WFS News: Scientists discover an ancient whale with a Pokémon face and a predator bite

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Long before whales were majestic, gentle giants, some of their prehistoric ancestors were tiny, weird and feral. A chance discovery of a 25 million-year-old fossil on an Australian beach has allowed paleontologists to identify a rare, entirely new species that could unlock mysteries of whale evolution.

Researchers this week officially named Janjucetus dullardi, a cartoonish creature with bulging eyes the size of tennis balls, in the Zoological Journal of the Linnean Society. Unlike today’s whales, the juvenile specimen was small enough to fit in a single bed.

Boasting fiendish teeth and a shark-like snout, however, this oddball of the ocean was nasty, mean and built to hunt.

“It was, let’s say, deceptively cute,” said Erich Fitzgerald, senior curator of vertebrate paleontology at Museums Victoria Research Institute, and one of the paper’s authors.

“It might have looked for all the world like some weird kind of mash-up between a whale, a seal and a Pokémon but they were very much their own thing.”

Extinct species was an odd branch on the whale family tree

The rare discovery of the partial skull, including ear bones and teeth, was made in 2019 on a fossil-rich stretch of coast along Australia’s Victoria state. Jan Juc Beach, a cradle for some of the weirdest whales in history, is becoming a hotspot for understanding early whale evolution, Fitzgerald said.

Few family trees seem stranger than that of Janjucetus dullardi, only the fourth species ever identified from a group known as mammalodontids, early whales that lived only during the Oligocene Epoch, about 34 to 23 million years ago. That marked the point about halfway through the known history of whales.

The tiny predators, thought to have grown to 3 meters (10 feet) in length, were an early branch on the line that led to today’s great baleen whales, such as humpbacks, blues and minkes. But the toothy ancestors with powerful jaws would have looked radically different to any modern species.

That mystery will remain tantalizingly unsolved unless a specimen is uncovered with more of its skeleton intact, which would be something of a miracle. Even the partial skull that allowed the initial identification this week was an astonishing discovery.

For an amateur paleontologist, a life-long obsession paid off

Janjucetus dullardi was named by researchers after an amateur fossil hunter who doesn’t mind its looks in the slightest.

“It’s literally been the greatest 24 hours of my life,” said Ross Dullard, who discovered the skull while fossil hunting at Jan Juc Beach. After Wednesday’s confirmation of the new species, the school principal walked like a rock star onto campus with “high fives coming left, right and center,” he said.

His friends and family are probably just relieved it’s over.

“That’s all they’ve heard from me for about the last six years,” he said.

Dullard was on a regular low-tide hunt at Jan Juc the day he spotted something black protruding from a cliff. Poking it dislodged a tooth.

“I thought, geez, we’ve got something special here,” he said. Dullard sent photos to Museums Victoria, where Fitzgerald saw them and immediately suspected a new species.

Ancient whale finds are rare but significant

Confirming the find was another matter. This was the first mammalodontid to be identified in Australia since 2006 and only the third on record in the country.

Fossils of sufficient quality, with enough of the right details preserved to confirm uniqueness, aren’t common.

“Cetaceans represent a fairly miniscule population of all life,” Fitzgerald said. Millions of years of erosion, scavengers and ocean currents take their toll on whale skeletons too.

“It’s only the chosen few, the vast minority of all whales that have ever lived and died in the oceans over millions of years, that actually get preserved as fossils,” he added.

Finds such as Janjucetus dullardi can unlock insights into how prehistoric whales ate, moved, behaved — and evolved. Researchers said the discoveries also helped to understand how ancient cetacean species adapted to warmer oceans, as they study how today’s marine life might respond to climate change.

Meanwhile, Dullard planned to host a fossil party this weekend, featuring cetacean-themed games and whale-shaped treats in jello, to celebrate his nightmare Muppet find, finally confirmed.

“That’s taken my concentration for six years,” he said. “I’ve had sleepless nights. I’ve dreamt about this whale.”

Source : Article by CHARLOTTE GRAHAM-MCLAY,New Zealand and South Pacific reporter, APnews.com

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WFS News: A new dinosaur species discovered in China didn’t roar, it chirped like a bird

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ith each new discovery in paleontology, we are gradually moving away from the Hollywood-inspired image of dinosaurs popularized by the Jurassic Park series. One of the most striking shifts has been in how we envision their appearance. Rather than the tough-skinned reptilian giants depicted on screen, many dinosaurs are now believed to have been covered in feather-like structures similar to modern birds.

Scientists are now saying that a group of herbivorous,  tweeted like birds, instead of the expected roaring and growling, a suggestion based on the discovery of new fossilized dinosaur bones, which included parts of the voice box.

Researchers from China discovered and identified fossils of a 2-foot-long new dinosaur species, Pulaosaurus qinglong, named after “Pulao,” a mythical Chinese dragon known for its loud sound. The species belongs to Neornithischia, a subgroup of Ornithischia, which includes  with bird-like pelvic structures.

