Category: Palaeontological articles

First Fossil Snake with Four Limbs Described

How Snakes Lost Their Legs

Serendipity can play a huge role in science, for Dr Dave Martill a chance encounter with a 115 million-year-old fossil whilst taking a group of third year students around a German museum, has led to a breakthrough in our understanding of how snakes evolved.   A beautifully preserved fossil snake with four limbs, the first snake fossil with four legs ever found, making this specimen a transitional form between limbed lizards and the snakes we know today, is helping scientists to piece together the puzzle of how snakes lost their legs.

Over the last fifteen years or so the University of Portsmouth has arranged a tour of German natural history museums for their third year vertebrate palaeontology students.  On a visit to one such museum, the famous Bürgermeister-Müller-Museum in Solnhofen (Southern Germany), to view the spectacular Jurassic limestone fossils including Archaeopteryx, by chance, the Museum was hosting an exhibit of much younger Cretaceous fossils from Brazil.  Dr. Martill, took his students around the exhibit and to his amazement he spotted on display a small, exquisitely preserved fossil of a snake, but this snake had tiny legs.  Enquiries were made and Dr. Martill working with Dr. Helmut Tischlinger (Bürgermeister-Müller-Museum) and Dr Nicholas Longrich (University of Bath), have published today in the academic journal “Science” a description of this unique fossil specimen.

The Four-Legged Snake Fossil

A beautifully preserved early, limbed snake.

A beautifully preserved early, limbed snake.

Picture Credit: Dr. Dave Martill/University of Portsmouth with additional annotation by Everything Dinosaur

This new snake species has been named Tetrapodophis amplectus (pronounced Tet-tra-poe-doh-fis am-pleck-tus), and it means “four-legged embracing snake”, the embracing element as the limbs were too small to be used in locomotion, they may well have served a function in holding prey or embracing mates.

Both the slab and counter slab are known but their exact provenance remains a mystery.  The fossil specimens were collected many decades ago and held in a private collection.  The fine-grained limestone matrix is dotted with occasional coprolites from an ancient fish called Dastilbe, bedding plains associated with these coprolites come from the Nova Olinda Member of the Crato Formation found in north-eastern Brazil.  The exact age of this Formation is contentious, the lack of marine zonal fossils make dating extremely difficult, but scientists estimate that this important, highly fossiliferous strata dates from between 126 to 113 million years ago (Aptian to Early Albian faunal stages).

The snake measures around twenty centimetres in length and it was very probably a juvenile.  Just how big this snake could grow to remains unknown.  The fossil is preserved in almost complete articulation indicating a low energy fossil preservation environment and a lack of disturbance by scavengers.  This little snake ended up in a hyper saline salt lake and this is what aided its fantastic preservation.

An Illustration of the Early Snake Tetrapodophis (T. amplectus) with Prey

The tiny limbs may have been used to hold prey.

The tiny limbs may have been used to hold prey.

Picture Credit: Julius Csotonyi

Evidence of the snake’s last meal was also preserved, however, it was not a small mammal as depicted in the excellent illustration by renowned palaeoartist Julius Csotonyi.  Dr. Tischlinger, is an expert in the use of UV light to help expose hidden details of fossil specimens, a technique he has used to great effect on the finely-grained, lithographic limestone specimens of Solnhofen.  When viewed under ultraviolet light, the fossil revealed the remains of a small vertebrate, most probably a salamander.

Abdomen Viewed under Ultraviolet Light Reveals Gut Contents

Viewed under UV light the stomach contents are revealed.

Viewed under UV light the stomach contents are revealed.

Picture Credit: Journal Science 

The photograph above shows the position of the gut contents (fluorescing white) – (a) and (b) phosphatised gut contents (also fluorescing white) with tiny fragments of bone (orange).

It is generally accepted that snakes evolved from lizards at some point in the distant past.

Commenting on the significance of this fossil Dr. Martill stated:

“What scientists don’t know yet is when they evolved, why they evolved and what type of lizard they evolved from.  This fossil answers some very important questions, for example it now seems clear to us that snakes evolved from burrowing lizards, not from marine lizards.”

 Dr. Longrich who has extensively studied the evolution of snakes, commented:

“It is a perfect little snake, except it has these little arms and legs, and they have these strange long fingers and toes.  The hands and feet are very specialised for grasping.  So when snakes stopped walking and started slithering, the legs didn’t just become useless little vestiges – they started using them for something else.  We’re not entirely sure what that would be, but they may have been used for grasping prey, or perhaps mates.”

Those Hands and Feet were Not for Walking

At just 4 mm and 7 mm long respectively, the tiny hands and feet were not aiding locomotion, but the well-defined claws suggest that they might have helped Tetrapodophis grasp and hold prey.  They may also have served a role as “claspers” in mating.

A Close Up of the Left Forelimb (Tetrapodophis amplectus)

A close up of the left forelimb.

A close up of the left forelimb.

Picture Credit: Science Journal

The photographs and illustrations above show the T. amplectus holotype (BMMS BK 2-2), specifically a close up view of the left forelimb and hand (manus).  Photograph (a) shows the forelimb, whilst (b) is a close up view of the manus (scale bar 1 mm).  Illustrations (c) and (d)  show the layout of the bones, the dotted line in (d) indicates a missing bone.


  • hu – humerus
  • man – manus
  • ra – radius
  • ul – ulna

A Close Up of the Hindlimbs (Ventral View – Looking from Underneath)

Probably used to help grasp prey or mates.

Probably used to help grasp prey or mates.

Picture Credit: Science Journal

The pictures and diagrams above show the arrangement of the hindlimbs (ventral view), as seen from underneath the body.  Photograph (a) shows the hindlimbs, (d) an illustration of the hindlimbs, (b) is a close up of sacrum and pelvic area, illustrated by diagram (e).  Photograph (c) shows the delicate hind foot which measures approximately 7 mm long.  Diagram (f) shows a layout of the bones in the foot.


  • fem – femur
  • fib – fibula
  • tib – tibia

The fossil suggests that snakes may have lost their limbs to help them burrow, either through sediment of through leaf litter, speculated a member of the Everything Dinosaur team.  Cladistic analysis places the origin of the snakes close to the Iguana and the Anguimorpha families, (the Anguidae family includes limbless lizards such as slow worms), although the exact phylogenetic relationship remains disputed.  The discovery of this fossil suggests that the snake family, a very widespread and diverse group of reptiles today, probably first evolved on the southern super-continent of Gondwana.

Dinosaur Chemical Ghosts

Manchester University Leads the Way With Mapping Elements

Studying fossils has changed radically over the last two decades.  More and more tools are being added to the palaeontologist’s armoury, many of these tools are drawn from a variety of other scientific disciplines, engineering, materials science and medicine for example.  Manchester University has been pioneering the mapping of elements including metals in fossil material.  Once an understanding of a fossil in terms of the elements preserved has been achieved, researchers can begin to piece together clues about the biology of the organism and the burial history.

Using a sophisticated piece of technology (synchrotron-based X-ray imaging), scientists can explore the composition of scales, teeth, skin and feathers from long extinct creatures.  Elements such as zinc (Zn) and Calcium (Ca) can be plotted on the fossil, providing details on features that would not be visible under normal light or ultra-violet lighting conditions.

