WFS News:Large new titanosaurian dinosaur from the Pyrenees

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Researchers from the Institut Català de Paleontologia Miquel Crusafont (ICP), the Conca Dellà Museum (MCD), the Universitat Autònoma de Barcelona (UAB), the University of Zaragoza (UNIZAR) and the NOVA University of Lisbon (UNL) have described the new species of titanosaur dinosaur Abditosaurus kuehnei from the remains excavated at the Orcau-1 site, in the southern Pyrenees (Catalonia, Spain). The semiarticulated 70.5-million-year-old skeleton is the most complete specimen of this herbivorous group of dinosaurs discovered so far in Europe. Moreover, Abditosaurus is the largest titanosaur species found in the Ibero-Armorican island — an ancient region nowadays comprising Iberia and the south of France — representing a senescent individual estimated to be 17,5 meters in length with body mass of 14,000 kg.

The size of this giant is one of the most surprising facts to researchers. “Titanosaurs from the Upper Cretaceous of Europe tend to be small or medium-sized due to their evolution in insular conditions,” explained Bernat Vila, paleontologist at the ICP leading the research. During the Upper Cretaceous (between 83 and 66 million years ago), Europe was a large archipelago made up of dozens of islands. The species that evolved there tend to be relatively small, or even dwarves compared to their relatives living in large landmasses, due primarily to the limitation of food resources in islands. “It is a recurring phenomenon in the history of life on Earth, we have several examples worldwide in the fossil record of this evolutionary trend. That’s why we were astonished by the large dimensions of this specimen,” said Vila.

The fieldwork conducted over several decades unearthed 53 skeletal elements of the specimen. These include several teeth, vertebrae, ribs, and limb, scapular and pelvic bones, as well as a semiarticulated fragment of the neck formed by 12 cervical vertebrae. “We were really lucky, it is unusual to find such complete specimens in the Pyrenees due to its troubled geologic history,” explains Àngel Galobart, ICP researcher and director of the Conca Dellà Museum (Isona, Catalonia).

The excavation of the neck in 2014 was a technical challenge. Once prepared for extraction, the neck was encased in a large block of polyurethane foam, becoming one of the largest jackets ever excavated in Europe.

The history of the research that has led to the description of the new species dates back to 1954, when German paleontologist Walter Kühne collected the first remains and sent them to Madrid. The site fell into oblivion until 1986, when some more remains began to be extracted until a great storm forced the cancellation of the excavation. Subsequently, fieldwork on the site fell again into oblivion until a paleontologist from the ICP resumed systematic excavations in Orcau-1. The story of this finding was featured in the 2017 documentary “Europe’s last giant.” The generic name Abditosaurus means ‘forgotten reptile’ and the specific epithet kuehnei is a tribute to its discoverer.

A migrating dinosaur

In their article published in Nature Ecology & Evolution, researchers conclude that Abditosaurus belongs to a group of saltasaurine titanosaurs from South America and Africa, different from the rest of European titanosaurs that are characterized by a smaller size. These authors hypothesize that the Abditosaurus lineage reached the Ibero-Armorican island taking advantage of a global drop in sea level that reactivated ancient migration routes between Africa and Europe.

“Other evidence support the migration hypothesis,” explains Albert Sellés, paleontologist at the ICP and co-author of the article. “In the same site we have found eggshells of dinosaur species known to have inhabited Gondwana, the southernmost continent.”

The new finding is a major advance in the understanding of the evolution of sauropod dinosaurs at the end of the Cretaceous and brings a new perspective to the phylogenetic and paleobiogeographic puzzle of sauropods in the last 15 million years before their extinction.

In addition to Vila, Sellés and Galobart, Novella Razzolini (Institut Català de Paleontologia Miquel Crusafont and Conca Dellà Museum), Miguel Moreno (Museu de Lurinhã and NOVA University of Lisbon), Iñaki Canudo (Aragosaurus-IUCA Group, University of Zaragoza) and Alejandro Gil (Universitat Autònoma de Barcelona) participated in this study.

“During the Jurassic and Cretaceous, Iberia was the point of connection between Eurasia, Africa and North America. Studying how Abditosaurus relates to the fauna of these continents helps us to understand when there were connections between them, and when they became isolated,” says Miguel Moreno, researcher at the Museu de Lurinhã and NOVA University of Lisbon that has performed the paleobiogeographic study.

The large Cretaceous herbivores

Titanosaurs are a group of sauropod dinosaurs that become very diverse and abundant in the terrestrial ecosystems of the Cretaceous. All of them were quadrupeds and phytophagous. Titanosaurs had a small and pointed skull, with small nail-shaped teeth used to uproot vegetation. Their body was robust, with forelimbs shorter than the hindlimbs and a long necks and tails. Some species sported a skin covered with bony plates named osteoderms that may have served as a protective shield or as a reserve of calcium.

The paleontological sites within the Catalan Pyrenees have provided exceptional dinosaur fossils over the last century. Research is especially significant as its fossil record includes the last vertebrate faunas, including non-avian dinosaurs, that lived in Europe right before the global extinction event that took place 66 million years ago.