The fossils marked a significant find, as they became the first-ever neornithischian dinosaur specimen discovered in the Yanliao Biota—a world-renowned dinosaur fossil hotspot in northeastern China, dating to the Middle to Late Jurassic period, approximately 165–150 million years ago. The research findings are published in PeerJ.

Previous studies from the Yanliao Biota and the Asian region in general mostly focused on small theropods and early birds, with ornithischians receiving very little attention. The lack of a robust fossil record created a knowledge gap, making it difficult for researchers to trace back early diversification within Ornithischia.

The researchers in this study discovered a remarkably well-preserved fossil of an immature Pulaosaurus qinglong in the Upper Jurassic Tiaojishan Formation in Hebei Province, northern China. The fossil included a near-complete skeleton, comprising of vertebrae, limbs, pelvis, bones of the larynx or voice box, and even some rare soft tissue structures.

The researchers conducted a  to gain a better understanding of the evolutionary family tree of Pulaosaurus qinglong. The results indicated that it was among the earliest-known neornithischian dinosaurs ever discovered. Remarkably, it is also only the second dinosaur found with fossilized larynx bones, which allowed the researchers to take a closer look at sound production and vocalization in the dinosaur. The elongated, leaf-shaped, cartilage structures in Pulaosaurus’s larynx resembled those in , suggesting possible bird-like vocal abilities.

The scientists were also curious about the dietary habits of these dinosaurs. They examined the gut cavity and found small, round pebbles and tiny impressions, which could be interpreted as plant seeds or other plant material. The teeth, jaw and tongue structure indicated that Pulaosaurus preferred chomping on soft plant foods.

WFS News: Oldest physical evidence of butterflies or moths discovered in 236-million-year-old poop

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A team of paleontologists affiliated with several institutions in Argentina, working with a colleague from the U.K., has discovered evidence of scales from lepidopterans in dung samples recovered from a dig site in Talampaya National Park, Argentina. In their paper published in the Journal of South American Earth Sciences, the group describes how they found the scales in the dung samples and what the find means for scientists who study butterflies and moths.

In 2011, digging began at a site in Talampaya National Park. As the work unfolded, it was discovered that the site had once hosted an ancient communal latrine—many different animals had used the same place over and over to urinate or defecate, including many large plant-eating animals.

Dung samples were collected from the site and sent to various places for study. One such sample wound up in Argentina’s Regional Center for Scientific Research and Technology Transfer of La Rioja, which is where the researchers involved in this new study found it.

The team took the dung sample back to their lab and studied it in a variety of ways, finding it to be approximately 236 million years old, putting it in the middle of the Triassic, and just 16 million years after the close of the end-Permian extinction event that wiped out approximately 90% of all  on Earth. They also found tiny (200 microns long) scales that they were able to identify as from a lepidopteran, which is a moth or butterfly.

Prior research has suggested Lepidoptera first evolved approximately 241 million years ago, but  of them only went back to 201 million years ago, leaving a gap of approximately 40 million years. The new find by the team in Argentina may help to fill in missing data from that gap. It also meant the team may have found a new species—they gave it the name Ampatiri eloisae.

The timescale, the researchers note, suggests that the newly identified species likely belonged to a subgroup called Glossata, which meant it would have had a proboscis similar to those used by modern moths and butterflies. But there would have been a major difference—flowers did not exist during the Triassic. That means that A. eloisae would have had to get its nourishment from sugary droplets produced by conifer and cycad trees.

Source:Lucas E. Fiorelli et al, Back to the poop: the oldest hexapod scales discovered within a Triassic coprolite from Argentina, Journal of South American Earth Sciences (2025). DOI: 10.1016/j.jsames.2025.105584 and article by Bob Yirka.Phys.org

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WFS News: Duonychus tsogtbaatari , a Unique two-clawed dinosaur discovered

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Duonychus tsogtbaatari would have been adept at grasping vegetation

                       Duonychus tsogtbaatari would have been adept at grasping vegetation

A rare new species of two-clawed dinosaur has been discovered by scientists in Mongolia’s Gobi Desert.

The species, named Duonychus tsogtbaatari, was unique within a group of dinosaurs called Therizinosaurs, which stood on their hind legs and usually had three claws.

It was medium-sized, with an estimated weight of approximately 260kg.

Researchers believe the species’ long, curved claws and its ability to strongly flex them would have made it an efficient grasper of vegetation.

Researchers believe the dinosaur weighed approximately 260kg

                            Researchers believe the dinosaur weighed approximately 260kg

Therizinosaurs were a group of either herbivorous or omnivorous theropod dinosaurs that lived in Asia and North America during the Cretaceous Period, which began 145 million years ago and ended 66 million years ago.

They are exemplified by the massive, long-clawed form Therizinosaurus, featured in the film Jurassic World Dominion, and were “awkward looking”, according to one of the study’s authors Dr Darla Zelenitsky, associate professor at the University of Calgary.