A False Colour SRS-XRF map of an Archaeopteryx Fossil

Looking at the individual elements of a fossil specimen.

Looking at the individual elements of a fossil specimen.

Picture Credit: Manchester University

The picture above shows a close up of the skull, cervical vertebrae (neck bones) ribs and the wings of Archaeopteryx (Archaeopteryx lithographica).


red = Ca (calcium, the matrix is limestone, hence, high levels of calcium surrounds the fossil)

green – Zn (zinc)

blue = Mn (manganese)

The brighter and more intense the colour the higher concentration of that element.

Blue flecks of colour on the surface of the fossil are the result or the presence of tiny precipitates of manganese minerals, which has probably been deposited by ground water.  There is some zinc associated with mineral precipitates too, but virtually all of the zinc in this image is associated with the fossil bone material.  This suggests that zinc was present in large quantities in the original bone (as found in many types of organism today).  The zinc has been locked within the bones for over 150 million years, as Archaeopteryx (A. lithographica) lived during the Late Jurassic.

 It is the application of new technologies that is opening up a whole world of new possibilities when it comes to investigating creatures that lived in the past.

Back in January, 2015 Everything Dinosaur team members made a number of predictions as to what might happen in the palaeontology over the next twelve months.  One of our “palaeontology predictions” was that there would be more research undertaken into biometals preserved as fossils, there would be more work on the metallome.  A metallome is the presence of metallic elements in relation to organic matter.  From analysis of this data, scientists will be able to learn more about the type of biological processes that once were carried out by long dead organisms.

To read more about Everything Dinosaur’s palaeontology predictions for 2015: Palaeontology and Fossil Predictions for the Next Twelve Months (2015)

For an article published in May 2014 that explains in a little more detail some of the research currently being undertaken into biometals and their presence in the fossil record: Palaeontology Enters the Metal Age

Karoo Rocks Provides Fresh Insight into Extinction Event

Shedding Light on an Extinction Event from 260 Million Years Ago

One global extinction event may have affected both terrestrial and marine biotas at the same time, some 260 million years ago.  With all the news recently of our planet entering a sixth mass extinction, studies into previous extinction events can help scientists to model and predict the impact of future events on environments and the species that live within them.

An international team led by researchers from the Evolutionary Studies Institute (ESI) at the University of the Witwatersrand, (Johannesburg), has obtained an age from rocks of the Great Karoo that shed light on the timing of a mass extinction event that occurred around 260 million years ago.  The Great Karoo refers to a enormous sequence of rocks often cited as the “Karoo Supergroup”, which consists of mostly non marine sandstones and shales that represent a vast tract of geological time, from the Carboniferous through to the Jurassic.  This research focused on exploring fossils from the Beaufort unit, a sequence of rocks that were laid down in South Africa from the Mid Permian through to the Early Triassic.  These rocks provide a record of the plants, invertebrates and vertebrates that thrived in the semi-arid conditions found in southern Africa during the Permian and Triassic.  In particular, they provide evidence of the wide variety of terrestrial vertebrates that lived at this time, the forerunners of today’s reptiles and mammals.

The mass extinction event of 260 million years ago led to the disappearance of a diverse group of early mammal-like reptiles called dinocephalians, which were the largest land-living animals of the time.  Dinocephalians, were large bodied and evolved into a variety of forms including carnivores and herbivores.  They were synapsids and as such, ancestral to modern mammals.

The research project was led by Dr. Michael Day, (postdoctoral fellow at Wits University), the findings have been published today in the Royal Society’s biological journal, “Proceedings of the Royal Society B.”  The paper is entitled:  “When and how did the terrestrial Mid-Permian mass extinction occur?  Evidence from the tetrapod record of the Karoo Basin, South Africa.”

The Karoo is very rich in fossils of terrestrial animals from the Permian and Triassic geological periods, which makes it one of the few places to study extinction events on land during this time.  As a result, South Africa’s Karoo region provides not only a historical record of biological change over a period of Earth’s history but also a means to test theories of evolutionary processes over long stretches of time.  By collecting fossils in the Eastern, Western and Northern Cape Provinces the team was able to show that around 74–80% of species became extinct along with the dinocephalians in a geologically short period of time.

Dr Michael Day with Some of the Fossils Used in the Study (Cranial Material)

Dr. Michael Day and some of the fossils used in the study.

Dr. Michael Day and some of the fossils used in the study.

Picture Credit: Wits University

The new date was obtained by high precision analysis of the relative abundance of uranium and lead in small zircon crystals from a volcanic ash layer close to this extinction horizon in the Karoo.  This provides a means of linking the South African fossil record with the fossil record in the rest of the world.  In particular, it helps correlate the Karoo with the global marine record, which also records an extinction event around 260 million years ago.

Dr. Day explained:

“A Mid-Permian extinction event on land has been known for some time but was suspected to have occurred earlier than those in the marine realm.  The new date suggests that one event may have affected marine and terrestrial environments at the same time, which could mean its impact was greater than we thought.”

The Mid-Permian extinction occurred near the end of what geologists call the Guadalupian epoch that extended from 272.3 to around 259.1 million years ago.  It pre-dated the massive and much more famous end-Permian mass extinction event by 8 million years.

Mid Permian Terrestrial Extinction Plotted Against Proposed Marine Extinction Dates

Table examining the impact of the Mid Permian extinction event on terrestrial fauna.

Table examining the impact of the Mid Permian extinction event on terrestrial fauna.

Table Credit: Proceedings of the Royal Society B.

The table shows that in this new study of Karoo fauna, the demise of the Dinocephalia can be clearly mapped to a marine extinction event (marked by the yellow star).  The marine extinction event has been identified through a study in the change of marine fossils deposited in strata from China (Wuchiapingian age, which has been dated to around 260 million years ago).  The scientists have therefore concluded that one global event may have affected both marine and terrestrial environments simultaneously.  The impact of this event was greater than previously thought.

Dr. Day added:

“The South African Karoo rocks host the richest record of Middle Permian land-living vertebrate animals.  This dataset, the culmination of 30 years of fossil collecting and diligent stratigraphic recording of the information, for the first time provides robust fossil and radioisotopic data to support the occurrence of this extinction event on land.”

Jahandar Ramezani (Massachusetts Institute of Technology), was responsible for dating the stratigraphic sequences using the zircon uranium to lead degradation study (CA-TIMS method).  Dr. Ramezani, of the Department of Earth and Planetary Sciences at the Massachusetts Institute of Technology commented:

“The exact age of the marine extinctions remains uncertain, but this new date from terrestrial deposits of the Karoo, supported by palaeontological evidence, represents an important step towards a better understanding of the Mid-Permian extinction and its effect on terrestrial faunas.”

The “Grandfather” of All Tortoises and Turtles

German Fossil Discovery Could be Transitional Fossil

How did the turtle get its shell?  It sounds like the opening line from one of Aesop’s fables but in reality this question has been vexing palaeontologists for the best part of two hundred years.  Thanks to some remarkable fossil discoveries from southern Germany (Baden-Württemberg) and the work of scientists from the Natural History Museum of Stuttgart and the Smithsonian Institute (National Museum of Natural History, Washington D.C.), we might be one step closer to solving this puzzle.