On the ICP: The Institut Català de Paleontologia Miquel Crusafont (ICP) is a CERCA center (Centres de Recerca de Catalunya, Generalitat de Catalunya) ascribed to to the Universitat Autònoma de Barcelona (UAB) and devoted to research in vertebrate and human paleontology at the highest international level, as well as the conservation and dissemination of the Catalan paleontological heritage. It is constituted as a public foundation with a board of trustees made up of the Government of Catalonia and the UAB.

Journal Reference:

  1. Bernat Vila, Albert Sellés, Miguel Moreno-Azanza, Novella L. Razzolini, Alejandro Gil-Delgado, José Ignacio Canudo, Àngel Galobart. A titanosaurian sauropod with Gondwanan affinities in the latest Cretaceous of EuropeNature Ecology & Evolution, 2022; DOI: 10.1038/s41559-021-01651-5

Citation: Universitat Autonoma de Barcelona. “Large new titanosaurian dinosaur from the Pyrenees: The skeleton of Abditosaurus kuehnei is the most complete titanosaur fossil discovered so far in Europe.” ScienceDaily. ScienceDaily, 7 February 2022. <www.sciencedaily.com/releases/2022/02/220207124822.htm>.

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: Fruits of Euphorbiaceae from the Late Cretaceous Deccan Intertrappean Beds of India.

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Just before the closing scenes of the Cretaceous Period, India was a rogue subcontinent on a collision course with Asia. Before the two landmasses merged, however, India rafted over a “hot spot” within the Earth’s crust, triggering one of the largest volcanic eruptions in Earth’s history, which likely contributed to the extinction of the dinosaurs.

In a recent study, scientists excavating the fossilized remains of plant material wedged between layers of volcanic rock describe a new plant species based on the presence of distinctive fruit capsules that likely exploded to disperse their seeds. The fossils may be the oldest fruit discovered to date of the spurge family (Euphorbiaceae), a group of plants with more than 7,000 species, with well-known representatives that include poinsettia, castor oil plant, rubber trees and crotons.

The fossilized fruits were discovered near the village of Mohgaon Kalan in central India, where the remains of the once-widespread volcanic rock lie just beneath the surface in a complex mosaic.

“You can walk around these hills and find chunks of chert that have just weathered up through the topsoil,” said senior author Steven Manchester, curator of paleobotany at the Florida Museum of Natural History. “Some of the best collecting is where farmers have plowed the fields and moved the chunks to the side. For a paleobotanist, it’s like finding little Christmas presents all along the edge of the fields.”

Although there is some uncertainty in the timing, the volcanic eruptions are thought to have lasted for up to 1 million years, occurring in prolonged pulses that blanketed the surrounding landscape in thick lava layers up to 1 mile deep. Today, the basalt rocks leftover from the eruptions, known as the Deccan Traps, cover an area larger than the state of California.

The most violent of the volcanic events, which occurred at the tail end of the Cretaceous, may have been triggered by the asteroid impact half a world away.

“The impact in the Yucatan may have caused seismic perturbations that actually disturbed the regime on the other side of the planet, causing lava to erupt,” Manchester said.

New species grew in stunted forests

Sandwiched between the basalt, paleontologists have found shales, chert, limestone and clays stacked in a giant layer cake of alternating bands, most of which are rich in the fossilized remains of plants and animals. These fossils provide a glimpse into what seem to have been relatively calm periods of stability between massive lava flows.

The newly described species were likely shrubs or small trees that grew near hot springs created by the interaction of groundwater with naturally heated rock beneath the surface, similar to present-day environments in Yellowstone National Park. At the time of their preservation, India was inching its way through the Earth’s equatorial zone, creating warm, humid conditions that supported a number of tropical species, including bananas, aquatic ferns, mallows and relatives of modern crepe myrtles.

Petrified wood is a common find in the Deccan traps, but most of them have small diameters, suggesting a lack of large trees whose conspicuous absence has stumped scientists trying to stitch together the ecological history of the region.

“India was positioned at a low latitude, so we’d expect to find big forest giants. But that’s not what we’re seeing,” Manchester said.

It’s unclear why the trees were unable to obtain greater stature, but Manchester suspects the underlying basalt may have restricted the growth of roots. Alternatively, he said, the plants may have been part of young forests that grew in volcanically active regions, which would have wiped out the surrounding vegetation before it had a chance to mature. “You’re most likely to get fossils preserved when there’s been recent eruptions, which creates a lot of volcanic ash that can bury and preserve plants,” he said.

Scientists peel back the layers of mystery fruit

Fruits from the new species were found pristinely preserved in a matrix of chert by co-author Dashrath Kapgate. But with only the fruits to go on, determining which plants they belonged to required a significant amount of investigative research.

“It didn’t really fit well into any known plant group,” said lead author Rachel Reback, who studied the fossils while working as an undergraduate researcher at the Florida Museum. “We ended up having to take a large number of CT scans not only of the fossils we had but of the fruit of living species as well so that we could directly compare them.”

