Helmholtz-Zentrum Dresden-Rossendorf (HZDR), Sandia National Laboratories in the USA and the French Alternative Energies and Atomic Energy Commission (CEA) has introduced a simulation method that promises new insights into the Earth’s core. The method simulates not only the behavior of atoms, but also the magnetic properties of materials. The approach is significant for geophysics, but could also support the development of future technologies such as neuromorphic computing — an innovative approach to more efficient AI systems. The team presents its findings in the journal PNAS.

The Earth’s magnetic field is essential for sustaining life, as it shields the planet from cosmic radiation and solar wind. It is generated by the geodynamo effect. “We know that the Earth’s core is primarily composed of iron,” explains Attila Cangi, Head of the Machine Learning for Materials Design department at CASUS. “As you get closer to the Earth’s core, both temperature and pressure increase. The increase in temperature causes materials to melt, while the increase in pressure keeps them solid. Because of the specific temperature and pressure conditions inside the Earth, the outer core is in a molten state, while the inner core remains solid.” Electrically charged, liquid iron flows around the solid inner core driven by Earth’s rotation and convection currents. These movements produce electric currents, which, in turn, generate the planet’s magnetic field.

However, important questions about the Earth’s core remain unanswered. For instance, what is the exact structure of its core? And what role do additional elements — thought to be present alongside iron — play? Both factors could profoundly influence the geodynamo effect. Clues come from experiments where scientists send seismic waves through the Earth and measure their “echoes” with highly sensitive sensors. “These experiments suggest that the core contains more than just iron,” says Svetoslav Nikolov from Sandia National Laboratories, lead author of the study. “The measurements do not agree with computer simulations that assume a pure iron core.”

Simulating shock waves on the computer

The research team now achieved significant progress by developing and testing a new simulation method. The key innovation of the method called molecular-spin dynamics lies in the integration of two previously separate simulation approaches: molecular dynamics, which models atomic motion, and spin dynamics, which accounts for magnetic properties. “By combining these two methods, we were able to investigate the influence of magnetism under high-pressure and high-temperature conditions on length and time scales that were previously unattainable,” emphasizes CEA physicist Julien Tranchida. Specifically, the team simulated the behavior of two million iron atoms and their spins to analyze the dynamic interplay between mechanical and magnetic properties. The researchers also employed artificial intelligence (AI), using machine learning to determine force fields — interactions between atoms — with high precision. Developing and training these models required high-performance computing resources.

Once the models were ready, the researchers performed the actual simulations: the digital model of two million iron atoms, representative of the Earth’s core, was subjected to the temperature and pressure conditions found in the Earth’s interior. This was done by propagating pressure waves through the iron atoms, simulating their heating and compression. When the speed of these shock waves was lower, the iron remained solid and adopted different crystal structures. When the shock waves were faster, the iron became mostly liquid. In particular, the researchers found that magnetic effects significantly affect the material’s properties. “Our simulations agree well with the experimental data,” says Mitchell Wood, a materials scientist at Sandia National Laboratories, “and they suggest that under certain temperature and pressure conditions, a particular phase of iron could stabilize and potentially affect the geodynamo.” This phase, known as the bcc phase, has not been experimentally observed in iron under these conditions, only hypothesized. If confirmed, the results of the molecular-spin dynamics method could help resolve several questions about the geodynamo effect.

Driving energy-efficient AI

Beyond uncovering new details about the Earth’s interior, the method also has the potential to drive technological innovations in materials science. Both in his department and through external collaboration, Cangi plans to use the technique to model neuromorphic computing devices. This is a new type of hardware inspired by the way the human brain works, which could one day process AI algorithms faster and more energy-efficiently. By digitally replicating spin-based neuromorphic systems, the new simulation method could support the development of innovative, efficient hardware solutions for machine learning.

Data storage offers a second compelling avenue for further research: Magnetic domains along tiny nanowires could serve as storage media that are faster and more energy-efficient than conventional technologies. “There are currently no accurate simulation methods for either application,” says Cangi. “But I am confident that our new approach can model the required physical processes in such a realistic way, that we can significantly accelerate the technological development of these IT innovations.”

Reference:
Svetoslav Nikolov, Kushal Ramakrishna, Andrew Rohskopf, Mani Lokamani, Julien Tranchida, John Carpenter, Attila Cangi, Mitchell A. Wood. Probing iron in Earth’s core with molecular-spin dynamics. Proceedings of the National Academy of Sciences, 2024; 121 (51) DOI: 10.1073/pnas.2408897121

Note: The above post is reprinted from materials provided by Helmholtz-Zentrum Dresden-Rossendorf.