The specimen was recovered from the Bayanshiree formation in the Gobi Desert of Mongolia, which dates back to the Late Cretaceous period (between 100.5 to 66 million years ago).

Unesco, the UN’s Educational, Scientific and Cultural Organization, calls the Mongolian Gobi Desert the largest dinosaur fossil reservoir in the world.

The region is an especially important source of fossils from the later Cretaceous period, which is the last of the main three periods of the dinosaur age, representing the final phase of dinosaur evolution.

The claws may also have been used as formidable weapons

                           The claws may also have been used as formidable weapons

At nearly a foot long, the claws themselves were much larger than their underlying bone, the study revealed.

Besides better grasping, the two-fingered hands may have been used for display, digging, or as formidable weapons.

The most famous two-fingered theropods are species within the group tyrannosaurids, which includes Tyrannosaurus rex, but Duonychus evolved its two-fingered hands separately from them and from other two-fingered theropods.

The specimen also preserves the first keratinous sheath of a therizinosaur, an element that covers the claw much like human fingernails, aiding defence, movement, or prey catching.

Source: Article By Tim Dodd (Climate and science reporter) ,BBC.Com

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WFS News: Rare pterosaur fossil reveals crocodilian bite 76m years ago

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The fossilised neck bone of a flying reptile unearthed in Canada shows tell-tale signs of being bitten by a crocodile-like creature 76 million years ago, according to a new study published today [23 January] in the Journal of Palaeontology.

The juvenile pterosaur vertebra, discovered in Dinosaur Provincial Park, Alberta, bears a circular four-millimetre-wide puncture mark from a crocodilian tooth.

TMP 2023.012.0237 in dorsal (1, 7, 13), ventral (2, 8, 14), right lateral (3, 9, 15), left lateral (4, 10, 16), anterior (5, 11, 17), and posterior (6, 12, 18) views. Upper images (1–6) show bone surface color, middle images (7–12) are ammonium chloride powder-coated, lower images (13–18) are schematic line drawings. For the line drawings (13–18), light and medium gray indicates bone surface, hatches indicate broken bone surface, light stipples indicate matrix infill creating natural internal mold, and dark stipples indicate matrix infill with no specific form. apf, accessory pneumatic foramen; lpf, lateral pneumatic foramen; nc, neural canal; ns, neural spine; tr, trace (i.e., feeding trace/tooth mark).

TMP 2023.012.0237 in dorsal (1, 7, 13), ventral (2, 8, 14), right lateral (3, 9, 15), left lateral (4, 10, 16), anterior (5, 11, 17), and posterior (6, 12, 18) views. Upper images (1–6) show bone surface color, middle images (7–12) are ammonium chloride powder-coated, lower images (13–18) are schematic line drawings. For the line drawings (13–18), light and medium gray indicates bone surface, hatches indicate broken bone surface, light stipples indicate matrix infill creating natural internal mold, and dark stipples indicate matrix infill with no specific form. apf, accessory pneumatic foramen; lpf, lateral pneumatic foramen; nc, neural canal; ns, neural spine; tr, trace (i.e., feeding trace/tooth mark).

Researchers from the Royal Tyrrell Museum of Palaeontology (Canada), the University of Reading (UK) and the University of New England (Australia) say this rare evidence provides insight into predator-prey dynamics in the region during the Cretaceous Period.

The discovery was made during an international field course that took place in July 2023, led by Dr Brian Pickles from the University of Reading.

Ammonium chloride coated images (1, 2), CT-scan slice (3), and digital render (4) of TMP 2023.012.0237: (1) entire element in ventral view (anterior at right), with gray area approximating the missing portion; (2) detail of anterior end with tooth mark; (3, 4) outputs of CT-scan data: (3) two-dimensional slice through the tooth mark at plane indicated in 2.3; (4) solid three-dimensional render of the element. Solid vertical lines in (1, 2) show plane of slice in (3). Dashed lines in (3) show missing extent of bone surface at the point of the trace.

Ammonium chloride coated images (1, 2), CT-scan slice (3), and digital render (4) of TMP 2023.012.0237: (1) entire element in ventral view (anterior at right), with gray area approximating the missing portion; (2) detail of anterior end with tooth mark; (3, 4) outputs of CT-scan data: (3) two-dimensional slice through the tooth mark at plane indicated in 2.3; (4) solid three-dimensional render of the element. Solid vertical lines in (1, 2) show plane of slice in (3). Dashed lines in (3) show missing extent of bone surface at the point of the trace.

Dr Caleb Brown from the Royal Tyrrell Museum of Palaeontology is the lead author of the paper.

He said: “Pterosaur bones are very delicate — so finding fossils where another animal has clearly taken a bite is exceptionally uncommon. This specimen being a juvenile makes it even more rare.”

Dinosaur Provincial Park has produced some of the most important dinosaur fossil discoveries ever made.

The punctured vertebra belongs to a young Azhdarchid pterosaur (Cryodrakon boreas), with an estimated wingspan of two metres.