The researchers ultimately determined the fossils belonged to the spurge family by studying similar fruit specimens provided by the Smithsonian Institution. However, one of the fossils was so unlike anything they’d seen, they determined it represented an entirely new species belonging to the fossil genus Euphorbiotheca.

The orientation of fibers inside the fruit indicated they were likely explosive, a common means of seed dispersal in other euphorbs, including cassava, rubber trees, crown of thorns and castor oil plant. Once the fruit in these species has ripened, they begin to dry out, losing as much as 64% of their original weight, which builds up tension in the rigid outer layers. Once enough water has evaporated, “You hear this loud pop, and the seeds and pieces of the fruit go flying everywhere,” Manchester said, describing the process in rubber trees. “We think this is the case for these two fossil species as well, because we see the same anatomy, where the fibers in the inner and outer layers of the fruit wall are oriented in opposing directions, which helps build torque.”

India an incubation chamber for new groups and species

Fossils like these offer paleontologists tantalizing clues regarding the origin and movement of species. About 140 million years ago, a conjoined India and Madagascar began drifting away from the supercontinent Gondwana in the Southern Hemisphere, carrying with them plants and animals that evolved in isolation throughout the Cretaceous.

By the time India finally slammed into Eurasia, 10 million years after the extinction of the dinosaurs, it had given rise to an incredible diversity of life found nowhere else. It’s likely the first grapes evolved in India, as did the ancestors of whales. As the Himalayas took shape above the sutured landmasses, new groups of insect-eating pitcher plants, flightless birds, lizards, freshwater crabs, scorpions and praying mantises all made their way out of India and into new environments in Europe and Asia.

Manchester hopes these fossils and others like them coming out of the Deccan Traps will help illuminate the distribution of species at a critical time in Earth’s history. “What were the environments in India like at a time when it had not yet connected to Eurasia and how do they compare with other regions at that time?” he said. “It’s like filling in the pieces of a puzzle.”

The team published its results in the International Journal of Plant Sciences.

  1. Rachel G. Reback, Dashrath K. Kapgate, Ken Wurdack, Steven R. Manchester. Fruits of Euphorbiaceae from the Late Cretaceous Deccan Intertrappean Beds of IndiaInternational Journal of Plant Sciences, 2022; 183 (2): 128 DOI: 10.1086/717691
  2. Source: www.sciencedaily.com/releases/2022/02/220217102028.htm

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: Ankylosaur was sluggish and deaf?

@WFS,World Fossil Society,Riffin T Sajeev, Russel T Sajeev

Ankylosaurs could grow up to eight meters in body length and represent a group of herbivorous dinosaurs, also called ‘living fortresses’: Their body was cluttered with bony plates and spikes. Some of their representatives, the ankylosaurids sometimes possessed a club tail, while nodosaurids had elongated spikes on their necks and shoulders. However, some aspects of their lifestyle are still puzzling.

(A) Outline drawing of Austria with a star marking Muthmannsdorf, the type locality of Struthiosaurus austriacus. (B) Silhouette of Struthiosaurus austriacus (measuring 2.7 m in length here; copyright: Fabrizio De Rossi) and a human for comparison. Photographs (C,D,G,J) and ambient occlusion photogrammetric models (E,F,H,I,K) of the holotype specimen of Struthiosaurus austriacus, IPUW 2349/6, in (C,E) right lateral, (D,F) left lateral, (I) anterior, (J,K) ventral and (G,H) posterior views. a, armour; bo, basioccipital; bs, basisphenoid; bt, basal tuber; ct, crista tuberalis; d, damage; fm, foramen magnum; fo/cr, fenestra ovalis/columellar recess; met, metotic foramen; pbp, posterior branching plexus; sg, stapedial groove; st/pit, sella turcica/pituitary; tov, transverso-occipital vein; uvd, uncertain vascular duct; V3/icg, groove for the mandibular branch of the trigeminal nerve or for the internal carotid; VI, abducens nerve; VII, facial nerve; vcm, dorsal middle cerebral vein; XII, hypoglossal nerve

(A) Outline drawing of Austria with a star marking Muthmannsdorf, the type locality of Struthiosaurus austriacus. (B) Silhouette of Struthiosaurus austriacus (measuring 2.7 m in length here; copyright: Fabrizio De Rossi) and a human for comparison. Photographs (C,D,G,J) and ambient occlusion photogrammetric models (E,F,H,I,K) of the holotype specimen of Struthiosaurus austriacus, IPUW 2349/6, in (C,E) right lateral, (D,F) left lateral, (I) anterior, (J,K) ventral and (G,H) posterior views. a, armour; bo, basioccipital; bs, basisphenoid; bt, basal tuber; ct, crista tuberalis; d, damage; fm, foramen magnum; fo/cr, fenestra ovalis/columellar recess; met, metotic foramen; pbp, posterior branching plexus; sg, stapedial groove; st/pit, sella turcica/pituitary; tov, transverso-occipital vein; uvd, uncertain vascular duct; V3/icg, groove for the mandibular branch of the trigeminal nerve or for the internal carotid; VI, abducens nerve; VII, facial nerve; vcm, dorsal middle cerebral vein; XII, hypoglossal nerve

While many dinosaurs likely lived in groups, at least some ankylosaurs seemed to prefer a lonesome life because of an inferior sense of hearing. That’s what the scientists from the universities of Greifswald and Vienna concluded when they examined the braincase of the Austrian dinosaur with a high-resolution computer tomograph to produce a digital three-dimensional cast.