About thirty-five miles north-east of the city of Stuttgart, lies the picturesque town of Vellberg, there are a large number of quarries extracting Triassic-aged limestone and other materials in this locality, as in this part of the Germany, there are extensive outcrops of Lower Keuper sedimentary material.  In a band of claystone, which represents strata from the Erfurt Formation, (Lower Keuper stratigraphic unit), scientists have excavated eighteen specimens of a small reptile, the fossils of which, could represent a transitional fossil between basal Chelonians (turtles and tortoises) and the types of turtles and tortoises we see today.

The claystone represents sediments deposited at the bottom of a large lake that existed some 240 million years ago in the Middle Triassic ((Ladinian faunal stage).  Although the claystone layer is relatively thin, no more than fifteen centimetres deep at its thickest part, palaeontologists have been exploring these rocks since 1985 as the fossils they provide give a unique insight into the fauna of this part of the world a few million years after the End Permian extinction event, at around the time of the very first dinosaurs.

Dr. Rainer Schoch at the Excavation Site (Erfurt Formation)

Dr. Rainer Schoch working at the claystone bed.

Dr. Rainer Schoch working at the claystone bed.

Picture Credit: Dr. Rainer Schoch/Natural History Museum of Stuttgart

The reptile has been named Pappochelys rosinae, the genus name translates from the Greek meaning “grandfather turtle”, the species name honours Isabell Rosin of the Natural History Museum of Stuttgart as she was responsible for preparing the fossil specimens for study.  This little reptile measured around twenty centimetres in length, the long tail made up about fifty percent of the total body length.  Anatomical features indicate that this reptile is a transitional animal from the more primitive and older Eunotosaurus known from strata dating from approximately 260 million years ago and the more recent Odontochelys, whose fossils come from Chinese rocks and date from about 220 million years ago.

Pappochelys could be an intermediary form in between Eunotosaurus and Odontochelys.  It helps to fill the forty million year gap in Chelonian fossils.  Whilst Odontochelys, lacked the full turtle shell (carapace) it did possess a hard, flat underbelly (plastron).  P. rosinae lacks a plastron, but the gastralia (belly ribs) on its underside are broader and closer to fusing than in Eunotosaurus.

To read about the discovery of Eunotosaurus: An Insight into Chelonian Evolution

Associated Post Cranial Material of Pappochelys rosinae

Post cranial fossil material including the thickened trunk ribs.

Post cranial fossil material including the thickened trunk ribs.

Picture Credit: Natural History Museum of Stuttgart

Hans-Dieter Sues, (Curator of Vertebrate Palaeontology, at the National Museum of Natural History, Washington D.C.) explained:

“In the case of Pappochelys, we see that its belly was protected by an array of rod-like bones, some of which are already fused to each other.  Such a stage in the evolution of the turtle shell has long been predicted by embryological research on present-day turtles but never observed in fossils – until now.”

An Illustration of Pappochelys and Outline Plan of Key Bones

Illustration and outline plan of bones - ribs (yellow), gastralia (red), shoulder girdle (green), pelvis (brown), femur and vertebrae (mustard)

Illustration and outline plan of bones – ribs (mustard), gastralia (red), shoulder girdle (green), pelvis (brown), femur and vertebrae (yellow)

Picture Credit: Natural History Museum of Stuttgart

The diagram shows the thickened trunk ribs of this ancient reptile and the lacustrine (lake) deposit might provide a clue as to why such creatures eventually evolved a hard shell.  The bones are thickened and more dense, if this animal was semi-aquatic, then the heavier bones would help to provide ballast and counter the animal’s natural buoyancy in water.  The more robust, heavier bones might have helped this reptile to dive deeper and to stay underwater for longer.  The pelvis and the shoulder girdle are very similar to those found in Odontochelys, which is regarded by many scientists as the earliest true turtle.

A Dorsal view of the Bauplan Showing Modified Ribs and Gastralia

Expanded ribs (yellow) gastralia (red)

Expanded ribs (mustard) gastralia (red)


Picture Credit: Natural History Museum of Stuttgart

The picture above shows a skeletal reconstruction of Pappochelys.  The ribs (mustard) and the gastralia (red).

Dr. Sues outlined the anatomical developments leading to modern-day turtles that could be traced from the fragmentary fossils found at Vellberg.  The paper on these specimens, which Dr. Sues co-authored has just been published in “Nature”.

He stated:

“It [Pappochelys] has real beginnings of the belly shell developing, little rib-like structures beginning to fuse together into larger plates and then ultimately making up the belly shell [plastron].”

Where do the Tortoises and Turtles Fit in with Other Reptile Groups?

The origins of the Chelonia (turtles and tortoises) remain controversial.  More modern Chelonia, such as those genera still around today do not have teeth.  Instead, they have a beak.  Pappochelys had teeth, (some cranial material including jawbones and teeth have been found) and it is known that Odontochelys also had teeth (the genus name translates as “toothed turtle with half a shell”).  However, scientists have long argued where in the Order Reptilia the Chelonia actually sit.  They are regarded as a very ancient group of reptiles.  It had been thought that turtles and tortoises were descended from ancient Parareptiles, but the skull bones of Pappochelys reveal an affinity to the Diapsid reptiles, a wide-ranging group that includes lizards, snakes, crocodiles as well as extinct marine reptiles and the Dinosauria.

It had been thought that tortoises and turtles were Anapsids, lacking temporal fenestrae (holes behind the eye socket in the skull, but the Pappochelys cranial material shows a pair of openings in the skull behind each eye socket.  This suggests that the Chelonia are not descended from Parareptiles but have phylogenetic affinities to the Diapsids.  This places them in the same clade as lizards and snakes.

Fibres and Cellular Structures Observed in Dinosaur Fossils

Soft Tissue Preservation in Late Cretaceous Dinosaur Bones

When Everything Dinosaur team members were first informed of a paper being published that reported on “blood cells and soft tissue” having been discovered in dinosaur fossils the day before the film “Jurassic World ” was released, there was some scepticism around the office.  Amid the inevitably lurid and rather dramatic headlines which have been seen in some publications we thought it a good idea to try to put this fascinating piece of research into a wider context.  The study was undertaken by scientists at the Imperial College London, their findings were published in the academic journal “Nature Communications”, it is not going to herald the establishment of a number of genetically engineered dinosaur themed safari parks, but it does suggest that even poorly preserved body fossils may contain more than just permineralised materials.

Bones and Teeth Alone are Not Enough

Most of what we have learned about the Dinosauria has been gained from studying their bones and teeth.  Trace fossils too have proved useful, even permitting researchers to speculate on behaviours such as social groupings and pack hunting, but if traces of soft tissue could be analysed, then our understanding could move forward exponentially.  Such a study could provide valuable insights into dinosaur physiology, it would for example, provide strong evidence with regards to the endothermy versus ectothermy debate (warm-blooded versus cold-blooded).  Importantly, the link between the Coelurosauria and birds could be established beyond doubt.  In short, it could be proved that the Robin perched on your bird table is indeed a distant relative of Tyrannosaurus rex.

Dr. Susannah Maidment One of the Authors of the Study Holding a Stegosaurus Skull Cast

Dr Susannah Maidment, one of the authors of the study holding a cast of a Stegosaurus skull.

Dr Susannah Maidment, one of the authors of the study holding a cast of a Stegosaurus skull.

Picture Credit: Laurent Mekul

A point that we frequently make is that dinosaur biology remains very much a mystery.  What we have learned has come about through some very remarkable research that utilises techniques and scientific methods that were undreamed of even a few years ago.  It is the collaboration between different scientific disciplines that is providing so much new information on dinosaurs and other extinct creatures.  The use of computerised tomography (CT), for example, has enabled palaeontologists to explore the three-dimensional structures of fossil bone, even when it has been embedded in extremely dense rock.  In this study, samples from eight dinosaur bone specimens were subjected to scanning electron microscopy (SEM) to provide exquisite images of the fossil structures in minute detail.  A number of samples were studied using a focused ion beam  (FIB), an imaging and resolution technology more at home in a materials science lab but now finding an increasing number of applications in other scientific areas of enquiry including vertebrate palaeontology.  It is the adoption and application of different scientific methods, drawn from a whole variety of research fields that is enabling academics to make some remarkable discoveries, shedding light, or in this case electrons and ions on those most enigmatic of extinct creatures – the dinosaurs.

Any Old Fossils?

The novel approach undertaken by the Imperial College scientists sets up an intriguing possibility, one that allows us to use an analogy from the “Jurassic Park” franchise  to explain.  The eight fossils used in this study came from the Natural History Museum (London), which is conveniently located just a few hundred metres away from the College.  Specifically the fossils come from two collections at the Museum, all of them relate to Late Cretaceous dinosaur fossil material from North America (Dinosaur Provincial Park and Lance Formations respectively).  The fossils studied represent a claw bone from an unknown species of meat-eating dinosaur, a partial rib from an indeterminate duck-billed dinosaur and other bits and pieces of assorted dinosaur that would not have got a second glance had they been on display.  That’s the point.  Evidence for soft tissue preservation in a number of vertebrate fossils have been reported before, even in the Dinosauria.  This area is not without controversy, but here evidence has been presented for the potential preservation of organic remains from reptiles that died more than seventy million years ago.

Dinosaur Claw Bone used in the Study

Manual ungual (dinosaur claw) from an unknown species of Theropod used in the Imperial College London study.

Manual ungual (dinosaur claw) from an unknown species of Theropod used in the Imperial College London study.

Picture Credit: Laurent Mekul

If these fragments of fossils can possibly contain proteins and other biological structures, then maybe, just maybe there is a lot more preserved within the fossil record – we just have not been looking for it.

Jurassic Park

Let’s use that “Jurassic Park” analogy to look at this intriguing aspect further.  In the original book, written by Michael Crichton and published in 1990, the InGen scientists (the team behind the creation of various dinosaurs using DNA recovered from blood-sucking insects preserved in amber, mixed with amphibian genetic material and so forth), come up with what they think to be an infallible method of ensuring that all their engineered dinosaurs stay on their island home.  Each animal’s position is tracked and movements can be recorded using a simple receiver.  With three hundred dinosaurs on the preserve, it is just a case of asking the software that tracks the animals’ comings and goings to find three hundred dinosaurs.  Every day without fail, when asked, the computer read out states that there are three hundred dinosaurs on the island.  The flaw in this safety precaution is pointed out by Dr. Ian Malcolm, a mathematician who has been brought to the resort in order to validate it prior to the park opening to the public.  The good doctor, asks the computer programme to find three hundred and one dinosaurs, and sure enough the software reports on that number.  Dr. Malcolm continues to interrogate the team behind the computer programme asking repeatedly for the software to detect more and more dinosaurs.  The doctor, a  specialist in Chaos Theory, had predicted that the biological preserve would fail “nature finds a way” as he so eloquently states in the film.  Despite the entire dinosaur population starting out as female, the animals had started to breed and that was why there were more dinosaurs recorded than expected.

Just like in the example above, scientists may have been asking the wrong questions.  Soft tissue preserved in the fossil record of long extinct creatures might be more common than previously thought.  Similar structures have been observed before, but for most of the time, the research was focused on investigating the range of criteria that were believed to have existed to have led to the preservation of organic remains, these specimens were treated as the exception – could they be the norm?

Caution Advised

Tiny egg-like shapes identified deep within a dinosaur claw bone that have a resemblance to red blood cells, certainly deserve further analysis and investigation.  Admittedly, the red and green images of the structures with the different colours reflecting varying material densities can be confusing, after all, if a lay person reads a headline in a magazine stating that dinosaur blood may have been found and sees a picture covered in red, he or she may jump to one very obvious conclusion.  Mass spectrometry analysis, another relatively recent addition to the palaeontologist’s ever increasing technical armoury, this time from the laboratory of an analytical chemist, threw up tantalising results when the red blood cell-like materials were scrutinised.  Four different regions from the same fossilised Theropod claw were compared to the mass spectrometry report for Emu blood.  The resulting data suggested that there were indeed chemical similarities.  If this really is some form of preserved, (although quite probably severely degraded), remnant of a Theropod dinosaur’s blood then, as Ratites such as the Emu are believed to be closely related to the Theropoda then similar mass spectrometry results could be anticipated.

Potential Evidence of Preserved Red Blood Cells in Dinosaur Bone

Evidence of potential red blood cells preserved in 75 million year old dinosaur bone.

Evidence of potential red blood cells preserved in 75 million year old dinosaur bone.

Picture Credit: Laurent Mekul

Microscopic Fibres – More Caution Advised

Fibres or fibrous-like structures were reported from half the samples studied.  In one specimen, a fragment of rib bone from an unknown dinosaur revealed a structure within it that resembled collagen.  Further chemical analysis revealed traces of amino acid fragments such as glycine, alanine and proline.  This is consistent what you would expect to find if you were analysing collagen.  If a fragment of collagen could be recovered, then that would be a remarkable discovery indeed.  Like blood and other organic materials these substances are believed to degrade relatively quickly after death.  However, if a protein based structure like collagen could be found in the fossilised bones of a dinosaur then this would open up an entirely new area of research into the Dinosauria.

Potential Collagen Structures Preserved in Fossil Bone

Fibrous structures preserved in fossilised bone.

Fibrous structures preserved in fossilised bone.

Picture Credit: Laurent Mekul

The scientists behind this paper are keen to point out that further study is required.  Two of the fossil bones used in this research revealed no traces of any potential soft tissue components, a point missed by a number of media outlets that covered this story. However, if poorly preserved fossil material can retain microscopic traces of blood and other organic materials then it will change our science forever.  Dig sites will be subjected to forensic procedures, perhaps a clean room will be have to be set up in the field to help minimise the risk of organic cross-contamination.  What about the use of glues and resins that act as fossil bone stabilisers?  Could the over enthusiastic use of super glue at a dig station compromise the chances of retrieving viable traces of organic material later, back in the prep lab?

If other institutes can repeat these experiments and produce the same results consistently, then this has some dinosaur-sized implications for palaeontology.  If it can be concluded that the structures observed and analysed within the samples do indeed originate from preserved proteins from the extinct animal, then we may have an opportunity to study soft tissues in long dead creatures.  A more complete understanding of dinosaur biology may be within our grasp.