Unlocking the journey of gold through magmatic fluids

Gold nugget found in the field. Credit: University of Adelaide
Gold nugget found in the field. Credit: University of Adelaide

When one tectonic plate sinks beneath another, it generates magmas rich in volatiles such as water, sulphur and chlorine. As these magmas ascend, they release magmatic fluids, in which sulphur and chlorine bind to metals such as gold and copper, and transport these metals towards the surface of the Earth. As the extreme conditions relevant to natural magmas are very difficult to reproduce in the laboratory, the precise role of the different forms of sulphur in metal transport remains highly debated. However, an innovative approach by a team from the University of Geneva (UNIGE) has demonstrated that sulphur, in its bisulphide (HS-) form, is crucial for the transport of gold in magmatic fluids. These findings are published in Nature Geoscience.

When two tectonic plates collide, the subducting plate plunges into the Earth’s mantle, heats up and releases large amounts of water. This water lowers the melting temperature of the mantle, which melts under high pressure and temperatures exceeding a thousand degrees Celsius to form magmas. As the liquid magma is less dense than the rest of the mantle, it migrates towards the Earth’s surface.

”Due to the drop in pressure, magmas rising towards the Earth’s surface saturate a water-rich fluid, which is then released as magmatic fluid bubbles, leaving a silicate melt behind” explains Stefan Farsang, a postdoctoral fellow at the Department of Earth Sciences at UNIGE’s Faculty of Science and first author of the study. Magmatic fluids are therefore composed partly of water, but also of dissolved volatile elements such as sulphur and chlorine. These two elements are crucial because they extract gold, copper and other metals from the silicate melt into the magmatic fluid, thus facilitating their migration towards the surface.

Several forms of sulphur

Sulphur can easily be reduced or oxidised, i.e. gain or lose electrons, a process known as redox. The redox state of sulphur is important because it affects its ability to bind to other elements, such as metals. However, one debate has divided the scientific community for more than a decade: what is the redox state of the sulphur present in the magmatic fluid that mobilizes and transports metals?

Zoltán Zajacz, associate professor in the Department of Earth Sciences at UNIGE’s Faculty of Science and coauthor of the study, explains: “A seminal paper in 2011 suggested that S3- sulphur radicals play this role. However, the experimental and analytical methods had several limitations, particularly when it came to reproducing relevant magmatic pressure-temperature and redox conditions, which we have now overcome.”

Methodological revolution

The UNIGE team placed a quartz cylinder and a liquid with a composition similar to that of a magmatic fluid in a sealed gold capsule. The capsule was then put into a pressure vessel, which was then brought to pressure and temperature conditions characteristic of magmas emplaced in the Earth’s upper crust. ”Above all, our setup facilitates flexible control of the redox conditions in the system, which wasn’t possible before,” adds Stefan Farsang.

During the experiments, the quartz cylinder is fractured, allowing the synthetic magmatic fluid to enter. The quartz then traps microscopic-sized droplets of fluid like those found in nature, and the form of sulphur in these can be analysed at high temperature and pressure by using lasers with an analytical technique known as Raman spectroscopy. While previous spectroscopic experiments were typically run up to 700 °C, the UNIGE team succeeded in raising the temperature to 875 °C characteristic of natural magmas.

Bisulphide as a transporter

The study shows that bisulphide (HS-), hydrogen sulfide (H₂S) and sulphur-dioxide (SO₂) are the major sulphur species present in the experimental fluids at magmatic temperatures. The role of bisulphide in metal transport was already well documented in lower-temperature so-called hydrothermal fluids that originate from the higher-temperature magmatic fluids. However, bisulfide was thought to have very limited stability at magmatic temperatures. Thanks to their cutting-edge methodology, the UNIGE team was able to show that in magmatic fluids too, bisulphide is responsible for transporting most of the gold.

”By carefully choosing our laser wavelengths, we also showed that in previous studies, the amount of sulphur radicals in geologic fluids was severely overestimated and that the results of the 2011 study were in fact based on a measurement artefact, putting an end to this debate,” says Stefan Farsang. The conditions leading to the formation of important precious metal ore deposits have now been clarified. Since much of the world’s copper and gold production comes from deposits formed by magma-derived fluids, this study may contribute to their exploration by opening up important perspectives for understanding their formation.

Reference:
Stefan Farsang, Zoltán Zajacz. Sulfur species and gold transport in arc magmatic fluids. Nature Geoscience, 2024; DOI: 10.1038/s41561-024-01601-3

Note: The above post is reprinted from materials provided by Université de Genève.