Fossil braincases, which once housed the brain and other neurosensory tissues, are rare but important for science because these structures can provide insights into the lifestyle of a given animal. For example, the inner ears can hint to auditory capacities and skull orientation.

Struthiosaurus austriacus is a comparably small nodosaurid from the Late Cretaceous (80 Ma) of Austria and comes from a locality near Muthmannsdorf, south of Vienna. The fossil remains of this dinosaur already belonged to the collection of the Institute for Paleontology in Vienna in the 19th century. For their study, Marco Schade (University of Greifswald), Cathrin Pfaff (University of Vienna) and their colleagues examined the tiny (50 mm) braincase to reveal new details of the anatomy and lifestyle of Struthiosaurus austriacus. With these data, it was possible to learn more about its sense of equilibrium and audition.

The results of this study show that Struthiosaurus’ brain was very similar to the brains of its close relatives. For example, the flocculus, an evolutionary old part of the brain, was very small. The flocculus is important for the fixation of the eyes during motions of the head, neck and whole body, which can be very useful if such an animal was trying to target potential competitors or aggressors. “In contrast to its Northamerican relative Euoplocephalus, which had a tail club and a clear flocculus on the brain cast, Struthiosaurus austriacus may rather relied on its body armor for protection,” says Marco Schade. Together with the form of the semicircular canals in the inner ear, this hints towards an exceptionally sluggish lifestyle of this Austrian plant eater. Furthermore, the scientists found the — so far — shortest lagena of a dinosaur. The lagena is the part of the inner ear where audition takes place and its size can help to infer auditory capacities. This study delivers new insights into the evolutionary history of dinosaurs and their world, in which Europe was largely submerged in the ocean.

Citation : Marco Schade, Sebastian Stumpf, Jürgen Kriwet, Christoph Kettler, Cathrin Pfaff. Neuroanatomy of the nodosaurid Struthiosaurus austriacus (Dinosauria: Thyreophora) supports potential ecological differentiations within AnkylosauriaScientific Reports, 2022; 12 (1) DOI: 10.1038/s41598-021-03599-9

Source:  www.sciencedaily.com

@WFS,World Fossil Society,Riffin T Sajeev, Russel T Sajeev

WFS News: A giant millipede 326 million years old found

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Scientists say they have discovered the largest-ever fossil of a giant millipede on a beach in Northumberland, totally by chance.

The millipede, known as Arthropleura, is thought to have been more than 2.5m (8ft) long. It would have weighed about 50kg (eight stone).

The fossil segment was first spotted in 2018 when a large block of sandstone fell on to a beach at Howick Bay.

It will be displayed in Cambridge’s Sedgwick Museum next year.

“It was a complete fluke of a discovery,” said Dr Neil Davies, from Cambridge’s Department of Earth Sciences, who has been analysing the 75cm-long fossil.

“The way the boulder had fallen, it had cracked open and perfectly exposed the fossil, which one of our former PhD students happened to spot when walking by,” Dr Davies said.

When the giant millipede lived, 326 million years ago, the north-east of England had a much more tropical climate than today.

Largest ever Millipede Fossil

This specimen was found in what researchers believe was an old river channel. It may well not actually be the fossil of a dead creature, but an exoskeleton that was shed as the massive millipede grew.

“Finding these giant millipede fossils is rare, because once they died, their bodies tend to disarticulate, so it’s likely that the fossil is a moulted carapace that the animal shed as it grew,” said Mr Davies. “We have not yet found a fossilised head, so it’s difficult to know everything about them.”

One thing that can be said with certainty is, that in common with almost all millipedes, it did not have 1,000 legs – the researchers believe it had at least 32, but it may have been up to 64.

This fossil is just the third Arthropleura to be discovered, and is far older and larger than the two previous specimens which were both found in Germany.

The researchers believe that to get to such a large size, Arthropleura must have had a high-nutrient diet. That could have meant it supplementing a diet of nuts and seeds with small creatures and amphibians.

The fossil is due to go on public display in Cambridge in the new year.

A paper analysing the discovery has been published in the Journal of the Geological Society.