Now that would be something to make a movie about.

Annual Queensland Dinosaur Dig Yields Fossils

Queensland Dinosaur Dig Unearthing Bones

At the beginning of the month we reported on the annual Australian dinosaur excavations that were opening up once again in Queensland.  As the digs continue to progress, scientists from the Australian Age of Dinosaurs Museum (Winton), have stated that a number of new dinosaur fossils have been found.  At the start of the dig season, palaeontologists had expressed the wish to discover a new species of Cretaceous dinosaur, given the wealth of material recovered so far it seems that there is a strong possibility that the fossil specimens, once fully prepared might lead to the identification of a new genus of Australian dinosaur.

To read Everything Dinosaur’s earlier article about the annual excavations: Time for Some More Aussie Dinosaurs

The exposed strata around Winton dates from the Late Cretaceous (98 to 95 million years ago).  During this time, (Late Albian faunal stage of the Lower Cretaceous), Australia was beginning to separate from Antarctica as the super-continent of Gondwana continued to break up, most of the dinosaur’s described from Queensland rocks are unique to Australia, although they are related to other types of dinosaur found elsewhere in the southern hemisphere.

Fossil Bone is Carefully Cleaned

An air scribe is used to remove the surrounding rock from the bone.

An air scribe is used to remove the surrounding rock from the bone.

Picture Credit: ABC News (Chrissy Arthur)

 Dr. Stephen Poropat (Australian Age of Dinosaurs), commented that a number of intriguing specimens had already been found including some large dinosaur bones.

He added:

“We are looking for a Sauropod dinosaur, so a long-necked dinosaur with four elephant-like legs and then a long tail – and we know that because we have found some of its back bone and some of its ribs.”

A number of locations are currently being explored, some of them have not been studied and mapped before.   It is hoped that these excavations and the dinosaur discoveries will help to provide a boost to the local economy as tourists visit the area to view Australia’s very own “Jurassic Park”, or to be more correct and with the age of the strata considered it would be more appropriate to refer to this location as “Cretaceous Park”.

The Australian Age of Dinosaurs Executive Chairman, David Elliott explained that the work carried out so far, it had been hard going but some significant finds had been unearthed.

Mr Elliott stated:

“We found one really nice scapula [shoulder bone], like a big shoulder blade and it is beautiful, it is quite a large bone.”

Dinosaur bones had been found at several locations, the Executive Chairman added:

“We’re just starting to really hit on the bones now, we have found this big row of boulders, and we are talking massive boulders, like the size of a ute [utility vehicle].”

Once identified as fossil bearing rock, these large boulders will have to be carefully jacketed and then loaded onto either large pick-up trucks (utes to use the local vernacular), or onto a low loader.  Once safely back at the laboratory, the careful job of preparing and cleaning the fossilised bones can begin.

Volunteers and Scientists Work Together to Explore Another Likely Dig Site

Digging for dinosaurs in the Outback.

Digging for dinosaurs in the Outback.

Picture Credit: Australian Age of Dinosaurs

Although, Everything Dinosaur team members have no additional information at this stage and we have not received details of the measurements of any fossil material, but if the fossils are as large as predicted, then the palaeontologists will probably be looking at another sizeable Australian Titanosaur, perhaps something in excess of twenty metres in length.  A number of Titanosaurs are already known from this part of the world, dinosaurs such as Wintonotitan (W. wattsi), which may have reached a length of around fifteen metres or so when fully grown and the slightly smaller Diamantinasaurus (Diamantinasaurus matildae).  The palaeoenvironment must have been particularly rich and diversified to be able to sustain a number of different types of Titanosaurs within the same habitat.

We look forward to hearing more about these new fossil discoveries from Queensland.

Britain’s Oldest Sauropod

A New Sauropod Dinosaur from the Middle Jurassic

Here is a tale of a tail bone from the United Kingdom, one that once formed part of the skeleton of a primitive Sauropod that lived in Yorkshire some 176 million years ago.  It fell out of a cliff and was found on the beach close to the north Yorkshire coastal town of Whitby, not too far away from the famous Abbey.  The fossil was sent to the University of Manchester for further study and detailed X-ray computer tomography analysis was undertaken at the nearby Manchester Royal Infirmary (Dept. of Radiology) in a bid to learn more about the specimen.  The fossil represents a caudal vertebra (a tail bone) one that would have been located in the long tail but near to the hips.

Team members at Everything Dinosaur have seen this specimen up close.  We were shown the fossil on a visit to Manchester University some years ago by Professor Phil Manning.  A paper detailing this discovery has been published in the journal PLOS One, Professor Phil Manning co-authored this paper along with colleague Victoria Egerton (School of Earth, Atmospheric and Environmental Sciences) with the help of Mike Romano, an independent researcher based in Sheffield (South Yorkshire).

The Sauropod Dinosaur Tail Bone

The specimen is currently housed at the Yorkshire Museum (York).

The specimen is currently housed at the Yorkshire Museum (York).

Picture Credit: Manchester University

The picture above shows the indeterminate Sauropod caudal vertebrae, the face of the centrum can clearly be seen as can the hole in the bone which represents the neural canal where the spinal cord passed through.  The specimen is significant as it comes from the Saltwick Formation which forms one of the oldest sequences of rock from the Ravenscar Group of largely terrestrial deposits laid down in an estuarine environment.  Very few body fossils have been found in these rocks, but a number of dinosaur trackways have been described.  These tracks represent a number of different types of dinosaur, Theropods, Stegosaurs, Ornithopods and long-necked dinosaurs – Sauropods.  The strata was formed around 176 million years ago (Aalenian faunal stage ) of the Middle Jurassic.  This fossilised bone is therefore the oldest Sauropod fossil scientifically described from the British Isles.  It is some 4 million  years older than the Cetiosaurus spp. material which has been described from strata laid down during the Bajocian and Bathonian faunal stages of the Jurassic.

It most certainly represents a new species and the specimen had been nick-named “Hildasaurus” after St Hilda, the abbess who founded Whitby Abbey on the East Cliff overlooking the town.  However, due to the very low number of Sauropod caudal vertebrae that have been described from the Middle Jurassic, it is not possible to assign this fossil to a new species and to give the dinosaur bone a binomial scientific name.

A Typical Cetiosaurid Sauropod Dinosaur

Cetiosaurus early Sauropod

Cetiosaurus early Sauropod

Picture Credit: Everything Dinosaur

Professor Manning explained:

“It was a splendid surprise to come face-to-face with a fossil vertebra from the Jurassic rocks of Yorkshire that was clearly from a Sauropod dinosaur.  This fossil offers the earliest “body fossil” evidence for this important group of dinosaurs but it’s impossible to define a new species based on this single bone.”

 Views of the Caudal Vertebra (Specimen Number: YORYM: 2001.9337)

Not possible to determine a species for this important fossil.

Not possible to determine a species for this important fossil.

Picture Credit: PLOS One

The picture above shows two further views of the fossil material (A) oblique view (photograph taken at an angle, not quite an anterior view), which shows a distinct keel on the bottom of the bone and a partial caudal rib (CR) that can be seen on the left of the bone.