Adults of this species would have been as tall as a giraffe with a wingspan in the region of 10m.

The researchers used micro-CT scans and comparisons with other pterosaur bones to confirm the puncture is not a result of damage during fossilisation or excavation, but an actual bite.

Dr Brian Pickles from the University of Reading and co-author of the paper said: “Bite traces help to document species interactions from this period. We can’t say if the pterosaur was alive or dead when it was bitten but the specimen shows that crocodilians occasionally preyed on, or scavenged, juvenile pterosaurs in prehistoric Alberta over 70 million years ago.”

The paper also shows that this new bone documents the first evidence in North America of ancient crocodilians opportunistically feeding on these giant prehistoric flying reptiles. Other examples of Azhdarchid bones with possible crocodilian bites have previously been found in Romania.

Journal Reference: Caleb M. Brown, Phil R. Bell, Holly Owers, Brian J. Pickles. A juvenile pterosaur vertebra with putative crocodilian bite from the Campanian of Alberta, CanadaJournal of Paleontology, 2025; 1 DOI: 10.1017/jpa.2024.12

University of Reading. “Rare pterosaur fossil reveals crocodilian bite 76m years ago.” ScienceDaily. ScienceDaily, 23 January 2025. <www.sciencedaily.com/releases/2025/01/250123110253.htm>.
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WFS News: UK’s biggest ever dinosaur footprint site unearthed

These footprints were made 166 million years ago as a dinosaur walked across a lagoon

These footprints were made 166 million years ago as a dinosaur walked across a lagoon

The UK’s biggest ever dinosaur trackway site has been discovered in a quarry in Oxfordshire.

About 200 huge footprints, which were made 166 million years ago, criss-cross the limestone floor.

They reveal the comings and goings of two different types of dinosaurs that are thought to be a long-necked sauropod called Cetiosaurus and the smaller meat-eating Megalosaurus.

The longest trackways are 150m in length, but they could extend much further as only part of the quarry has been excavated.

“This is one of the most impressive track sites I’ve ever seen, in terms of scale, in terms of the size of the tracks,” said Prof Kirsty Edgar, a micropalaeontologist from the University of Birmingham.

“You can step back in time and get an idea of what it would have been like, these massive creatures just roaming around, going about their own business.”

The dinosaurs left their mark as they walked across a tropical lagoon

The dinosaurs left their mark as they walked across a tropical lagoon

The tracks were first spotted by Gary Johnson, a worker at Dewars Farm Quarry, while he was driving a digger.

“I was basically clearing the clay, and I hit a hump, and I thought it’s just an abnormality in the ground,” he said, pointing to a ridge where some mud has been pushed up as a dinosaur’s foot pressed down into the earth.

“But then it got to another, 3m along, and it was a hump again. And then it went another 3m – hump again.”

Another trackway site had been found nearby in the 1990s, so he realised the regular bumps and dips could be dinosaur footprints.

“I thought I’m the first person to see them. And it was so surreal – a bit of a tingling moment, really,” he told BBC News.

This summer, more than 100 scientists, students and volunteers joined an excavation at the quarry which features on the new series of Digging for Britain.

The team found five different trackways.

Four of them were made by sauropods, plant-eating dinosaurs that walked on four legs. Their footprints look a bit like an elephant’s – only much much bigger – these beasts reached up to 18m in length.

Another track is thought to have been created by a Megalosaurus.

“It’s almost like a caricature of a dinosaur footprint”, explained Dr Emma Nicholls, a vertebrate palaeontologist from the Oxford University Museum of Natural History.

“It’s what we call a tridactyl print. It’s got these three toes that are very, very clear in the print.”

The carnivorous creatures, which walked on two legs, were agile hunters, she said.

“The whole animal would have been 6-9m in length. They were the largest predatory dinosaurs that we know of in the Jurassic period in Britain.”

The environment they lived in was covered by a warm, shallow lagoon and the dinosaurs left their prints as they ambled across the mud.

“Something must have happened to preserve these in the fossil record,” said Prof Richard Butler, a palaeobiologist from the University of Birmingham.

“We don’t know exactly what, but it might be that there was a storm event that came in, deposited a load of sediments on top of the footprints, and meant that they were preserved rather than just being washed away.”

The team studied the trackways in detail during the dig. As well as making casts of the tracks, they took more than 20,000 photographs to create 3D models of both the complete site and individual footprints.

“The really lovely thing about a dinosaur footprint, particularly if you have a trackway, is that it is a snapshot in the life of the animal,” Prof Butler explained.

“You can learn things about how that animal moved. You can learn exactly what the environment that it was living in was like. So tracks give us a whole different set of information that you can’t get from the bone fossil record.”

One area of the site even reveals where the paths of a sauropod and megalosaurus once crossed.

The prints are so beautifully preserved that the team have been able to work out which animal passed through first – they believe it was the sauropod, because the front edge of its large, round footprint is slightly squashed down by the three-toed megalosaurus walking on top of it.