Source: Article by By Jonah Fisher,Environment Correspondent,BBC News

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: New fossils of Australopithecus sediba reveal a nearly complete lower back

@WFS,World Fossil Society,Riffin T Sajeev,Russel Sajeev

The lower back of Malapa Hominin 2 in ventral (left) and dorsal (right) views. New second and third lumbar vertebrae (U.W.88–232, U.W.88–233) are positioned at the top, and U.W.88–234 contributes to the upper portion of the fourth lumbar vertebra (U.W.88–127/153/234). The fifth lumbar vertebra (U.W.88–126/138) sits atop the sacrum (U.W.88–137/125). The lower back elements are preserved together in four blocks, each containing multiple elements held together in matrix and/or in partial articulation: (1) The vertebral body fragment of L1 (U.W.88–280) is preserved within the matrix of a block containing the lower thoracic vertebrae (U.W.88–43/114 and U.W.88–44) (Figure 2—figure supplement 1, Figure 3—figure supplement 1); (2) L1 inferior neural arch (U.W.88–281; concealed in matrix), L2 (U.W.88–232), L3 (U.W.88–233), and upper neural arch of L4 (U.W.88–234); (3) the L4 (U.W.88–127) and L5 (U.W.88–126) vertebral bodies, and partial S1 body (U.W.88–125); (4) most of the sacrum (U.W.88–137), the neural arch of L5 (U.W.88–153), the inferior portion of the neural arch of L4 (U.W.88–138).

The lower back of Malapa Hominin 2 in ventral (left) and dorsal (right) views.
New second and third lumbar vertebrae (U.W.88–232, U.W.88–233) are positioned at the top, and U.W.88–234 contributes to the upper portion of the fourth lumbar vertebra (U.W.88–127/153/234). The fifth lumbar vertebra (U.W.88–126/138) sits atop the sacrum (U.W.88–137/125). The lower back elements are preserved together in four blocks, each containing multiple elements held together in matrix and/or in partial articulation: (1) The vertebral body fragment of L1 (U.W.88–280) is preserved within the matrix of a block containing the lower thoracic vertebrae (U.W.88–43/114 and U.W.88–44) (Figure 2—figure supplement 1, Figure 3—figure supplement 1); (2) L1 inferior neural arch (U.W.88–281; concealed in matrix), L2 (U.W.88–232), L3 (U.W.88–233), and upper neural arch of L4 (U.W.88–234); (3) the L4 (U.W.88–127) and L5 (U.W.88–126) vertebral bodies, and partial S1 body (U.W.88–125); (4) most of the sacrum (U.W.88–137), the neural arch of L5 (U.W.88–153), the inferior portion of the neural arch of L4 (U.W.88–138).

Adaptations of the lower back to bipedalism are frequently discussed but infrequently demonstrated in early fossil hominins. Newly discovered lumbar vertebrae contribute to a near-complete lower back of Malapa Hominin 2 (MH2), offering additional insights into posture and locomotion in Australopithecus sediba. We show that MH2 possessed a lower back consistent with lumbar lordosis and other adaptations to bipedalism, including an increase in the width of intervertebral articular facets from the upper to lower lumbar column (‘pyramidal configuration’). These results contrast with some recent work on lordosis in fossil hominins, where MH2 was argued to demonstrate no appreciable lordosis (‘hypolordosis’) similar to Neandertals. Our three-dimensional geometric morphometric (3D GM) analyses show that MH2’s nearly complete middle lumbar vertebra is human-like in overall shape but its vertebral body is somewhat intermediate in shape between modern humans and great apes. Additionally, it bears long, cranially and ventrally oriented costal (transverse) processes, implying powerful trunk musculature. We interpret this combination of features to indicate that A. sediba used its lower back in both bipedal and arboreal positional behaviors, as previously suggested based on multiple lines of evidence from other parts of the skeleton and reconstructed paleobiology of A. sediba.

Cite this articleas: eLife 2021;10:e70447 DOI: 10.7554/eLife.70447

@WFS,World Fossil Society,Riffin T Sajeev,Russel Sajeev

WFS News: Reconstructing the dragonfly and damselfly family tree

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Many people hate insects, but the iridescent colors and elegant flying style of dragonflies and damselflies have made them firm favorites worldwide. They have been around in some form for hundreds of millions of years, but the evolutionary history of these relics of prehistoric life has been poorly understood — until now.

In newly published study, researchers including a member of the University of Tsukuba have applied transcriptomics, a type of gene sequencing, to reconstruct the phylogeny of the insect order Odonata. By calibrating this sequencing using the fossil record, they have been able to determine when dragonflies and damselflies first emerged.

Transcriptomics is the study of the collection of ribonucleic acid (RNA) — known as the transcriptome — that is present in a cell at any given time. This RNA contains a wealth of information and can be used to determine relationships among different members of a species. Understanding these relationships is essential for reconstructing evolutionary histories, or phylogenies, which are essentially like a family tree in a genetic sense.

“This is the first transcriptome-based phylogenetic reconstruction of the order Odonata,” says one of the authors of the study Professor Ryuichiro Machida. “We analyzed a total of 2,980 protein-coding genes in 105 species, covering all but two of the order’s families.”

There are thousands of living (extant) species of Odonata, but few have been analyzed in a phylogenetic context, and most species have been identified or differentiated on the basis of physical characteristics, such as wing patterns or larvae appearance. Although comparing appearances can be useful for extant species, it’s not always as helpful when trying to reconstruct evolutionary histories — that’s where transcriptomics and fossil calibration are useful.