Key (Picture A)

PRZ = prezygapophysis – a peg of bone located on the neural arch which articulates with the next tail bone in the caudal vertebrae sequence.

SPRF = spinoprezygapophyseal fossa – a channel in the reinforcing ridge of bone commonly associated with Sauropod vertebrae that strengthens the connection between the bones

CPRL = centroprezygapophyseal lamina – the ridge of bone the connects the centrum with the prezygapohysis at the top of the vertebra

CR = caudal rib – one of a pair of thin, struts of bone that point out at roughly ninety degrees to the face of the centrum.  These small bones support tail muscle attachments.

KEEL = keel – describes the shape of the bone at the base of the centrum.

Although the fossil bone is not complete, these features have helped the scientists to determine that this specimen, most probably does not represent a Cetiosaurus.  Caudal tail bones located relatively close to the hips, such as those fossils assigned to the “Rutland Cetiosaurus” lack the keel shaped portion of bone on the ventral face of the vertebra.  In addition, the fragment of caudal rib present in the specimen is located at a different position in relation to the centrum when compared to the caudal ribs found on cetiosaurid fossil material.

Picture B shows a lateral view (a view of the right side of the fossil).  The shape of the neural spine (NS) can be clearly seen in this view.

Key (Picture B)

NS = neural spine, a blade shaped bone projection that sits on top the neural arch.

SPRL =  spinoprezygapophyseal laminae – a ridge of bone that strengthens the connection between the neural  with one of the prezygapophyses.

FOSSAE = recessed areas or depressed areas of bone (single = fossa).

In both picture A and B, the scale bar is 5 cm.

Although, the caudal vertebra is similar to that found in Cetiosaurus spp. and has some potential affinity with another Sauropod called Haplocanthosaurus (Upper Jurassic Morrison Formation of the United States), the morphological differences described indicate that this fossil bone does represent a new, as yet undescribed species of long-necked, Middle Jurassic dinosaur.

A Close up View of the Sauropod Fossil showing the Distinctive Keel

Ventral view (view from underneath)

Ventral view (view from underneath)

Picture Credit: PLOS One with additional annotation from Everything Dinosaur

The pointed keel shape can be made out in this ventral view (photograph above).  The density of the surrounding matrix made CT interpretation difficult but enough of the fossil bone has been prepared to confirm the Sauropod diagnosis but genus level or even family level identification is not possible.  Fossilised fragments of plant rootlets and other material has helped the palaeontologists to identify the origins of this fossil, even though it was found on the beach having eroded out of the cliff face.  The lack of abrasion (erosion) on any of the exposed faces suggests that this fossil was not transported far prior to burial, or indeed, that the fossil material had not been exposed on the shore for very long prior to its discovery.

This discovery gives team members at Everything Dinosaur the opportunity to applaud the hard-working team of scientists (both amateur and professional) that so conscientiously dedicate so much time to the exploration and study of the many important geological sites in the British Isles.  It was Alan Gurr who actually found this proximal caudal vertebrae on a field trip led by Professor Phil Manning.  The specimen (YORYM:2001.9337), may not be able to be assigned to a species, but the fossil was nick-named “Alan” in honour of the finder.  The very talented Mike Marshall of Yorkshire Coast Fossils was responsible for preparing the vertebrae and such careful preparation permits a rare insight into the ancient fauna of the Jurassic.

Dinosaurs were Warm-blooded? Debate Hots Up

New Study Suggests Dinosaurs were Warm-blooded (Endothermic)

A scientist from Stony Brook University has reassessed a study into whether dinosaurs were cold or warm-blooded.  Dr. Michael D’Emic, a palaeontologist at the New York based university, has re-examined the research in a report published last summer which proposed that dinosaur metabolism was a kind of “half-way house” between a cold-blooded reptile and that of a warm-blooded mammal.  Palaeontologist Dr. D’Emic suggests that dinosaurs were not mesotherms (half-way between cold and warm-blooded), but instead their growth rates suggest that the Dinosauria are indistinguishable from the Mammalia in terms of their metabolism.

The Debate Over Dinosaur Metabolism Heats Up

Where on the spectrum between endothermic and ectothermic are the Dinosauria?

Where on the spectrum between endothermic and ectothermic are the Dinosauria?

Picture Credit: Everything Dinosaur

Yesterday, (May 29th), Dr. D’Emic’s study was published as a technical comment in the academic journal “Science” in response to the 2014 research.  In the absence of a living, non-avian dinosaur to study, the debate boils down to interpretation of the evidence and statistical analysis. But why the fuss over what kind of metabolism the dinosaurs had?

Ectothermic versus Endothermic – It is Rather Important

We at Everything Dinosaur doubt very much that members of the public are going to be whopping and hollering about ectotherms (cold-blooded animals) or endotherms (warm-blooded) as they leave cinemas in a few weeks time having just watched “Jurassic World”, but understanding the metabolism of the Dinosauria is essential if scientists are really going to be able to learn how these animals lived and behaved.  Let’s kick off with some simple explanations.

What does it mean to be Cold-blooded or Warm-blooded?

These terms are frequently used, but they are themselves a little misleading.  These two distinct states do not define all vertebrates, things are a little more complicated than that, but in essence a creature that is regarded as cold-blooded relies on external sources to help regulate its body temperature.  Typical examples are lizards and snakes basking in the sun to warm up in the morning, but then seeking much cooler shade to avoid over-heating in the middle of the day.  Warm-blooded animals (mammals and birds), are able to maintain a body temperature that is higher than the temperature of the environment.  In simple terms, they can generate their own body heat. This heat comes from the animal’s metabolism, the chemical reactions that take place in the body (although there are other methods of keeping cool and warming up).

Applying this to the Dinosauria

If the dinosaurs had the same body chemistry as a crocodile (a reptile, regarded as an ectotherm), then they would have been relatively inactive compared to large mammals.  Nocturnal activity could have been reduced along with geographical distribution, very cold environments would have been extremely hostile to cold-blooded dinosaurs.  This is why today, we see the majority of reptile species confined to the tropics.  If the dinosaurs had the same metabolism as birds and mammals, then they would have been much more active and not reliant on external sources to help maintain a body temperature that enabled them to function.  The type of body chemistry employed would impact on every aspect of their lives – migration, breeding, food intake, social interactions, growth rates, intra-specific and inter-specific competition and so forth.

Take food as an example.  Whether herbivore, omnivore or carnivore, an ectotherm requires a lot less food in order to survive than an equivalent sized endotherm.  Lions (warm-blooded),  have to feed every three to five days on average.  They have high metabolisms and high food demands as a result.  Nile crocodiles that live in the same environment need much less food.  One substantial meal can last a Nile crocodile several months, crocs are much less expensive to run.  Sunlight can provide their bodies with all the heat they need, they don’t need to create it themselves, so their bodies need less food.

Over the years, team members at Everything Dinosaur have posted up articles on the ectotherm versus endotherm debate.  In June 2014, we published a feature on the research carried out by student John Grady (University of New Mexico) in association with colleagues from the University of Arizona and the Sante Fe Institute.  It is the results of this research that Dr. D’Emic has reassessed.

To read about the June 2014 study: Goldilocks and Dinosaurs – The Warm-blooded/Cold-blooded Debate

Dr. D’Emic proposes that further analysis of microscopic growth rings preserved in dinosaur fossil bone, suggests that dinosaurs grew as quickly as mammals.  This suggests fast metabolisms and therefore that the Dinosauria were endothermic.  The earlier study had undertaken a detailed analysis on the growth rates of a wide variety of extinct and extant organisms.  The research team led by John Grady concluded that dinosaurs were mostly like mesotherms.

Dr. D’Emic stated:

“Upon re-analysis, it was apparent that dinosaurs weren’t just somewhat like living mammals in their physiology – they fit right within our understanding of what it means to be a “warm-blooded” mammal.”

As a Research Instructor in the Dept. of Anatomical Sciences, Dr. D’Emic specialises in the study of the structure of bone.  Using microscopic slices of fossil bone that has been carefully cut and polished, the doctor read growth rings preserved in the bone just as a dendrochronologist examines tree rings.  He looked at the 2014 study from two specific view points, firstly the research had scaled down yearly growth rates to daily ones in order to standardise  the data.

Commenting on this aspect of the earlier study, he explained:

“This is problematic, because many animals do not grow continuously throughout the year, generally slowing or pausing growth during colder, drier, or otherwise more stressful seasons.”

He concluded that the 2014 study may have underestimated the growth rate of the different types of dinosaur included in the dataset, by failing to account for their uneven growth.  Like many extant animals, dinosaurs slowed or paused their growth.  This is marked by the growth rings that can be made out in micro-anatomical bone studies.  The doctor added that growth rates were especially underestimated for larger animals and animals that live in very stressful or seasonal environments – both of which characterise the Dinosauria.

Microscopic studies of Dinosaur Bone Reveal Growth Rings

The bands mark periods of arrested or stopped growth.

The bands mark periods of arrested or stopped growth.

Picture Credit: Stony Brook University

Secondly, in the paper entitled “Evidence for Mesothermy in Dinosaurs”, birds in the sample studied were treated separately from the twenty-one dinosaurs that were included,  In this reassessment, birds and dinosaur data was included as one homogeneous group.  Birds are warm-blooded and they are direct descendants of dromaeosaur dinosaurs.

The doctor explained:

“Separating what we commonly think of as “dinosaurs” from birds in a statistical analysis is generally inappropriate, because birds are dinosaurs – they’re just the dinosaurs that haven’t gone extinct.”

Under these new conditions for examining the statistics, the birds being included in the dinosaur assessment data, lends more weight to the idea that the Dinosauria were endothermic and not the “half-way house” as mesotherms.

It seems that as with virtually all studies of this nature, the way that the data is handled and the terms of reference will influence the conclusions that can be drawn.

Microscopic Analysis of Fossilised Bones Helps Identify Growth Patterns

A microscopic image of the thigh bone (femur) of a dinosaur shows concentric rings. The rings represent unrecorded time, so an annual growth rate (dashed line in graph) is an underestimate relative to the true growth rate during the favourable growing season.

A microscopic image of the thigh bone (femur) of a dinosaur shows concentric rings. The rings represent unrecorded time, so an annual growth rate (dashed line in graph) is an underestimate relative to the true growth rate during the favourable growing season.

Picture Credit: Scott Hartman

Comments regarding this new assessment of the earlier research have already been made.  For example, the team behind the 2014 study have responded to this analysis by commenting that the new study raises a number of important statistical and methodological questions, however, the proposals made lack biological and statistical justification.

All scientists who step bravely into this area of academic endeavour deserve our admiration, both papers are part of the rich and extremely diverse range of research that has gone into tackling this very thorny problem, it seems that the warm-blooded versus cold-blooded debate is likely to rumble on.

A New Face to the Human Family Tree

Australopithecus afarensis Had Neighbours!  Say Hello to Australopithecus deyiremeda 

Had you and I been able to travel back in time to the Afar region of northern Ethiopia some 3.4 million years ago in a bid to meet our ancient ancestors, we might have been spoilt for choice when it comes to trying to work out from which species we are descended from.  Lucy* the most famous example of Australopithecus afarensis had company, she had neighbours, a newly described species of Australopithecine has just been announced.

Two fragmentary upper jaws along with two fragments of lower jaws, representing fossil material from three individuals were found in March 2011 in the Woranso-Mille area of the Afar region.  These fossils have been assigned to an entirely new genus of Australopithecine, say hello to Australopithecus deyiremeda. 

Casts of the Four Fossil Jaws are Displayed

A new Australopithecus species has been described.

A new Australopithecus species has been described.

Picture Credit: Laura Dempsey

The fossil material assigned to Australopithecus deyiremeda (pronounced ost-tral-oh-pith-e-kus day-ihremy-dah) was described by a team of international palaeoanthropologists led by Dr. Yohannes Haile-Selassie, the Curator of Physical Anthropology at the Cleveland Museum of Natural History (Cleveland, Ohio).  The fossils are estimated to between 3.3 million and 3.5 million years old, which means that this species overlapped and lived in the same region as Australopithecus afarensis, the species that the famous fossils called “Lucy” have been assigned to.  However, although A. deyiremeda and A. afarensis lived at the same time and shared the same habitat, the “Lucy” fossil material has been dated to 3.2 million years ago, meaning that the most famous representative of the Australopithecus afarensis species – “Lucy” lived more recently and could never have met the individuals whose jawbones have been preserved.

A Field Photograph Showing the First Jaw Fragment Found

The upper jaw (holotype) found on March 4th 2011.

The upper jaw (holotype) found on March 4th 2011.

Picture Credit: Yohannes Haile-Selassie/Cleveland Museum of Natural History

The picture above shows a field photograph of the holotype (upper jaw), five teeth can be clearly seen.  The discovery of this new species is significant for a number of reasons.

  1. This is the first irrefutable evidence of two species of Australopithecine co-existing.  These two species lived at the same time in the Middle Pliocene and in the same part of the world.
  2. These fossils suggest that the Australopithecus genus was more diverse than previously thought, it had been thought that the Homo genus evolved from A. afarensis but this may not have been the case, a number of candidate species are emerging.
  3. The morphology of the jaws, the size and shape of the teeth and their enamel thickness suggest characteristics not found in A. afarensis but more akin to later genera, the Paranthropus and the Homo genus, for example.  These traits go back much further in time than previously thought.

The Left Half of a Lower Jaw Found on March 4th 2011

A lower jaw fragment  of A. deyiremeda.

A lower jaw fragment of A. deyiremeda.

Picture Credit: Yohannes Haile-Selassie/Cleveland Museum of Natural History

The academic paper that details this discovery has just been published in the journal “Nature”.  In recent years, the hypothesis of a relatively simple, linear progression from Australopithecus to the Homo genus and ultimately the origin of our own species has become less popular amongst researchers.  It seems the hominin family tree is much more complicated than previously thought.

To read an article written by Everything Dinosaur back in 2011, about other Australopithecus discoveries, but this time from southern Africa: The Human Family Tree Just Got More Complicated

A Close Up of the Left Lower Jaw Prior to Cleaning

The left portion of the lower jaw, prior to cleaning.

The left portion of the lower jaw, prior to cleaning.

Picture Credit: Yohannes Haile-Selassie/Cleveland Museum of Natural History

Commenting on the importance of this fossil discovery Dr. Yohannes Haile-Selassie stated:

“The new species is yet another confirmation that Lucy’s species, Australopithecus afarensis, was not the only potential human ancestor species that roamed in what is now the Afar region of Ethiopia during the Middle Pliocene.  Current fossil evidence from the Woranso-Mille study area clearly shows that there were at least two, if not three, early human species living at the same time and in close geographic proximity.  This new species from Ethiopia takes the ongoing debate on early hominin diversity to another level.  Some of our colleagues are going to be sceptical about this new species, which is not unusual.  However, I think it is time that we look into the earlier phases of our evolution with an open mind and carefully examine the currently available fossil evidence rather than immediately dismissing the fossils that do not fit our long-held hypotheses”.

The Very Near Complete Lower Jaw (Field Photograph)

A field photograph of a nearly complete lower jaw fossil with teeth.

A field photograph of a nearly complete lower jaw fossil with teeth.

Picture Credit: Yohannes Haile-Selassie/Cleveland Museum of Natural History

This discovery raises the question of how multiple types of early hominins may have been able to co-exist in the same environment.  For those readers unfamiliar with the term hominin, a hominin is defined as a species more closely related to humans than to our closest extant ape relative the chimpanzee.  Clues can be found in the fossilised jaws and teeth.  The jaws of A. deyiremeda are very deep and robust, but the teeth are proportionately smaller than seen in other Australopithecines.  The canine teeth are particularly small, smaller than all known hominins that have been described previously.  The jaws and teeth may reflect adaptations to a different type of diet.

A member of the Everything Dinosaur team explained:

“Teeth are relatively common in the hominin fossil record, as the extreme hardness of the enamel means that, compared to bones for example, they have a greater fossilisation potential.  If patterns of wear can be discerned then it might be possible to hypothesis on the diet of this new species.  As the jaws and teeth are different from A. afarensis, it could be assumed that these two hominins did not compete directly with each other for food resources, in short, each species ate different types of food.”

The size of the canine teeth may also be very significant.  We have four canine teeth, two in the top jaw and two in the lower  jaw. They sit between the first premolar and the last incisor and the size of the canine teeth can provide evidence about social behaviours associated with a species.  In primates, where males compete with each other over females, the canine teeth of the males are usually much larger than the canines of females.  Canine teeth can be used as weapons as the males fight each other to establish social hierarchies and dominance.

A Close Up of the Upper Jaw Fragment with the Canine Tooth Highlighted

Teeth can tell us a lot about an extinct creature.

Teeth can tell us a lot about an extinct creature.

Picture Credit: Laura Dempsey, with additional annotation by Everything Dinosaur

If more teeth ascribed to A. deyiremeda can be found, then more research can be undertaken on the potential dietary differences between different hominins and some exciting inferences about social behaviours and social structures could be made.

Everything Dinosaur, acknowledges the contribution of the Cleveland Museum of Natural History in the compilation of this article.

Prehistoric Parasites from the Silurian

 Rare Discovery Provides Insight into Ancient Parasite

A team of international researchers have got up close to a prehistoric parasite, one that is perfectly preserved along with its 425 million-year-old host.  The ancient parasite, known as a “tongue worm” provides scientists with a glimpse of life and the interactions between species in a warm tropical sea that existed in Britain back in the Middle Silurian.  Fossils of tongue worms are extremely rare, examples have been recovered from Ordovician as well as older Cambrian deposits, the Silurian fossils are exceptionally well preserved, we at Everything Dinosaur believe the fossils to be part of the Wenlock Epoch biota.  The actual location of the fossil find has not been disclosed in order to protect the site from amateur fossil hunters and those keen to exploit the fossil deposits commercially.

The fossils come from a deposit in Herefordshire, close to the border with Wales, scientists from the University of Leicester, who took part in the study stated that the tongue worm represents a new species and they range in size from 1mm to 4mm in length.  Tongue worms have tongue shaped bodies, a distinct head and two pairs of limbs.  At least 140 species are known to exist today, most are respiratory or gut parasites of vertebrates (usually reptiles), these fossils provide scientists with information on how these creatures evolved before they made the move onto land to become parasites of terrestrial vertebrates.

The Computer Model Showing the Ostracod Shell (grey) with the Tongue Worm attached (orange)

Looking at the micro-fauna of the Silurian.

Looking at the micro-fauna of the Silurian.

Picture Credit: Siveter, Briggs, Siveter and Sutton

The picture above shows the pentastomid Invavita piratica and its host, the Ostracod Nymphatelina gravida.

The newly described fossils show the tongue worm species in association with its host, in this case a species of Ostracod (an Arthropod).  It was professor David Siveter, (Department of Geology) at Leicester University, who  made the discovery.  An academic paper describing the new species, named as Invavita piratica, (the name translates as ancient, pirate intruder) has been published in the journal “Current Biology”.  As well as academics from the University of Leicester, the research team included scientists from Imperial College (London), Oxford University and Yale.  Tongue worms belong to the Pentastomida Family, part of the Subphylum Crustacea, although for many years the taxonomic relationship between this group of obligate parasites and other parts of the Arthropoda was disputed.

Professor Siveter, explained that the tongue worms were not “worms” at all, they got their name because one genus resembles the tongue of an animal.  They are an unusual and widespread group of mainly obligate parasites.  An obligate parasite is an organism that cannot complete its life-cycle without finding a suitable host.

The professor stated:

“This discovery affirms that tongue worms were “external” parasites on marine invertebrates animals at least 425 million years ago.  It also suggests that tongue worms likely found their way into land-based environments and associated hosts in parallel with the movement of vertebrates onto the land by some 125 million years later.”

The Computer Model with the Ostracod Shell Removed to Reveal the Internal Parasites

Internal parasites identified by high powered scans and computer modelling.

Internal parasites identified by high powered scans and computer modelling.

Picture Credit: Siveter, Briggs, Siveter and Sutton

The computer image above shows the Ostracod with its shell removed, showing the external pentastomids and a pentastomid near the eggs of the Ostracod (parasites in orange).  The picture shows how this group of parasites got their name.  “Penta” refers to the number five and these parasites have five anterior appendages.  One is the simple mouth, the others are two pairs of hooks which they use to attach themselves to their host.  The large pentastomid  (top left) is a highly magnified image of a single parasite, not to scale with the rest of the image.

Using sophisticated microscopic scanning techniques and three-dimensional computer modelling, the scientists were able to reconstruct the Ostracod and its parasites.  Some of the tongue worms were found inside the Ostracod’s shell , near its eggs, on which they probably fed.  Other tongue worms are attached to the external surface of the Ostracod’s shell, a unique position for any fossil or living tongue worm.  These tiny fossilised creatures are helping the scientists to understand a little more about inter-relationships between parasites and potential hosts in ancient marine environments.

Back in 2012, Everything Dinosaur reported on the discovery of another ancient Ostracod from the same location.  The fossil had been identified using the same techniques to discover the parasites.  Professor Siveter, named this new genus of Ostracod after his wife.

To read more about this: Ostracod from Herefordshire, reconstructing the Silurian

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