“Knowing that this one individual dinosaur walked across this surface and left exactly that print is so exhilarating,” said Dr Duncan Murdock from Oxford University.

“You can sort of imagine it making its way through, pulling its legs out of the mud as it was going.”

The future fate of the trackways hasn’t yet been decided but the scientists are working with Smiths Bletchington, who operate the quarry, and Natural England on options for preserving the site for the future.

They believe there could be more footprints, these echoes of our prehistoric past, just waiting to be discovered.

Source: article by Rebecca Morelle(Science Editor),Alison Francis (Senior Science Journalist), BBC.Com

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WFS News: platypterygiid ichthyosaur,98-Million-Year-Old Ichthyosaur Fossil Uncovered in New Zealand

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Paleontologists in New Zealand have discovered a partial skeleton of platypterygiid ichthyosaur dating to the Cretaceous period.

“Ichthyosaurs were a clade of secondarily aquatic marine reptiles that inhabited the seas for much of the Mesozoic Era, first appearing in the Early Triassic before their ultimate extinction at the Cenomanian-Turonian boundary,” said University of Canterbury paleontologist George Young and his colleagues.

A pair of Platypterygius sp. Image credit: Dmitry Bogdanov / CC BY 3.0.

A pair of Platypterygius sp. Image credit: Dmitry Bogdanov / CC BY 3.0.

“Cretaceous ichthyosaurs were once thought of as a group with low diversity and disparity resulting from a long-term decline since the Jurassic.”

“However, recent work has produced a growing body of evidence that Cretaceous ichthyosaurs were much more diverse than previously thought.”

“Ichthyosaur fossils were first recorded in New Zealand by von Haast in 1861 from Mt Potts in the central South Island,” they added.

“Over the subsequent 150 years, fossil material of ichthyosaurs has been recovered from the Triassic, Jurassic, and Cretaceous.”

The new New Zealand ichthyosaur was found in the Coverham area at the northern end of the Waiau Toa/Clarence valley.

The specimen is a disarticulated partial skeleton preserved within a concretion.

It dates back 98 million years ago to the Cretaceous period — approximately 4 million years before the final extinction of the ichthyosaurs.

“The material derives from a concretion that was found in situ within the Swale Siltstone Member of the Split Rock Formation, a siliciclastic unit deposited during the Cenomanian age and found throughout southern Marlborough and northernmost Canterbury in the New Zealand’s South Island,” the paleontologists said.

“All of New Zealand’s previously described Cretaceous ichthyosaur material comes from the North Island.”

The specimen is the most completely preserved individual ichthyosaur known from New Zealand.

It possesses a well-preserved pelvis and hindfin which have added to the known dataset of these elements which are so rarely preserved in Cretaceous species.

“Whilst the specimen is too fragmentary to formally name, this taxon shows an extreme reduction of the basioccipital extracondylar area, a scapula with a prominent acromion process and a strap-like scapula shaft, as well as a complete left pelvic girdle with an elongated depression on the anteroproximal face of the ischiopubis,” the researchers said.

They suggest that it is a late branching member of the platypterygiid ichthyosaurs, closely related to an Eastern Gondwanan species called Platypterygius australis and to many European Cretaceous ichthyosaurs.

However, it appears to be unrelated to the Cretaceous ichthyosaurs of Western Gondwana, suggesting potential regionalism amongst the Gondwanan Cretaceous ichthyosaur populations.

“The new New Zealand ichthyosaur adds to the known diversity of Gondwanan Cretaceous ichthyosaurs and may suggest a regionalized rather than cosmopolitan distribution of ichthyosaur populations around the margin of Cretaceous Gondwana,” the scientists conlcuded.

The findings appear in the Journal of Vertebrate Paleontology.

REFERENCE: George R.A. Young et al. A platypterygiid ichthyosaur from the Cenomanian of central New Zealand. Journal of Vertebrate Paleontology, published online October 30, 2024; doi: 10.1080/02724634.2024.2408391

Source : Article By Natali Anderson @sci.news.com

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WFS News: World’s oldest lizard wins fossil fight

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A storeroom specimen that changed the origins of modern lizards by millions of years has had its identity confirmed.

The tiny skeleton, unearthed from Triassic-aged rocks in a quarry near Bristol, is at least 205 million years old and the oldest modern-type lizard on record.

Recently, the University of Bristol team’s findings came under question, but fresh analysis, published today in Royal Society Open Science, proves that the fossil is related to modern anguimorphs such as anguids and monitors. The discovery shifts the origin of the whole lizard-snake group, called Squamata, back by 35 million years.

In the original study, Dr David Whiteside, Dr Sofia Chambi-Trowell and Professor Mike Benton, named the little critter Cryptovaranoides microlanius, meaning ‘hidden lizard, small butcher’ because of its identification as a lizard and its sharp teeth, probably used for cutting up prey animals for food. The Bristol team identified many anatomical features of the skull and skeleton that allowed them to place it well within Squamata, and even close to the Anguimorpha.

Figure 1. Images from the holotype NHMUK PV R36822 of C. microlanius, separate isolated bones referable to the taxon and a palatine of †Tanystropheus longobardicus for comparison. (a) Distal end of left humerus in anterior view exposed on the surface of the holotype rock showing an ectepicondylar and an entepicondylar foramen and the capitellum. (b) NHMUK PV 38911 isolated larger specimen of the distal end of left humerus of †Cryptovaranoides microlanius in (above) anterior and (below) posterior views showing similar features except the condyle of the capitellum. (c) Right maxilla, right vomer in ventral view, right septomaxilla in dorsal view and both premaxillae exposed on the surface of the holotype rock. (d) Scan of right septomaxilla in posteromedial view. (e) Scan of NHMUK PV R36822, mainly in ventral view, showing right lower jaw, orbitosphenoid, right jugal, right quadrate, basioccipital, sphenoid, anterior vertebrae and ribs as well as pectoral and forelimb bones. (f) Scan of left jugal in lateral view for comparison. (g,h) Fragment of right otoccipital from scan of NHMUK PV R36822 showing position of vagus foramen, in (g) medial and (h) lateral views. (i,j) NHMUK PV 38889, fragment of left exoccipital part of otoccipital in (i) lateral and (j) medial views, annotated to show vagus foramen. (k) Isolated right palatine NHMUK PV R 38916 of †Cryptovaranoides microlanius in ventral view, showing extent of the choanal sulcus (fossa). (l) Right palatine of †Tanystropheus longobardicus PIMUZ T 2484 showing position of choanal channel. Scale bars all 2 mm except (a) = 0.5 mm and (d) = 1 mm. Arrows show anterior.ant, anterior; at, atlas; ax, axis; ba, basioccipital; bi, bicapitate; cap, capitellum; cen, centrum; ch, choana; chn, channel; cv, cavity; ect, ectepicondyle; ent, entepecondyle (entepicondylar); fct, facet; fo, foramen (foramina); for, foramen; fos, fossa; hg, hypoglossal; hu, humerus (humeral); hyo, hyoid; in, intercentrum; ju, jugal; l., left; lj, lower jaw; msof, margin of suborbital fenestra; mx, maxilla (maxillary); ne, neural; od, odontoid; orbs, orbitosphenoid; oto, otoccipital; pcf, posterior of the choanal fossa; pm, premaxilla; posl, posterolateral; post, posterior; pmd, posteromedial; proc, process; pt, pterygoid; q, quadrate; r, right; ra, radius; raul, radioulnar; ri, rib; s, spine; sp, septomaxilla; sph, sphenoid; th, tooth (teeth); thr, tooth row; tr, trochlea; unc, unicapitate; vf, vagus foramen; vo, vomer (vomerine).

Figure 1. Images from the holotype NHMUK PV R36822 of C. microlanius, separate isolated bones referable to the taxon and a palatine of †Tanystropheus longobardicus for comparison. (a) Distal end of left humerus in anterior view exposed on the surface of the holotype rock showing an ectepicondylar and an entepicondylar foramen and the capitellum. (b) NHMUK PV 38911 isolated larger specimen of the distal end of left humerus of †Cryptovaranoides microlanius in (above) anterior and (below) posterior views showing similar features except the condyle of the capitellum. (c) Right maxilla, right vomer in ventral view, right septomaxilla in dorsal view and both premaxillae exposed on the surface of the holotype rock. (d) Scan of right septomaxilla in posteromedial view. (e) Scan of NHMUK PV R36822, mainly in ventral view, showing right lower jaw, orbitosphenoid, right jugal, right quadrate, basioccipital, sphenoid, anterior vertebrae and ribs as well as pectoral and forelimb bones. (f) Scan of left jugal in lateral view for comparison. (g,h) Fragment of right otoccipital from scan of NHMUK PV R36822 showing position of vagus foramen, in (g) medial and (h) lateral views. (i,j) NHMUK PV 38889, fragment of left exoccipital part of otoccipital in (i) lateral and (j) medial views, annotated to show vagus foramen. (k) Isolated right palatine NHMUK PV R 38916 of †Cryptovaranoides microlanius in ventral view, showing extent of the choanal sulcus (fossa). (l) Right palatine of †Tanystropheus longobardicus PIMUZ T 2484 showing position of choanal channel. Scale bars all 2 mm except (a) = 0.5 mm and (d) = 1 mm. Arrows show anterior.ant, anterior; at, atlas; ax, axis; ba, basioccipital; bi, bicapitate; cap, capitellum; cen, centrum; ch, choana; chn, channel; cv, cavity; ect, ectepicondyle; ent, entepecondyle (entepicondylar); fct, facet; fo, foramen (foramina); for, foramen; fos, fossa; hg, hypoglossal; hu, humerus (humeral); hyo, hyoid; in, intercentrum; ju, jugal; l., left; lj, lower jaw; msof, margin of suborbital fenestra; mx, maxilla (maxillary); ne, neural; od, odontoid; orbs, orbitosphenoid; oto, otoccipital; pcf, posterior of the choanal fossa; pm, premaxilla; posl, posterolateral; post, posterior; pmd, posteromedial; proc, process; pt, pterygoid; q, quadrate; r, right; ra, radius; raul, radioulnar; ri, rib; s, spine; sp, septomaxilla; sph, sphenoid; th, tooth (teeth); thr, tooth row; tr, trochlea; unc, unicapitate; vf, vagus foramen; vo, vomer (vomerine).

“We knew our paper would be controversial,” explained Dr Whiteside. “But we were confident that we had looked at every possible feature and compared it with everything we could.”

Professor Benton said: “We were therefore surprised, perhaps even shocked, that in 2023 another team of academics suggested that Cryptovaranoides was not a lizard or even a lizard relative, but in fact an archosauromorph, more closely related to crocodilians and dinosaurs.”

In checking their original work, and the questions posed in the rival paper, the Bristol team explored all the data, including the original specimen as well as the X-ray scans that show the details hidden within the rock. “We had the marvellous images from those CT scans as well as further access to the fossil which enabled us to check all their suggestions,” said Dr Chambi-Trowell. “We found that most of the concerns raised were wrong.”

Figure 2. Photographs and CT scan images of NHMUK PV R36822 holotype bones of †Cryptovaranoides microlanius and isolated quadrate, prefrontal and premaxillae. (a–c) Left side of holotype skull and lower jaw of †Cryptovaranoides microlanius. (a) Close-up of left lacrimal in medial view. (b) Left side of skull and lower jaw in medial view. (c) Computed tomography (CT) scan of left lacrimal in lateral view. (d) Holotype right quadrate CT scan in medial view. (e) Isolated left quadrate NHMUK PV R 37606 digitally removed from matrix. (f) CT scan image of holotype right pterygoid in ventromedial view. (g) CT scan of holotype left and right premaxillae in posteroventral views. (h) Isolated left premaxilla NHMUK PV R 38914 in posteroventral view. (i) Isolated right premaxilla NHMUK PV R 38913 in posterior view. (j) Isolated right prefrontal NHMUK PV R 38912 in medial view. (k) Lateral view of right prefrontal NHMUK PV R 38912 showing palpebral fossa. Scale bars all 2 mm except (a) which is 0.5 mm. Arrows show anterior. an, angular; ant, anterior; ar, articular; c, crest; con, condyle; conc, conch; cor, coronoid; ct, contact; den, dentary; dor, dorsal; ec, ectopterygoid; ep, epipterygoid; f, frontal; fct, facet; fo, foramen (foramina); fos, fossa; gr, groove; ju, jugal; l., left; lac, lacrimal; mar, missing anterior region; me, medial; mth, missing tooth; mx, maxilla (maxillary); nal, nasolacrimal; not, notch; olcw, olfactory chamber wall; pa, palatine; pal, palbebral; pm, premaxilla; post, posterior; proc, process; prf, prefrontal; pt, pterygoid; ram, ramus; re, resorption; q, quadrate; r, right; slf, shelf, th, tooth (teeth); trc, tract; ty, tympanic.

Figure 2. Photographs and CT scan images of NHMUK PV R36822 holotype bones of †Cryptovaranoides microlanius and isolated quadrate, prefrontal and premaxillae. (a–c) Left side of holotype skull and lower jaw of †Cryptovaranoides microlanius. (a) Close-up of left lacrimal in medial view. (b) Left side of skull and lower jaw in medial view. (c) Computed tomography (CT) scan of left lacrimal in lateral view. (d) Holotype right quadrate CT scan in medial view. (e) Isolated left quadrate NHMUK PV R 37606 digitally removed from matrix. (f) CT scan image of holotype right pterygoid in ventromedial view. (g) CT scan of holotype left and right premaxillae in posteroventral views. (h) Isolated left premaxilla NHMUK PV R 38914 in posteroventral view. (i) Isolated right premaxilla NHMUK PV R 38913 in posterior view. (j) Isolated right prefrontal NHMUK PV R 38912 in medial view. (k) Lateral view of right prefrontal NHMUK PV R 38912 showing palpebral fossa. Scale bars all 2 mm except (a) which is 0.5 mm. Arrows show anterior. an, angular; ant, anterior; ar, articular; c, crest; con, condyle; conc, conch; cor, coronoid; ct, contact; den, dentary; dor, dorsal; ec, ectopterygoid; ep, epipterygoid; f, frontal; fct, facet; fo, foramen (foramina); fos, fossa; gr, groove; ju, jugal; l., left; lac, lacrimal; mar, missing anterior region; me, medial; mth, missing tooth; mx, maxilla (maxillary); nal, nasolacrimal; not, notch; olcw, olfactory chamber wall; pa, palatine; pal, palbebral; pm, premaxilla; post, posterior; proc, process; prf, prefrontal; pt, pterygoid; ram, ramus; re, resorption; q, quadrate; r, right; slf, shelf, th, tooth (teeth); trc, tract; ty, tympanic.

Professor Benton added: “All the details of the skull, the jaws, the teeth, and the limb bones confirm that Cryptovaranoides is a lizard, not an archosauromorph.

“In our new paper, we provide great detail of every criticism made and we provide more photographs of the specimen and 3D images from the scans, so everyone can check the detail.”

Dr Whiteside concluded: “The result of all this had to be tested by a phylogenetic analysis.

“This is where we code hundreds of anatomical features in Cryptovaranoides and other modern and fossil lizards, as well as various archosauromorphs.

“We ran the analysis time after time, and it gave our original result, that the little Bristol reptile is indeed the world’s oldest modern-type lizard.”

Source : University of Bristol. “World’s oldest lizard wins fossil fight.” ScienceDaily. ScienceDaily, 26 November 2024. <www.sciencedaily.com/releases/2024/11/241126191725.htm

Ref: David I. Whiteside, Sofía A. V. Chambi-Trowell, Michael J. Benton. Late Triassic †Cryptovaranoides microlanius is a squamate, not an archosauromorphRoyal Society Open Science, 2024; 11 (11) DOI: 10.1098/rsos.231874

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WFS News: Rare whitefly fossils found in New Zealand shed light on ancient forest life

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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 study reveals rare whitefly insect fossils have been found in Miocene age crater lake sediments at Hindon Maar, near Dunedin.

Credit: Palaeobiodiversity and Palaeoenvironments (2024). DOI: 10.1007/s12549-024-00628-z

Credit: Palaeobiodiversity and Palaeoenvironments (2024). DOI: 10.1007/s12549-024-00628-z

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 where 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 color—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 fossilized,” 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 fossilized. It must have happened in rapid succession as the tiny insect fossils are exquisitely preserved.

“The  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  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% 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.”

REf: owita Drohojowska et al, 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

Provided by : University Of Otago , Source: Phys.org

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WFS News: Mbiresaurus raathi,a long-neck plant-eating dinosaur found in Zimbabwe

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Artistic reconstruction of Mbiresaurus raathi (in the foreground) with the rest of the Zimbabwean animal assemblage in the background. It includes two rhynchosaurs (at front right), an aetosaur (at left), and a herrerasaurid dinosaur chasing a cynodont (at back right)ANDREY ATUCHIN/VIRGINIA TECH

Artistic reconstruction of Mbiresaurus raathi (in the foreground) with the rest of the Zimbabwean animal assemblage in the background. It includes two rhynchosaurs (at front right), an aetosaur (at left), and a herrerasaurid dinosaur chasing a cynodont (at back right)
ANDREY ATUCHIN/VIRGINIA TECH

An international team of paleontologists have uncovered what they believe to be the oldest dinosaur skeleton ever discovered in Africa. The skeleton of the Mbiresaurus raathi — described as a long-neck plant-eating dinosaur — was found in northern Zimbabwe, according to a news release Wednesday from Virginia Tech. The Mbiresaurus raathi lived more than 230 million years ago, researchers said.

The Mbiresaurus raathi was about 6-feet-long, had a long tail, and weighed anywhere from 20 to 65 pounds. The Mbiresaurus raathi is considered a sauropodomorph, a long-necked dinosaur.

The mostly intact skeleton was found by Virginia Tech student Christopher Griffin and other paleontologists during two digs in Zimbabwe in 2017 and 2019. The international team of researchers who found the skeleton said its only missing parts were some of the hand and portions of the skull.

“The discovery of Mbiresaurus raathi fills in a critical geographic gap in the fossil record of the oldest dinosaurs, and shows the power of hypothesis-driven fieldwork for testing predictions about the ancient past,” Griffin said in a statement.

Based off their findings, the Mbiresaurus stood on two legs and had a relatively small head with serrated triangle-shaped teeth.

“These are Africa’s oldest-known definitive dinosaurs, roughly equivalent in age to the oldest dinosaurs found anywhere in the world.” Griffin said. “The oldest known dinosaurs — from roughly 230 million years ago, the Carnian Stage of the Late Triassic period — are extremely rare and have been recovered from only a few places worldwide, mainly northern Argentina, southern Brazil and India.”

Most of the Mbiresaurus skeleton is being kept in Virginia Tech’s Derring Hall to be cleaned and studied. However, it will eventually be transferred to the Natural History Museum of Zimbabwe in Bulawayo, along with any additional fossils found in the area, the university said.

“The fact that the Mbiresaurus skeleton is almost complete makes it a perfect reference material for further finds,” Michel Zondo, a curator and fossil preparer at the museum, stated in a press release. “It is the first sauropodomorph find of its size from Zimbabwe, otherwise most of our sauropodomorph finds from here are usually of medium- to large-sized animals.”

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