“A robust and reliable phylogenetic reconstruction is essential for dependable estimates of species divergence times,” explains Machida. “Different fossil calibration schemes can be applied, but these can greatly impact the range of estimated dates. We used a comprehensive fossil dataset combining newly assessed fossils with data from the literature to produce a well-resolved and robustly time-calibrated phylogeny for Odonata.”

This reconstruction provides the most comprehensive divergence time estimates for Odonata to date, meaning the researchers were able to determine when dragonflies and damselflies first appeared (around 200 million years ago). They were even able to estimate the time at which certain evolutionary characteristics developed, such as ovipositors (tube-shaped organs for laying eggs). Species that once flourished but have since died out were also identified. Given that these species can now only be identified in the fossil record, transcriptomics and phylogenetic reconstructions provide a unique opportunity to better understand the connections between extant and extinct species. Studies of a similar nature could shed light on equally obscured genetic histories for other species.

  1. Manpreet Kohli, Harald Letsch, Carola Greve, Olivier Béthoux, Isabelle Deregnaucourt, Shanlin Liu, Xin Zhou, Alexander Donath, Christoph Mayer, Lars Podsiadlowski, Simon Gunkel, Ryuichiro Machida, Oliver Niehuis, Jes Rust, Torsten Wappler, Xin Yu, Bernhard Misof, Jessica Ware. Evolutionary history and divergence times of Odonata (dragonflies and damselflies) revealed through transcriptomicsiScience, 2021; 103324 DOI: 10.1016/j.isci.2021.103324
University of Tsukuba. “Linking the past and present: Reconstructing the dragonfly and damselfly family tree.” ScienceDaily. ScienceDaily, 29 October 2021. <www.sciencedaily.com/releases/2021/10/211029114012.htm>.
@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: A New Genus and Species of Grass, Eograminis balticus (Poaceae: Arundinoideae), in Baltic Amber

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Amber research by the Oregon State University College of Science has produced the first definite identification of grass in fossilized tree resin from the Baltic region, home to the world’s most well-known amber deposits.

Side one view of Eograminis balticus gen. et sp. nov. in Baltic amber. The arrow indicates callus hairs. Scale bar = 1.0 mm. The inset shows details of the callus hairs (arrowhead). Scale bar = 0.3 mm.

Side one view of Eograminis balticus gen. et sp. nov. in Baltic amber. The arrow indicates callus hairs. Scale bar = 1.0 mm. The inset shows details of the callus hairs (arrowhead). Scale bar = 0.3 mm.

The specimen studied by George Poinar Jr., named Eograminis balticus, also represents the first fossil member of Arundinoideae, a subfamily of the widespread Poaceae family that includes cereal grasses, bamboos and many species found in lawns and natural grasslands.

Findings, now in preprint, will be published in the International Journal of Plant Sciences.

Blown or shoved against a resin-producing tree, the fossil grass lost one of its spikelets some 40 or 50 million years ago, along with an accompanying insect that had been feeding on it.

Detail of silica bodies (arrows) in the tip of a lemma of Eograminis balticus gen. et sp. nov. in Baltic amber. Scale bar = 13 μm

A spikelet is one unit of inflorescence, or flower arrangement, and consists of two glumes and one or more florets. A glume is a leaflike structure below the flower cluster, and a floret is one of the small flowers in the cluster.

The fossil spikelet is the first definite evidence that grasses were among the various plants in the Baltic amber forest.

“The discovery not only adds a new plant group to the extensive flora that have been described from Baltic amber but provides new insights into the forest habitat the amber came from, a controversial topic in this field of study,” said Poinar, an international expert in using plant and animal life forms preserved in amber to learn more about the biology and ecology of the distant past.

Poinar says some scientists have proposed that fossiliferous amber from the Baltic region was formed in tropical and subtropical woods, and others say it came from a humid, marshy, warm-temperate forest.

“Our new grass suggests that for at least a time the habitat was warm-temperate, like you see today in mixed deciduous and conifer forests,” said Poinar, who collaborated on the study with Roberg Soreng of the Smithsonian Institution. “Present on the spikelet is an immature grasshopper-like insect and a leaf-spot fungal spore that provide information on the microhabitat of the fossil grass. The spikelet has structural and developmental features that existed in early Cenozoic grasses and establishes an important calibration point for future studies on the origin and splitting of genera in its subtribe.”

Because of the excellent preservation of the spikelet, observations could be made under direct light with both stereoscopic and compound microscopes, Poinar said.

“The spikelet has some features of members of the extant wetland genus Molinia in the tribe Molinieae, subtribe Moliniinae,” Poinar said. “Molinia species are concentrated around the Baltic Sea, but some of those species’ characteristics are different from what we see in this fossil.”

Informally known as moor grass, Molinia is a wetland genus. In addition to the Baltic region, Molinia is found in sand in habitats ranging from coastal to subalpine, and in fens and sphagnum bogs in forests. A fen is a peat-accumulating wetland that is fed by surface or ground water rich in minerals.