Massive volcanic eruptions did not cause the extinction of dinosaurs

volcanoes
volcanoes

Massive volcanic eruptions on the Indian peninsula have long been proposed as an alternative cause for the demise of the dinosaurs. This phase of active volcanism took place in a period just before the Earth was struck by a meteorite, 66 million years ago. The effect of these volcanic eruptions on the Earth’s climate has been topic of fierce scientific debates for decades. Now, climate scientists from Utrecht University and the University of Manchester show that, while the volcanism caused a temporary cold period, the effects had already worn off thousands of years before the meteorite impacted. The scientists therefore conclude that the meteorite impact was the ultimate cause of the dinosaur extinction event.

What killed off the dinosaurs — was it the Chicxulub meteorite or did the effects of massive volcanism also play a role? Many modern children’s books on the history of dinosaurs include speculation on these two competing ideas.

The meteorite impact in the Gulf of Mexico roughly 66 million years ago is well researched and widely known as the defining end of the dinosaur age. But earth scientists have fiercely debated for decades whether a massive outpouring of lava on the Indian continent, which occurred both prior to and after the meteorite impact, also contributed to the demise of dinosaur populations roaming the Earth. These volcanic eruptions released vast amounts of CO2, dust, and sulphur, thereby significantly altering the climate on earth — but in different ways and on different timescales to a meteorite impact.

Ancient peats

A new publication in the scientific journal Science Advances by climate scientists from Utrecht University and the University of Manchester now provides compelling evidence that while the volcanic eruptions in India had a clear impact on global climate, they likely had little to no effect on the mass extinction of the dinosaurs.

By analysing fossil molecules in ancient peats from the United States of America, the scientific team reconstructed air temperatures for the time period covering both the volcanic eruptions and the meteorite impact. Using this method, the researchers show that a major volcanic eruption occurred about 30,000 years before the meteor impact, coinciding with at least a 5° Celsius cooling of the climate. They also conclude that this cooling was likely the result of volcanic sulphur emissions blocking sunlight from reaching the Earth’s surface.

Importantly, the scientists discovered that by around 20,000 years before the meteorite impact, temperatures on Earth had already stabilised and had climbed back to similar temperatures before the volcanic eruptions started. This period of global warming was likely aided by volcanic CO2 emissions, says Lauren O’Connor at Utrecht University: “These volcanic eruptions and associated CO2 and sulphur release would have had drastic consequences for life on earth. But these events happened millennia before the meteorite impact and probably played only a small part in the extinction of dinosaurs.”

Impact winter

With the effects of volcanism practically ruled out, this would leave the Chicxulub meteorite impact as the primary cause of the dinosaur mass extinction. “By comparison, the impact from the asteroid unleashed a chain of disasters, including wildfires, earthquakes, tsunamis, and an ‘impact winter’ that blocked sunlight and devastated ecosystems. We believe the asteroid that ultimately delivered the fatal blow,” says Rhodri Jerrett at the University of Manchester.

The fossil peats that the researchers analysed contain specific membrane-spanning molecules produced by bacteria. The structure of these molecules changes depending on the temperature of their environment. By analysing the composition of these molecules preserved in ancient sediments, scientists are able to calculate past temperatures. O’Connor adds: “This way, we were able to create a detailed ‘temperature timeline’ for the years leading up to the dinosaur extinction, which we can compare to the fossil record to understand the relative timing of events..”

The researchers from Utrecht University, the University of Manchester, Plymouth University, and the Denver Museum of Nature & Science, are now applying the same approach to reconstruct past climate at other critical periods in Earth’s history.

Reference:
Lauren K. O’Connor, Rhodri M. Jerrett, Gregory D. Price, Tyler R. Lyson, Sabine K. Lengger, Francien Peterse, Bart E. van Dongen. Terrestrial evidence for volcanogenic sulfate-driven cooling event ~30 kyr before the Cretaceous–Paleogene mass extinction. Science Advances, 2024; 10 (51) DOI: 10.1126/sciadv.ado5478

Note: The above post is reprinted from materials provided by Utrecht University.

Tyrannosaur teeth discovered in Bexhill-on-Sea, England

Discovered teeth of (a) spinosaur, (b) tyrannosaur, (c) dromaeosaur, (d) possible tyrannosaur, (e) indeterminate tyrannoraptoran - the group containing tyrannosaurs and dromaeosaurs (Velociraptor and kin). Credit Barker et al (2024)
Discovered teeth of (a) spinosaur, (b) tyrannosaur, (c) dromaeosaur, (d) possible tyrannosaur, (e) indeterminate tyrannoraptoran – the group containing tyrannosaurs and dromaeosaurs (Velociraptor and kin). Credit Barker et al (2024)

Research led by the University of Southampton has revealed that several groups of meat-eating dinosaur stalked the Bexhill-on-Sea region of coastal East Sussex 135 million years ago.

The study, published today [5 December 2024] in Papers in Palaeontology, has discovered a whole community of predators belonging to different dinosaur groups — including tyrannosaurs, spinosaurs and members of the Velociraptor family.

It’s the first time tyrannosaurs have been identified in sediments of this age and region.

“Meat-eating dinosaurs — properly called theropods — are rare in the Cretaceous sediments of southern England,” said Dr Chris Barker, visiting researcher at the University of Southampton and lead author of the research.

“Usually, Isle of Wight dinosaurs attract most of our attention. Much less is known about the older Cretaceous specimens recovered from sites on the mainland.”

Dinosaur teeth

The new Bexhill-on-Sea dinosaurs are represented by teeth alone.

Theropod teeth are complex, and vary in size, shape, and in the anatomy of their serrated edges. The University of Southampton team used several techniques to analyse the fossils, including phylogenetic, discriminant and machine learning methods, teaming up with colleagues at London’s Natural History Museum, the Hastings Museum and Art Gallery, and the Museo Miguel Lillo De Ciencias Naturales in Argentina.

“Dinosaur teeth are tough fossils and are usually preserved more frequently than bone. For that reason, they’re often crucial when we want to reconstruct the diversity of an ecosystem,” says Dr Barker.

“Rigorous methods exist that can help identify teeth with high accuracy. Our results suggest the presence of spinosaurs, mid-sized tyrannosaurs and tiny dromaeosaurs — Velociraptor-like theropods — in these deposits.”

The discovery of tyrannosaurs is particularly notable, since the group hasn’t previously been identified in sediments of this age and region. These tyrannosaurs would have been around a third of the size of their famous cousin Tyrannosaurus rex, and likely hunted small dinosaurs and other reptiles in their floodplain habitat.

“Assigning isolated teeth to theropod groups can be challenging, especially as many features evolve independently amongst different lineages. This is why we employed various methods to help refine our findings, leading to more confident classifications,” says Lucy Handford, co-author of the paper and former University of Southampton Master’s student, who is now undertaking a PhD at the University of York.

“It’s highly likely that reassessment of theropod teeth in museum stores elsewhere will bring up additional discoveries.”

Discovery at Ashdown Brickworks

The tireless collecting of retired quarryman Dave Brockhurst, who has spent the last 30 years uncovering fossils from Ashdown Brickworks, was key to the discovery.

Dave has uncovered thousands of specimens, ranging from partial dinosaur skeletons to tiny shark teeth. Around 5000 of his discoveries have already been donated to Bexhill Museum. Theropods are exceptionally rare at the site, and Dave has only found ten or so specimens there so far.

“As a child I was fascinated by dinosaurs and never thought how close they could be,” says Mr Brockhurst. “Many years later I started work at Ashdown and began looking for fossils. I’m happy with tiny fish scales or huge thigh bones, although the preservation of the dinosaur teeth really stands out for me.”

Exciting find

Dr Darren Naish, a co-author of the study, added: “Southern England has an exceptionally good record of Cretaceous dinosaurs, and various sediment layers here are globally unique in terms of geological age and the fossils they contain.

“These East Sussex dinosaurs are older than those from the better-known Cretaceous sediments of the Isle of Wight, and are mysterious and poorly known by comparison. We’ve hoped for decades to find out which theropod groups lived here, so the conclusions of our new study are really exciting.”

Dr Neil Gostling, also from the University of Southampton, supervised the project. He said: “This project shows that museum collections, curators, and collectors are vital for pushing forward our understanding of the diversity of dinosaurs, and other extinct groups. We’re also very thankful to Ashdown Brickworks for their cooperation in preserving the quarry’s important palaeontological heritage.

“200 years after the naming of the first dinosaur, Megalosaurus, there are still really big discoveries to be made. Dinosaur palaeobiology is alive and well.”

Several of the specimens are on display at Bexhill Museum in East Sussex.

The research was funded by the University of Southampton’s Institute for Life Sciences.

Reference:
Chris T. Barker, Lucy Handford, Darren Naish, Simon Wills, Christophe Hendrickx, Phil Hadland, Dave Brockhurst, Neil J. Gostling. Theropod dinosaur diversity of the lower English Wealden: analysis of a tooth‐based fauna from the Wadhurst Clay Formation (Lower Cretaceous: Valanginian) via phylogenetic, discriminant and machine learning methods. Papers in Palaeontology, 2024; 10 (6) DOI: 10.1002/spp2.1604

Note: The above post is reprinted from materials provided by University of Southampton.

Fossil dung reveals clues to dinosaur success story

The researchers have chosen to understand the biology of early dinosaurs based on their dietary preferences.
The researchers have chosen to understand the biology of early dinosaurs based on their dietary preferences.

In an international collaboration, researchers at Uppsala University have been able to identify undigested food remains, plants and prey in the fossilised faeces of dinosaurs. These analyses of hundreds of samples provide clues about the role dinosaurs played in the ecosystem around 200 million years ago. The findings have been published in the journal Nature.

“Piecing together ‘who ate whom’ in the past is true detective work,” says Martin Qvarnström, researcher at the Department of Organismal Biology and lead author of the study. “Being able to examine what animals ate and how they interacted with their environment helps us understand what enabled dinosaurs to be so successful.”

Palaeontologists from Uppsala University, in collaboration with researchers from Norway, Poland and Hungary, have examined hundreds of samples using advanced synchrotron imaging to visualise the hidden, internal parts of the fossilised faeces, known as coprolites, in detail. By identifying undigested food remains, plants and prey, they have recreated the structure of the ecosystems at the time when dinosaurs began their success story.

The study focused on a previously underexplored region, Polish Basin, located in the Late Triassic time in the in the northern parts of the then supercontinent Pangea. The researchers built up a comprehensive picture of the Triassic and Jurassic ecosystems (from about 230 to 200 million years ago) by combining the information from the coprolites with climate data and information from other fossils: plants, bite marks, vomit, footprints and bones.

“The research material was collected over a period of 25 years. It took us many years to piece everything together into a coherent picture,” says Grzegorz Niedźwiedzki, researcher at the Department of Organismal Biology and the study’s senior author. “Our research is innovative because we have chosen to understand the biology of early dinosaurs based on their dietary preferences. There were many surprising discoveries along the way.”

The coprolites contained remains of fish, insects, larger animals and plants, some of which were unusually well preserved, including small beetles and semi-complete fish. Other coprolites contained bones chewed up by predators that, like today’s hyenas, crushed bones to obtain salts and marrow. The contents of coprolites from the first large herbivorous dinosaurs, the long-necked sauropods, surprised the researchers. These contained large quantities of tree ferns, but also other types of plants, and charcoal. The palaeontologists hypothesise that charcoal was ingested to detoxify stomach contents, as ferns can be toxic to herbivores.

The research addresses a significant gap in current knowledge: the first 30 million years of dinosaur evolution during the Late Triassic period. Although much is known about their lives and extinction, the ecological and evolutionary processes that led to their rise are largely unexplored. The study results in a five-step model of dinosaur evolution that the researchers believe can explain global patterns.

The team emphasises that understanding how the first dinosaurs achieved their success can offer valuable insights into prehistoric ecosystems and evolutionary processes in general. The results show that dietary diversity and adaptability were crucial survival traits during the environmental changes of the Late Triassic.

“Unfortunately, climate change and mass extinctions are not just a thing of the past. By studying past ecosystems, we gain a better understanding of how life adapts and thrives under changing environmental conditions,” says Qvarnström.

“The way to avoid extinction is to eat a lot of plants, which is exactly what the early herbivorous dinosaurs did. The reason for their evolutionary success is a true love of green and fresh plant shoots,” Niedzwiedzki concludes.

Reference:
Martin Qvarnström, Joel Vikberg Wernström, Zuzanna Wawrzyniak, Maria Barbacka, Grzegorz Pacyna, Artur Górecki, Jadwiga Ziaja, Agata Jarzynka, Krzysztof Owocki, Tomasz Sulej, Leszek Marynowski, Grzegorz Pieńkowski, Per E. Ahlberg, Grzegorz Niedźwiedzki. Digestive contents and food webs record the advent of dinosaur supremacy. Nature, 2024; DOI: 10.1038/s41586-024-08265-4

Note: The above post is reprinted from materials provided by Uppsala University.

Giant prehistoric elephant skull from India belongs to mysterious extinct species

An imposing fully-grown male Palaeoloxodon turkmenicus wandering the Kashmir Valley, 400 thousand years ago, towering over a herd of Central Asian red deer traversing by. In the distance, a small band of prehistoric humans set up campfire to cook their meal. Credit: Chen Yu, University of Helsinki
An imposing fully-grown male Palaeoloxodon turkmenicus wandering the Kashmir Valley, 400 thousand years ago, towering over a herd of Central Asian red deer traversing by. In the distance, a small band of prehistoric humans set up campfire to cook their meal. Credit: Chen Yu, University of Helsinki

The giant fossil skull of an extinct elephant, discovered in northern India’s Kashmir Valley in 2000, sheds light on a poorly known episode in elephant evolutionary history.

The elephant skull was buried with 87 stone tools used by prehistoric humans, and all the materials were excavated under the leadership of Dr. Ghulam Bhat at the University of Jammu.

Recently, an international team of scientists from the Florida Museum of Natural History, the British Museum, the University of York, and the Natural History Museum (London), along with the University of Helsinki’s Dr. Steven Zhang, studied the Kashmir skull to uncover the age and evolutionary context of this megaherbivore. The paper is published in the Journal of Vertebrate Paleontology.

“From the general shape of the skull, it’s quite apparent that the elephant belonged to Palaeoloxodon, or straight-tusked elephants, among the largest land mammals that ever lived. Full-grown adults easily stood around 4m tall at the shoulder and weighed 9–10 tonnes,” says Zhang, a paleontologist from the University’s Department of Geosciences and Geography.

“Yet what’s puzzled experts for some time is that the Kashmir skull lacks a thickened, forward-projecting crest at the skull roof which typifies other Palaeoloxodon skulls found in India.”

Over recent decades, whether the developmental extent of this crest could tell apart different species of Palaeoloxodon and the relative position of these species on the evolutionary tree of elephants has remained controversial. However, recent research concluded that the skull crest in these extinct elephants became more prominent with developmental and sexual maturity. This means that, once specimens can be aged by examining their teeth, it would be possible to compare skulls from individuals with similar levels of maturity.

“From the size, the wisdom teeth and a few other telltale features of the skull, it is evident that the animal was a majestic bull elephant in the prime of its life, but the lack of a well-developed skull crest, particularly in comparison with other mature male skulls from Europe and from India, tells us we have a different species on our hands here,” Zhang explained.

Instead, the research team noticed how the Kashmir skull’s features conform best with another obscure skull from Turkmenistan studied in the 1950s, which was proposed to represent a distinct species, Palaeoloxodon turkmenicus.

“What’s always been puzzling about the Turkmen skull is that, besides the lack of a prominent crest at the skull roof, its other features are highly similar to the already well-known European species, P. antiquus. And this led a number of experts to suggest that the Turkmen specimen is simply an aberrant individual of the European species,” says Zhang.

“But with the Kashmir skull added to the mix, it becomes clear now that the two specimens can be theorized to represent a distinct species that we previously knew very little about, with a broad distribution from Central Asia to the northern Indian Subcontinent,” added Dr. Advait Jukar, the study’s lead author, currently based at the Florida Museum of Natural History.

By measuring protein decomposition in the tooth enamel of the Kashmir Palaeoloxodon skull, and examining stone tools buried alongside the elephant remains, the team concluded that the Kashmir skull dates to the Middle Pleistocene period 300,000–400,000 years ago, very similar to the estimated age of the Turkmen skull. This supports the belief that the two skulls represent a species distinct from other Eurasian Palaeoloxodon.

Palaeoloxodon first evolved in Africa around 1 million years ago; this early African form had a narrow, convex forehead and underdevelopment of the skull crest. Later Palaeoloxodon, best-known from fossils discovered in Europe and India, have very wide, flattened forehead often associated with a thick crest that juts forward from the roof of the skull.

The team thus concluded that with a wide, flat forehead with only the faintest trace of a skull crest, P. turkmenicus may represent a poorly-known missing link that fills a gap in our understanding of how these prodigious prehistoric megaherbivores evolved.

Reference:
Advait M. Jukar et al, A remarkable Palaeoloxodon (Mammalia, Proboscidea) skull from the intermontane Kashmir Valley, India, Journal of Vertebrate Paleontology (2024). DOI: 10.1080/02724634.2024.2396821

Note: The above post is reprinted from materials provided by University of Helsinki.

Extremely well-preserved fossil sawfly sheds new light on co-evolution of insects and toxic plants

The fossil is believed to be between 11 and 16 million years old, from the Miocene Period. Credit: Michael Frese, University of Canberra
The fossil is believed to be between 11 and 16 million years old, from the Miocene Period. Credit: Michael Frese, University of Canberra

A team of Australian researchers has described a new species of now-extinct sawfly from an extremely well-preserved fossil found in central NSW.

This fossilised sawfly, which is between 11 and 16 million years old from the Miocene Period, was the first of its kind discovered in Australia and only the second discovered in the world. It was found by a team of palaeontologists in 2018 who were exploring McGraths Flat, a fossil site in central NSW that has since yielded many other detailed fossils.

Despite the name, sawflies are not flies but a type of wasp, with spitfires the most widely recognised group of sawfly species in Australia. They are called sawflies because they have a saw-like ovipositor that is used to lay eggs, and they could be mistaken as flies because they lack a typical ‘wasp waist’.

With the approval of the Mudgee Local Aboriginal Land Council, Wiradjuri words were used to name the newly described species of sawfly Baladi warru. ‘Baladi’ means ‘saw’ and ‘warru’ means ‘wasp’. This name honours the Traditional Owners of the lands on which the fossil was located.

Researchers from Australia’s national science agency, CSIRO, the University of Canberra, Australian Museum and Queensland Museum have analysed the sawfly’s wing venation and other features preserved in the fossil and determined its taxonomic (scientific naming) placement within sawflies. This allowed them to describe it as a new species.

CSIRO research scientist, Dr Juanita Rodriguez, helped describe the new sawfly species.

“We looked at the fossil and its morphology and then put this information together with molecular and morphological data from a wide sample of current sawfly species. This helped us decipher the fossil’s placement in the sawfly tree of life,” Dr Rodriguez said.

“We used the fossil’s age and its placement to establish that sawflies originated in the Cretaceous Period, around 100 million years ago, which means their ancient ancestors lived in Gondwana. When this supercontinent split up, sawflies ended up distributed in Australia and South America.

“When we examined the fossil, we identified pollen grains on the sawfly’s head which revealed it had visited a flowering Quintinia plant. This helped our team trace complex species interactions in the palaeoenvironment of McGraths Flat.”

University of Canberra palaeontologist and CSIRO visiting scientist, Dr Michael Frese, who found the fossil sawfly, said this discovery would help researchers track evolution and distribution of sawflies.

“In particular, this find has helped us in understanding the incredible ability of sawflies to feed on toxic plants,” Dr Frese said.

“They eat the leaves of Myrtaceae – a family of woody plants that includes eucalypts – because they have mouthparts with which they can separate toxic oils or a chemical detoxification system inside their gut when feeding on myrtaceous leaves. This enables the larvae, sometimes called spitfires, to use the oils as a defensive weapon.

“In terms of the bigger picture, our work is helping researchers make sense of their current distribution across Australia and the Americas.

“Although this particular species, Baladi warru, has been extinct for millions of years, it provides information on native pollinators so we can understand their evolution and impact in the present.”

Reference:
Juanita Rodriguez et al, A new exceptionally preserved sawfly fossil (Hymenoptera: Pergidae) and an evaluation of its utility for divergence time estimation and biogeography, Systematic Entomology (2024). DOI: 10.1111/syen.12653

Note: The above post is reprinted from materials provided by CSIRO.

Golden bugs: Spectacular new fossil arthropods preserved in fool’s gold

The holotype specimen of Lomankus edgecombei. Photograph at left, other images at right are 3D models from CT scanning. Credit: Luke Parry (photograph), Yu Liu, Ruixin Ran (3D models).
The holotype specimen of Lomankus edgecombei. Photograph at left, other images at right are 3D models from CT scanning. Credit: Luke Parry (photograph), Yu Liu, Ruixin Ran (3D models).

A team of researchers led by Associate Professor Luke Parry, Department of Earth Sciences, University of Oxford, have unveiled a spectacular new 450-million-year-old fossil arthropod (the group that contains spiders, centipedes, and insects). Besides being an extraordinary-looking new scientific species, the specimens are entirely preserved by fool’s gold.

The work is published in the journal Current Biology.

Associate Professor Parry said, “As well as having their beautiful and striking golden color, these fossils are spectacularly preserved. They look as if they could just get up and scuttle away.”

The new fossil, named Lomankus edgecombei, after arthropod expert Greg Edgecombe of London’s Natural History Museum, belongs to a group called megacheirans, an iconic group of arthropods with a large, modified leg (called a “great appendage”) at the front of their bodies that was used to capture prey.

Megacheirans like Lomankus were very diverse during the Cambrian Period (538–485 million years ago) but were thought to be largely extinct by the Ordovician Period (485–443 million years ago).

This discovery offers important new clues towards solving the long-standing riddle of how arthropods evolved the appendages on their heads: one or more pairs of legs at the front of their bodies modified for specialized functions like sensing the environment and capturing prey. Such appendages include the antennae of insects and crustaceans, and the pincers and fangs of spiders and scorpions.

“Today, there are more species of arthropod than any other group of animals on Earth. Part of the key to this success is their highly adaptable head and its appendages, that has adapted to various challenges like a biological Swiss army knife,” Associate Professor Parry continued.

While other megacheirans used their large first appendage for capturing prey, in Lomankus the typical claws are much reduced, with three long and flexible whip-like flagella at their end. This suggests that Lomankus was using this frontal appendage to sense the environment, rather than to capture prey, indicating it lived a very different lifestyle to its more ancient relatives in the Cambrian Period.

Unlike other megacheirans, Lomankus seems to lack eyes, suggesting that it relied on its frontal appendage to sense and search for food in the dark, low-oxygen environment in which it lived.

“Rather than representing a ‘dead end,’ Lomankus shows us that megacheirans continued to diversify and evolve long after the Cambrian, with the formerly fearsome great appendage now performing a totally different function,” Associate Professor Parry continued.

The fossil offers new clues towards solving the highly-debated question of what the equivalent of the great appendage of megacheirans is in living species.

Co-corresponding author Professor Yu Liu (Yunnan University) said, “These beautiful new fossils show a very clear plate on the underside of the head, associated with the mouth and flanked by the great appendages. This is a very similar arrangement to the head of megacheirans from the early Cambrian of China except for the lack of eyes, suggesting that Lomankus probably lived in a deeper and darker niche than its Cambrian relatives.”

This arrangement of features on the head is similar to living arthropods, suggesting the great appendage is the equivalent of the antenna of insects and the chelicera (mouthparts) of spiders and scorpions.

The fossil was found at a site in New York State, U.S. that contains the famous “Beecher’s Trilobite Bed”; a layer of rock containing multiple trilobites with incredible preservation. Aside from trilobites, other kinds of organisms are much less common at this site, reflecting the rarity of this find.

The animals preserved in Beecher’s Trilobite Bed lived in a hostile, low oxygen environment that allowed pyrite, commonly known as fool’s gold, to replace parts of their bodies after they were buried in sediment, resulting in spectacular golden 3D fossils. Pyrite is a very dense mineral, and so fossils from this layer can be CT scanned to reveal hidden details of their anatomy.

This technique involves rotating the specimen while taking thousands of X-ray images, allowing the fossils to be reconstructed in three dimensions.

Professor Derek Briggs, a co-author of the study at Yale University said, “These remarkable fossils show how rapid replacement of delicate anatomical features in pyrite before they decay, which is a signature feature of Beecher’s Trilobite Bed, preserves critical evidence of the evolution of life in the oceans 450 million years ago.”

Reference:
A pyritized Ordovician leanchoiliid arthropod, Current Biology (2024). DOI: 10.1016/j.cub.2024.10.013.

Note: The above post is reprinted from materials provided by University of Oxford.

This ancient tadpole fossil is the oldest ever discovered

This image provided by Mariana Chuliver shows the oldest-known tadpole fossil found in Patagonia, Argentina. Credit: Mariana Chuliver via AP
This image provided by Mariana Chuliver shows the oldest-known tadpole fossil found in Patagonia, Argentina. Credit: Mariana Chuliver via AP

Scientists have discovered the oldest-known fossil of a giant tadpole that wriggled around over 160 million years ago.

The new fossil, found in Argentina, surpasses the previous ancient record holder by about 20 million years.

Imprinted in a slab of sandstone are parts of the tadpole’s skull and backbone, along with impressions of its eyes and nerves.

“It’s not only the oldest tadpole known, but also the most exquisitely preserved,” said study author Mariana Chuliver, a biologist at Buenos Aires’ Maimonides University.

Researchers know frogs were hopping around as far back as 217 million years ago. But exactly how and when they evolved to begin as tadpoles remains unclear.

This new discovery adds some clarity to that timeline. At about a half foot (16 centimeters) long, the tadpole is a younger version of an extinct giant frog.

“It’s starting to help narrow the timeframe in which a frog becomes a frog,” said Ben Kligman, a paleontologist at the Smithsonian National Museum of Natural History who was not involved with the research.

The results were published Wednesday in the journal Nature.

The fossil is strikingly similar to the tadpoles of today—even containing remnants of a gill scaffold system that modern-day tadpoles use to sift food particles from water.

That means the amphibians’ survival strategy has stayed tried and true for millions of years, helping them outlast several mass extinctions, Kligman said.

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