The Eograminis balticus spikelet specimen originated from the Samland Peninsula in the Kalinin District of the Russian Federation, Poinar said.

The name of the genus derives from the Latin words for age (aeon) and grass (graminis).

Journal Reference:

  1. George Poinar, Robert J. Soreng. A New Genus and Species of Grass, Eograminis balticus (Poaceae: Arundinoideae), in Baltic AmberInternational Journal of Plant Sciences, 2021; 000 DOI: 10.1086/716781
Oregon State University. “Grass found in Baltic amber.” ScienceDaily. ScienceDaily, 4 October 2021. <www.sciencedaily.com/releases/2021/10/211004104246.htm>
@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News:The Horseshoe Crab of the Genus Limulus: Living Fossil or Stabilomorph?

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

The Horseshoe Crab of the Genus Limulus: Living Fossil or Stabilomorph?

Citation: Kin A, Błażejowski B (2014) The Horseshoe Crab of the Genus Limulus: Living Fossil or Stabilomorph? PLoS ONE 9(10): e108036. https://doi.org/10.1371/journal.pone.0108036

Editor: Alistair Robert Evans, Monash University, Australia

A new horseshoe crab species, Limulus darwini, is described from the uppermost Jurassic (ca. 148 Ma) near-shore sediments of the Kcynia Formation, central Poland. The only extant species Limulus polyphemus (Linnaeus) inhabits brackish-marine, shallow water environments of the east coast of the United States. Here it is shown that there are no important morphological differences between the Kcynia Formation specimens and extant juvenile representatives of the genus Limulus. The palaeoecological setting inhabited by the new species and the trophic relationships of extant horseshoe crabs are discussed in an attempt to determine the potential range of food items ingested by these Mesozoic xiphosurans. In this paper we propose the adoption of a new term stabilomorphism, this being: an effect of a specific formula of adaptative strategy among organisms whose taxonomic status does not exceed genus-level. A high effectiveness of adaptation significantly reduces the need for differentiated phenotypic variants in response to environmental changes and provides for long-term evolutionary success.

Comparison of modern Limulus polyphemus (left) and oldest known member of the genus Limulus darwini (right) from Corbulomima horizon of unit III from Late Jurassic (upper Tithonian = Middle Volgian) sedimentary sequence at Owadów-Brzezinki Quarry (central Poland). (X), (Y) and (Z) - details emphasized, are most substantial morphological difference between both these forms. (cl) - cardiac lobe; (opr) – opisthosomal rim; (pa) – posterial area. Morphological elements of L. darwini exoskeleton not known from the fossil record (i.e. movable spines and telson) emphasized in grey.

Comparison of modern Limulus polyphemus (left) and oldest known member of the genus Limulus darwini (right) from Corbulomima horizon of unit III from Late Jurassic (upper Tithonian = Middle Volgian) sedimentary sequence at Owadów-Brzezinki Quarry (central Poland).(X), (Y) and (Z) – details emphasized, are most substantial morphological difference between both these forms. (cl) – cardiac lobe; (opr) – opisthosomal rim; (pa) – posterial area. Morphological elements of L. darwini exoskeleton not known from the fossil record (i.e. movable spines and telson) emphasized in grey.

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: Taytalura alcoberi, Fossil of Tuatara-Like Reptile

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

Taytalura alcoberi lived in what is now Argentina during the Late Triassic epoch, approximately 231 million years ago.

The ancient reptile was a member of Lepidosauromorpha, a large group that includes squamates (lizards and snakes) and sphenodontians (tuataras).

“Lepidosauromorphs and archosauromorphs represent the two main branches of the reptile tree of life that have survived to the present,” said Dr. Ricardo Martínez from the Instituto y Museo de Ciencias Naturales at the Universidad Nacional de San Juan and his colleagues.

“Today, the former mostly comprise squamates (about 11,000 species of lizards, snakes and amphisbaenians) and the latter are mostly represented by birds (about 10,800 species).”

“However, unlike for archosauromorphs, the early evolution of lepidosauromorphs remains one of the largest knowledge gaps in reptile evolution.”

Holotype of Taytalura alcoberi. Image credit: Martínez et al., doi: 10.1038/s41586-021-03834-3.

Holotype of Taytalura alcoberi. Image credit: Martínez et al., doi: 10.1038/s41586-021-03834-3.

Taytalura alcoberi predates the split between squamates and sphenodontians, and is close to the origin of lepidosauromorphs.

The species is about 11 million years younger than the oldest known lepidosauromorphs from Europe, and approximately the same age as the oldest known South American lepidosauromorphs.

The skull of Taytalura alcoberi shares features with modern tuataras, suggesting that several anatomical features, presumed exclusive to sphenodontians, must have originated early in lepidosauromorph evolution.

Taytalura alcoberi suggests that the strongly evolutionarily conserved skull architecture of sphenodontians represents the plesiomorphic condition for all lepidosaurs, that stem and crown lepidosaurs were contemporaries for at least 10 million years during the Triassic period, and that early lepidosauromorphs had a much broader geographical distribution than has previously been thought,” the paleontologists said.

Their paper was published in the journal Nature.

Source: http://www.sci-news.com/

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

WFS News: Sustained high rates of morphological evolution during the rise of tetrapods

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

One of the biggest questions in evolution is when and how major groups of animals first evolved. The rise of tetrapods (all limbed vertebrates) from their fish relatives marks one of the most important evolutionary events in the history of life. This “fish-to-tetrapod” transition took place somewhere between the Middle and Late Devonian (~400-360 million years ago) and represents the onset of a major environmental shift, when vertebrates first walked onto land. Yet, some of the most fundamental questions regarding the dynamics of this transition have remained unresolved for decades.

In a study published August 23 in Nature Ecology and Evolution Harvard researchers establish the origin date of the earliest tetrapods and discover they acquired several of the major new adaptive traits that enabled vertebrate life on land at accelerated evolutionary rates.

The study led by Dr. Tiago R. Simões, postdoctoral researcher, and senior author Professor Stephanie E. Pierce, both from the Department of Organismic and Evolutionary Biology, Harvard University, applied recently developed statistical methods (Bayesian evolutionary analysis) to precisely estimate the time and rates of anatomical evolution during the rise of tetrapods. The Bayesian method was adapted from methods originally developed in epidemiology to study how viruses like COVID-19 evolve and only recently became a tool in paleontology for the study of species evolution.

The study also innovates by combining data from fossil footprints and body fossils to pinpoint the time of origin of the tetrapods. “Normally footprint data shows up after body fossils of their track makers. In this case, we have tetrapod footprints much older than the first body fossils by several million years, which is extremely unusual. By combining both footprint and body fossils, we could search for a more precise age for the rise of tetrapods,” said Pierce.

“We were able to provide a very precise age for the origin of tetrapods at approximately 390 million years ago, 15 million years older than the oldest tetrapod body fossil,” said Simões.

The researchers also found that most of the close relatives to tetrapods had exceptionally slow rates of anatomical evolution, suggesting the fish relatives to tetrapods were quite well adapted to their aquatic lifestyle.

“On the other hand, we discovered the evolutionary lineages leading to the first tetrapods broke away from that stable pattern, acquiring several of the major new adaptive traits at incredibly fast rates that were sustained for approximately 30 million years,” said Simões.

Simões and Pierce also extended molecular approaches to study how fast different parts of the early tetrapod body plan evolved — such as the skull, jaws, and limbs — and the strength of natural selection acting on each of them. They found that all parts of the tetrapod skeleton were under strong directional selection to evolve new adaptive features, but that the skull and jaws were evolving faster than the rest of the body, including the limbs.

“This suggest that changes in the skull had a stronger role in the initial stages of the fish-to-tetrapod transition than changes in the rest of the skeleton. The evolution of limbs to life on land was important, but mostly at a later stage in tetrapod evolution, when they became more terrestrial,” said Pierce.

“We see several anatomical innovations in their skull related to feeding and food procurement, enabling a transition from a fish-like suction-based mode of prey capture to tetrapod-like biting, and an increase in orbit size and location” said Simões. “These changes prepared tetrapods to look for food on land and to explore new food resources not available to their fish relatives.”

The researchers also found that the fast rates of anatomical evolution in the tetrapod lineage were not associated with fast rates of species diversification. In fact, there were very few species around, so few they had a very low probability of being preserved in the fossil record.

This finding helps to answer an ongoing debate in evolution of whether new major animal groups originated under fast rates of anatomical change and species diversification (the classical hypothesis). Or, if there were high rates of anatomical evolution first, with increased rates of species diversification occurring only several million years later (a new hypothesis).

“What we’ve been finding in the last couple of years is that you have lots of anatomical changes during the construction of new animal body plans at short periods of geological time, generating high rates of anatomical evolution, like we’re seeing with the first tetrapods. But in terms of number of species, they remained constrained and at really low numbers for a really long time, and only after tens of millions of years do they actually diversify and become higher in number of species. There’s definitely a decoupling there,” said Simões.

Pierce agreed, “It takes time to get a foothold in a new niche in order to take full advantage of it.”

“Our study starts at the very beginning of this evolutionary story. There are many, many more chapters to come,” said Pierce. “We want to next dig further in terms of what happened after the origin of tetrapods, when they started to colonize land and diversify into new niches. How does that impact their anatomical rates of evolution compared to their species diversification across the planet? This is just the very beginning. It’s the introductory chapter to the book.”

  1. Tiago R. Simões, Stephanie E. Pierce. Sustained high rates of morphological evolution during the rise of tetrapodsNature Ecology & Evolution, 2021; DOI: 10.1038/s41559-021-01532-x
Harvard University, Department of Organismic and Evolutionary Biology. “Sustained fast rates of evolution explain how tetrapods evolved from fish.” ScienceDaily. ScienceDaily, 23 August 2021. <www.sciencedaily.com/releases/2021/08/210823125839.htm>.
@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev