Category: Photos/Pictures of Fossils

Notes on Lyme Regis

A Private Fossil Walk Represents Good Value

With the completion of the eastern sea wall at Lyme Regis last year the access to the beach between the town and Charmouth has certainly got easier.  No more climbing over the slippery rocks and the groynes that laid between the end of the beach front and the Church Cliffs.  That might sound like good news and it certainly is, especially for families trying to access the beach.  There is a downside to the new sea defences though, greater access has meant that over the summer months there have been more people than ever scouring the beach between Charmouth and Lyme Regis looking for fossils.  Pickings can be somewhat slim as a result.

The Newly Completed Magnificent Sea Wall at Lyme Regis

Part of the coastal defences at Lyme Regis

Part of the coastal defences at Lyme Regis

Picture Credit: Everything Dinosaur

The sea wall is part of an extensive array of features to help secure the cliffs and the land immediately behind them in a bid to protect the area from further land slips.  Eventually, these defences will give way but the engineering works has probably given the many houses on the cliffs another fifty years of life or so.  Whether or not the sea wall and other defences such as the remodelled beach area close to the famous Cobb has had an impact on the way in which the waves scour the beaches remains uncertain, time will tell, although we have heard from one reliable source that there seems to be a greater amount of sediment deposited out into Lyme Bay.  To help stabilise the cliffs, the slopes have been planted with thousands of small bushes and other plants to help anchor the soil.

The Cliffs have been Planted to Help Prevent Further Land Slides

Stonebarrow and Golden Cap can be seen in the background.

Stonebarrow and Golden Cap can be seen in the background.

Picture Credit: Everything Dinosaur

What Do the Changes Mean for Fossil Hunters?

Lyme Regis has always been a popular destination for would-be fossil hunters. With easier access to the beaches to the east of the town, there is a feeling amongst locals that finding fossils along the shoreline is getting harder.  There are certainly lots of fossils to be found, but large pieces of ammonite and any Ichthyosaur vertebrae are increasingly rare.  For example, during a recent trip to Lyme Regis, we spent a morning on the beach walking slowly up to Charmouth and we were surprised by the lack of fossils.  Belemnite guards were still plentiful, especially as we approached the “Belemnite Beds” but we found no fossils of Promicroceras, which surprised us somewhat.  This small ammonite used to be a relatively common fossil find, there was also a lack of nodules on the beach, although from the scattered shards of split rock there was plenty of evidence of previous visitors having hammered away quite happily at any stone bigger than a house brick, whether or not it was likely to contain a specimen inside.

Not a Very Successful Fossil Hunt

Fossils are becoming more difficult to find at Lyme Regis.

Fossils are becoming more difficult to find at Lyme Regis.

Picture Credit: Everything Dinosaur

Advice for Visitors to Lyme Regis

With the popularity of fossil collecting on the increase and with the easier access to the beach, visitors to Lyme Regis might be disappointed by their lack of fossil discoveries.  One way of helping to get the most out of a visit is to book yourself onto an organised public walk.  There are a number of professional fossil hunters and guides who offer public walks.  These are a very good idea, especially when one considers the risk of getting cut off by an incoming tide or the hazards of rocks falling from the cliffs.  On a public walk your knowledgeable guide should be able to provide you with a very informative tour of the geology and help you to find a few fossils along the way.

Private Fossil Walks are Best

However, if you really want to make the best use of your time, try booking a private walk.  On some public walks that we have observed there can be as many as fifty people in the party.  Simply, getting a question answered amongst a throng of eager fossil hunters that size can be quite an ordeal, even the most dedicated guide can struggle to accommodate everybody’s needs.  Public walks tend to take place on the weekend, a time when the beaches are likely to be congested.  Private walks can be booked at a time to suit you (tides permitting) and you can be assured that your party will be very well looked after by the guide.  You are also more likely to be directed to the best fossil hunting locations, local knowledge wins out every time.  For example, for that beautiful Promicroceras ammonite, your best chance might be to sieve for fossils.  On a private walk, the guide can provide suitable sieves and show you the best technique to help you make your very own fossil discovery.  Knowing exactly where to start sieving on the beach is half the battle.

Still Fossils to be Found but Local Knowledge is Key

Fossils can still be found on the shore.

Fossils can still be found on the shore.

Picture Credit: Everything Dinosaur

Private walks book up very quickly in advance, if you are thinking of visiting the Dorset coast next year, now is an ideal time to get yourself and your family booked on one.  Fossil walks are arranged around safe tide times so be aware that some preferred days may not be suitable.  Most organisers of private fossil walks ask for children to be at least five years old.  Walks take around three to four hours, advice can be provided on where to park any vehicles and as for what you should bring here is a quick check list:

  • Suitable clothing, wellington boots or other stout footwear.  Warm clothing especially in the winter and early spring, having  a waterproof jacket on hand is very sensible, gloves in cold weather too.
  • Bring a snack and a drink although remember to take your rubbish home with you.
  • Bathroom breaks – there are no toilet facilities on the beaches, although most walks commence from the town centre and there are toilet facilities here at the start of the walk.
  • Tools to bring – most guides will be happy to break any nodules open for you, hammers are not usually supplied.  If you do bring your own hammer (please make sure it is a geological hammer), then remember the safety specs and tough gardening gloves.  For advice on the difference between geological hammers and tool box hammers: Geological Hammers What’s So Special About Them?

The fossil walk guide will be able to provide you with the very best chance of finding a top quality fossil and also be able to point out the best places to look.  You will learn a lot more about the history of the local area as well as having the opportunity to get one to one assistance and support.  Private fossil walks really do offer excellent value and they usually cost less than a family three-course meal in a pub.

For further information on private walks (public walks as well), Everything Dinosaur recommends: Lyme Regis Fossil Walks (Public and Private)

Private fossil hunting walks at Lyme Regis can prove to be a very worthwhile investment and provide visitors to the Jurassic Coast with an excellent opportunity to learn more about this fascinating area of Britain.

The Oldest Known Eurypterid

Not Jaws but Claws Pentecopterus decorahensis

Named after an ancient Greek ship (penteconter) which was renowned for its speed and agility, a new and somewhat surprising addition to the mega-fauna of the Middle Ordovician has been described in a paper published in the academic journal “BMC Evolutionary Biology – Bio Med Centre”.  Enter Pentecopterus decorahensis (pent-tee-kop-ter-rus dek-kor-rah-en-sis), which at around 1.7 metres in length suggests that this was an apex predator of the brackish, shallow marine environment represented by shale deposits located in north-east Iowa (United States).

A Very Fearsome Arthropod – P. decorahensis

Ancient predator of the Middle Ordovician.

Ancient predator of the Middle Ordovician.

Picture Credit: Patrick Lynch/Yale University

This armour-plated, marine predator is a member of the Order Eurypterida, an extinct group of Arthropods distantly related to spiders and lobsters.  These creatures are often referred to as sea scorpions as they are distantly related to modern-day scorpions too.  With its streamlined body, grasping limbs for trapping prey and large, well-protected head this formidable carnivore would have dined on a variety of invertebrates as well as jawless fishes.  The fossils are part of the extraordinary Winneshiek Lagerstätte fauna (Iowa) and have been dated to around 467 million years ago (Darriwilian faunal stage of the Middle Ordovician).  Something in excess of 250 different eurypterid species have been described, but only eleven species have been documented from the Ordovician (488-443 million years ago) to date.  P. decorahensis is the oldest known, extending the documented range of the eurypterids by more than nine million years.

Commenting on the fossils, James Lamsdell of Yale University and the lead author of the study stated:

“This shows that eurypterids evolved some ten million years earlier than we thought and the relationship of the new animal to other eurypterids shows that they must have been very diverse during this early time of their evolution, even though they are very rare in the fossil record.”

Some of the Fossil Specimens that have been Found

Examples of fossil specimens.

Examples of fossil specimens, scale bars = 1o mm

Picture Credit: Lamsdell et al

The highly fossiliferous strata was discovered by an Iowa Geological Survey team (University of Iowa), close to the Upper Iowa River.  A temporary dam had to be constructed to allow the fossil site to be excavated. More than 150 fossils of Pentecopterus have been found, many of them representing juveniles.

University of Yale palaeontologist Derek Briggs, a co-author of the study explained that the shale deposits represent an ecosystem that became established when the sea flooded a meteorite impact crater some three miles across.  The weak currents coupled with the oxygen depleted bottom contributed to the remarkable state of preservation of the fossil material.  Even tiny hairs on the limbs can still be seen.

Although, enormous for an Arthropod, it is not the biggest eurypterid known, Everything Dinosaur has reported on a number of very large fossil sea scorpions

To read more about giant eurypterids: Giant Eurypterid Tracks Discovered in Scotland

Giant Devonian Sea Scorpion: Claws! of the Devonian

The largest living member of this Phylum today is the Japanese spider crab (Macrocheira kaempferi), the diameter of the legs of the largest males can be in excess of 3.5 metres and some specimens have weighed more than fifteen kilogrammes.

A spokesperson from Everything Dinosaur stated:

“Thanks to the remarkable Winneshiek Lagerstätte scientists have been able to look into a window of marine life from some 467 million years ago.  Anyone taking a dip in the brackish waters that linked this part of Iowa to the seas surrounding the ancient land mass of Laurentia had better watch out.  This was one Arthropod capable of giving you more than just a “nip” with its claws.”

Cave in the Urals Reveals Haul of Cave Lion Bones

Imanai Cave – Strange Significance to Stone Age People

A team of Russian archaeologists have been putting on display some of the huge collection of prehistoric cave lion bones and other artefacts recovered from a cave in the Russian republic of Bashkiria close to the Ural mountains.  The small cave has yielded some five hundred cave lion bones so far, plus a number of flint spearheads and a cave bear skull that shows evidence of having been pierced by a spear.  The cave, known locally as the Imanai cave, shows no signs of sustained hominin habitation and it has been suggested that prehistoric people considered part of the cave to have some special, perhaps even religious significance and these items were brought into the cave deliberately.

Scientists Show some of the Flint Tools and Cave Lion Skulls

Imanai cave lion skulls on display.

Imanai cave lion skulls on display.

Picture Credit: Pavel Kosintsev

The concentration of cave lion bones in the cave is unique, nowhere else in the world has such a mass concentration of cave lion bones been discovered.  The bone assemblage probably represents six individual animals.

Pavel Kosintsev, a senior researcher at the regional Institute of Plant and Animal Ecology (Urals Branch of the Russian Academy of Science) stated:

“We found about five hundred bones and fragments of bones of the giant cave lion, but there could be more, after we finish with sorting the collection.  Such a large quantity of giant cave lion bones at one site is really unique, the only one in the world so far discovered.”

Giant Cave Lions

The cave lion (Panthera leo) shares the same scientific name of the modern African lion of the savannah.  Although some scientists believe that it is sufficiently different from its African relative to be classified as a sub-species (P. leo spelaea) It may be classified as the same species, by many academics, but the cave lion looked very different from its modern African counterpart.  It was around 15-20% bigger and it had longer legs.  It also possessed a thick, shaggy coat which during the winter months, when snow covered a large part of this animal’s range, that coat might well have turned white to help camouflage this large predator.  It seems that in the past, the lion as we know it today lived over a much wider area of the northern hemisphere.  Its range extended out of Africa and into Europe, indeed cave lion fossils have been found in the UK, most notably Kents Cavern near Torquay (Devon).

Despite their name, cave lions were not adapted to a life in caves, they were creatures of the open tundra, forests and plains.  Their bones may have been washed into caves or brought into cave dens by scavenging animals and as a result, since the bones of these large cats are associated with caves and rock overhangs the term cave lion was adopted to distinguish them from extant species.

An Illustration of a Cave Lion (note the light coloured coat)

An illustration of a cave lion.

An illustration of a cave lion.

Picture Credit: Russian Academy of Science/Pavel Kosintsev

Earlier excavations had found isolated bones deep inside the caves, but these were interpreted as having been sick or injured lions, or lost cubs.  The researchers believe that the cave may have been an ancient sanctuary and that these sick and injured animals could have been brought to the cave by ancient people.  This suggests that the Imanai cave had some significance to the ancient humans that inhabited this part of the Urals, perhaps it was a place of worship.  A number of other such sites were bone deposits have been made are known, the scientists hope to compare their cave data with similar sites from Austria and the Czech Republic.

The human relics found include ten stone spearheads, identified as being from the Mousterian culture, previously only two such spearheads had been found in the entire Urals region of Russia.

Inside the Cave (Imanai Cave Ural Mountains)

Going down to the bone deposit site.

Going down to the bone deposit site.

Picture Credit: Pavel Kosintsev

The Mousterian culture is defined by the style of stone tools associated with European hominins.  It relates to the Old Stone Age and dates from around 600,000 years ago with the youngest tools associated with this culture dating to around 30-40 thousand years ago.  This technology has been found in sites across southern Europe, Turkey and parts of the Middle East.  Mousterian flint tools have been discovered as far west as Wales and the Imanai cave represents one of the eastern margins for this stone tool culture.  During the Mousterian, Europe was populated by a range of hominin species, including Homo heidelbergensis, Homo neanderthalensis and latterly our own species which migrated into this part of the world from Africa – H. sapiens.

Spearheads the Only Sign of Human Activity

The spearheads and the cave bear skull with its spear hole are the only signs of human activity.  If ancient hominins had lived in this cave, even for a short period, the archaeologists would have expected to find a lot more evidence of human habitation.  For example, signs of fire having been used, animal bones with cut marks from being butchered and other stone tools.  The lack of other human artefacts supports the hypothesis that this site might have been a sanctuary of some sort or perhaps a shrine.

The latest finds have not been dated, but the upper layers of the cave floor mapped during an earlier reconnaissance are believed to be around 30,000 years old.  The lower layers are much older, how much older will have a significant bearing on the study, as the scientists cannot be sure what species of people (indeed, the cave could have been an important location to more than one type of hominin) they are dealing with.  Preliminary estimates place the lower, bone yielding layers at around 60,0000 years ago, so this site could be very significant in terms of Neanderthal research.  However, different populations of humans occupied different parts of Europe as the climate swung dramatically from very cold periods to much warmer inter-glacial periods during this part of the Pleistocene Epoch.  Further dating of material is currently being undertaken by scientists from the University of St Petersburg.


Archaeologists Working in the Cave at the Bone Deposit Site

Scientists carefully examining in situ evidence.

Scientists carefully examining in situ evidence.

Picture Credit: Pavel Kosintsev

Explaining the team’s future plans Pavel stated:

“We plan to continue the excavations next year, but the amount of finds we made this year is very large.  There are about twenty sacks with ground and small fragments and about twenty to twenty-five boxes with bones.  We need to examine all this and I think that some significant updates may appear as soon as this year.”

All the bone and tool finds come from an area of just six square metres in the cave, which has been excavated to a depth of around sixty centimetres.  The research team are excited at the prospect of exploring other parts of the cave and finding many more artefacts.  The greater the number of artefacts, then more information can be obtained which should help the scientists to understand more about the cave, its occupants and how it fitted into ancient human cultures.

Fossilised spermatozoa preserved in Annelid Cocoon from the Eocene

Fossilised Spermatozoa from Ancient Annelid

Dinosaurs and other large vertebrates might grab all the headlines when it comes to fossil discoveries but share a thought for those parts of the Kingdom Animalia which do not readily fossilise.  Invertebrate palaeontologists working on the Annelida (segmented worms and leeches), soft bodied creatures, have very few body fossils to study.  As a result, the dedicated scientists which work on them don’t have anything like a complete fossil record of these extremely important creatures.  Trace fossils, such as preserved burrows can help, but the evolutionary history of these ancient animals remains poorly understood.

In contrast, the distinctive egg cases, often referred to as cocoons of the worms that make up the Class Clitellata, are relatively common in the fossil record.  Everything Dinosaur team members have read published papers that explore the fossilised remains of the cocoons from worms that once lived in freshwater environments back in the Triassic.  These preserved cocoons provide valuable additional information as to the diversity of micro-faunas within ancient biotas.  Unfortunately, little work has been carried out so far on the possibility of using such fossils to establish phylogenetic relationships between families and genera.

The worms that make up the Class Clitellata are distinguished from other types of segmented worm, in that they have a “collar”.  It is this “collar”, called the clitellum that gives this Class its name and it is from the Clitellum that the reproductive cocoon is formed.

A Diagram of a Common Earthworm Showing the Clitellum

The Clitellum is marked by an arrow.

The Clitellum is marked by an arrow.

Picture Credit: Everything Dinosaur

A team of scientists from the University of Milan, the Swedish Natural History Museum and the Museo de la Plata (Argentina) have published a paper in the academic journal “Biology Letters” that details the discovery of fossilised spermatozoa (sperm) preserved within the secreted wall layers of a fifty million year old clitellate cocoon found in Antarctica.  This material represents the oldest fossil animal spermatozoa yet described.

The specimen was collected during a field expedition to the remote Seymour Island, one of a group of small islands at the tip of the Antarctic Peninsula.  The Island is extremely significant to palaeontologists as the strata exposed dates from the Late Cretaceous, the Palaeogene and into the early part of the Neogene (Eocene Epoch).  Fossils found on Seymour Island include marsupials, proving that in the past terrestrial mammals lived on Antarctica, but the rocks have proved most useful in helping scientists to plot climate change, including the global cooling during the Eocene that led to the glaciation of the Poles.

Strontium isotope dating gives an age of approximately fifty million years for the fossilised spermatozoa (Ypresian faunal stage of the Eocene), the fossil find was made by chance as a single worm fragment just 0.8 mm wide was studied using a scanning electron microscope.  A three-dimensional model was then created using sections of the fragment that had been examined under X-ray microscopy.

A Fragment of the Fossilised Worm Spermatozoa

Ancient remains - scale bar = 1 micron.

Ancient remains – scale bar = 1 micron.

Picture Credit: Swedish Museum of Natural History (Department of Palaeobiology)

When closely examined, the clitellate was found to consist of a solid inner wall, just one fortieth of a millimetre thick.  In addition, there was a spongy, outer layer of loosely interwoven cables between 100th and 200th of a millimetre in thickness.  The scientists were able to observe images of the microscopic cells embedded in the cocoon wall, including rod-shaped structures with a whip-like tail.

Modestly commenting on the discovery, Benjamin Bomfleur, a palaeobotanist at the Swedish Natural History Museum remarked:

“It was an accidental find.  We were analysing the fragments to get a better idea of the structure of the cocoon.  When we zoomed into the images, we started noticing these tiny biological structures that look like sperm.”

A Worm Mystery

Working with biologists the team were able to conclude that the fossils resemble the sperm of extant freshwater crayfish worms (Branchiobdellida), although since these worms are only found in the northern hemisphere it remains a mystery as to whether or not the Antarctic fossil specimen is closely related.  How the fossils came to form in the first place is a little bit of a puzzle too.

Diagram Illustrating the Inferred Method of Fossilisation of Microorganism (Clitellate Cocoons)

Inferred fossilisation process.

Inferred fossilisation process.

Picture Credit: Biology Letters

In the diagram above, the common medicinal leech is used to illustrate a potential theory of how the fossil preservation occurred.  Two leeches mate (a), a cocoon is secreted from the clitellum (b), then eggs and sperm are released into the cocoon before the animal retracts and eventually deposits the sealed cocoon on a suitable substrate.  Spermatozoa and microbes become encased in the solidifying inner cocoon wall (d).

The scientists anticipate that this accidental discovery will permit systematic surveys of cocoon fossils coupled with advances in non-destructive analytical techniques that will open up new opportunities to explore the evolutionary relationships of minute, soft-bodied animals that are otherwise so rarely found in the fossil record.

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

Fossil Site Threatened (Hall Dale Quarry)

Former Quarry Could be Transformed into Housing and Commercial Development

The huge Hall Dale Quarry near Matlock, Derbyshire, could be transformed, with the potential loss of an amazing fossil location, if the local authority grants permission for a mixed residential and commercial development on the site.  Hall Dale Quarry is a disused limestone quarry.  We at Everything Dinosaur, don’t know when the quarrying of limestone blocks ceased, what we do know is that the rocks exposed at this location contain a huge diversity of Carboniferous invertebrate fossils.  Fossils are extremely common at the quarry, whilst many amateur collectors split the boulders with heavy-duty chisels to access the fossil material, just a few minutes exploring the scree on the quarry floor will yield plenty of specimens.  Fossils of a variety of Brachiopods, Crinoid stems and large Corals litter the site and with careful searching some nice examples of marine Gastropods (mainly internal moulds), can be discovered too.

The strata represents a shallow, marine environment and the rocks at the quarry are part of the Eyam limestone formation.  They date from the Early Carboniferous (Visean faunal stage of the Middle Mississippian Epoch [345-328 mya]).  The site is hidden from the road and is approached via a small path leading through a wooded area, although it is just a few minutes’ drive from the bustling centre of the Derbyshire market town of Matlock, once at the quarry face, it’s a different world.  On the day Everything Dinosaur visited, the quarry was deserted, we did not see a single person for the best part of three hours.

A View from the Helicopter Pad at Hall Dale Quarry

Hall Dale Quarry (Derbyshire)

Hall Dale Quarry (Derbyshire)

Picture Credit: Everything Dinosaur

The rock strata forms a series of platforms (three in total), Hall Dale Quarry is a popular location with climbing clubs, the sheer rock faces and huge piles of stone provide plenty of different climbing routes to explore.  We would advise that fossil collectors stay on the ground level, there are plenty of fossils to be found and there is no need to climb the boulders.

Enormous Boulders at Hall Dale Quarry

Huge boulders - can you see our rucksack?

Huge boulders – can you see our rucksack?

Picture Credit: Everything Dinosaur

During our research, prior to our fossil hunting trip, we visited the excellent website of UK Fossils: UK Fossils.  As we prepared for our visit, we came across a news article from November 2014 that outlined plans for the development of this rural space, what is termed a brownfield site.  4M Property Partners had submitted plans to convert the quarry into a development consisting of mixed residential and commercial properties.  Plans had been submitted to the council to build some 220 houses, and to convert 400 square metres into a restaurant and a café.  In addition, the planning proposal contained details of some 6400 square metres of office space.  We at Everything Dinosaur are not sure exactly how fossil collecting would be affected by these developments, we are also unsure as to how the planning application has progressed.  However, we would like to express our concern that such an amazing place might be lost forever.

Whilst we can appreciate that Matlock, like many towns in the UK, may have a need for more houses and that such a development might boost the local economy, as we stood in the quarry, totally in awe of the spectacular scenery and surrounded by evidence of a tropical, marine environment that existed some 340 million years ago, it seemed such a shame that this location might soon be unrecognisable.

Many Different Types of Invertebrate Fossil can Be Found in the Scree

Fossils can be found in the scree.

Fossils can be found in the scree.

Picture Credit: Everything Dinosaur

There may be an urgent need for more local housing.  The town of Matlock might desperately require additional commercial properties.  We feel that we are unable to comment with regards to these development plans, but we sincerely hope that the developers have at least considered the need to preserve some part of this remarkable location’s fossil heritage.  There are fewer and fewer places in this country, where people can simply stop and stare and admire rock formations and the fossil treasures they contain within.  These special sites demonstrate the rich geology of our landscape and allow visitors to explore life in the past.  We hope that any development is undertaken in sympathy with the astonishing geology of this location.

A Few Minutes Collecting and So Many Fossils

A multitude of fossils can be picked out from the scree.

A multitude of fossils can be picked out from the scree.

Picture Credit: Everything Dinosaur

Wishing to express our concerns, the team member who visited the site contacted the planning department of Derbyshire Dales District Council.  A very helpful person in the department explained that the planning team could be emailed, allowing concerns about the need to develop the location in sympathy with the geology of the area to be put on record.  Everything Dinosaur subsequently did this and in addition, emailed Natural England to raise awareness of the development of this brownfield site with that organisation.

Raising Awareness About the Potential Loss of the Quarry

If you have collected fossils at Hall Dale Quarry and wish to make a point with reference to the re-development of this site and the potential loss of this fossil collecting location, then we would urge you to do so.

Planning application reference: 14/00541/OUT (please quote this reference when emailing the planning department or Natural England).

Email: to contact Derbyshire Dales District Council (we would advise that you include a contact telephone number in your email, so that a planning team member can get in touch)

Email: (again quoting planning reference: 14/00541/OUT) to get in contact with Natural England

Whilst we do understand the difficult and often challenging job of district councils and we aware of the potential economic benefits to the local community this project may bring.  We at Everything Dinosaur feel that it is important, to at least place on record a desire to consider the development of Hall Dale Quarry which takes into account the remarkable fossil bearing strata to be found at this location.

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Giant Ordovician Filter Feeder Provides Clues to Arthropod Evolution

Two Metre Long Aegirocassis benmoulae Expands Ecological Role of Anomalocarids

A beautifully preserved fossil of a giant Arthropod from Morocco is helping palaeontologists to gain a better understanding of the evolution and the development of the Arthropoda as well as providing a new perspective on the fauna that formed an extensive and diverse ecosystem in an Early Ordovician sea.

The Arthropoda are the largest phylum in the Kingdom Animalia and the first fossils of these segmented creatures with their hard, external skeletons date from the Early Cambrian.  Characteristics of these animals include that exoskeleton, a segmented body plan and paired, jointed appendages that can perform a variety of functions, such as swimming, walking and feeding.  Typical Arthropods include crustaceans, spiders, king crabs, scorpions, mites and insects, all very familiar to us today. Extinct forms include the Trilobita and the anomalocarids, one of which turns out to be a two metre long giant that fed like a baleen whale.

A team of researchers including scientists from Yale University and the University of Oxford have been examining the three-dimensional remains of this strange, new type of anomalocarid in a bid to understand how the Arthropods diversified and those highly adaptable paired, jointed appendages first evolved.  It could be argued that it is the Arthropods that dominate animal life on our planet.  As a phylum they have adapted to a huge range of different habitats and they make up over eighty percent of all described animal species.  Enter into the debate, a newly described anomalocarid named Aegirocassis benmoulae.  The anomalocarididae family are long-extinct.  However, they are regarded as basal members of the Arthropoda and their fossil record extends from the Cambrian into possibly the Devonian, although Devonian anomalocarids remain a controversial area of palaeontology due to differing interpretations of fossil material.   These marine creatures grew to very large sizes in relation to other marine fauna and the majority of them were nektonic predators.  However, A. benmoulae evolved in a very different direction.

An Illustration of the Giant Aegirocassis benmoulae – Filter Feeder of the Early Ordovician

An early, filter-feeding giant.

An early, filter-feeding giant.

Picture Credit: Marianne Collins, ArtofFact

The anomalocarids were like no living animal today.  The mouth was circular on the underside of the head and surrounded by frightening, jagged (in most cases) hard tooth plates, designed for crushing the exoskeletons of other Arthropods.  The large, compound eyes gave these active hunters an excellent all-round field of vision and at the front of the head was a pair of spiny, grasping appendages used to grab prey.  Their elongated, segmented bodies had flaps on the side that were used for propulsion.  Until the discovery of A. benmoulae it had been believed that anomalocarids had only one set of flaps per body segment and that they had completely lost their walking legs.

The fossils, which have been preserved in three dimensions, an extremely rare preservation state for an Arthropod, come from the Draa valley in south-east Morocco.  The sediments were formed at the bottom of a deep sea and the strata has provided palaeontologists with an insight into life in the Early Ordovician.  Very occasionally violent storms disturbed the seabed and buried large numbers of animals.  These events led to the formation of a very rich Lagerstätten, which has helped scientists to map the pace of evolution from the Cambrian explosion some sixty million years before these fossils formed to the end of the Ordovician some 443 million years ago.  The fossils from this part of Morocco form the Fezouata Biota, representing a marine habitat dating from around 485-480 million years ago.

To read about the discovery of a giant, predatory anomalocarid from the same region of Morocco: Giant Marine Predator of the Ordovician

The description of Aegirocassis benmoulae provides new evidence for Arthropoda evolution.  The exquisite preservation reveals that anomalocaridids had in fact, two separate sets of flaps per segment.  The upper flaps equate to the upper limb branch of modern Arthropods, while the lower set of flaps represent modified walking limbs that were adapted for swimming.  A reassessment of older anomalocarid fossilised remains also show two separate flaps per body segment.  The scientists have concluded that the anomalocaridids represent a stage of Arthropoda evolution before the fusion of the upper and lower appendages that form the double-branched limbs of extant Arthropods.

Peter Van Roy, an associate research scientist (Yale University) and an authority on the Fezouata Biota stated:

“It was while cleaning the fossil that I noticed the second, dorsal set of flaps.  It is fair to say I was in shock at the discovery and its implications.  It once and for all resolves the debate on where anomalocaridids belong in the Arthropod tree and clears up one of the most problematic aspects of their anatomy.”

As if to reflect the adaptability of the Arthropoda bauplan, it seems that this Moroccan giant evolved to exploit the abundance of small marine organisms that flourished in the Early Ordovician.  The head appendages that formed the spiky, grasping claws of this anomalocarid became modified into delicate filter feeding apparatus.  It is likely that this creature cruised the oceans feeding on tiny plankton and other organisms floating on the currents just like modern baleen whales, manta rays and whale sharks.

A Close up Showing the Delicate “Fronds” of the Filter Feeding Net

Delicate feeding apparatus.

Delicate feeding apparatus.

Picture Credit: Peter Van Roy (Yale University)

The picture shows a close up of the prepared fossil material showing the delicate fronds which the creature used to sieve sea water for food (scale bar = 10 mm).

Commenting on the implications for Early Ordovician ecosystems, c0-author of the scientific study, Dr. Allison Daley (Oxford University’s Department of Zoology) stated:

“These animals are filling an ecological role that hadn’t previously been filled by any other animal.  While filter feeding (filtering water to find food) is probably one of the oldest ways for animals to find food, previous filter feeders were smaller, and usually attached to the sea-floor [benthic].  We have found the oldest example of gigantism in a freely swimming filter feeder.”

Carnivorous Plant Remains Found Preserved in Amber

The Mystery of The Very First Carnivorous Plant Fossil Leaves

Some types of organism, despite having been on our planet for tens of millions of years have such a poor preservation potential that they rarely, if at all appear in the fossil record.  One such group are the carnivorous plants, be they Venus Fly Traps, Sundews or Pitcher plants.  The trapping structures are often derived from primary growth, this reduces the preservation potential and these types of plants tend to be found in areas such as peat bogs and tropical forests where rapid breakdown of organic material occurs.  Up to now, carnivorous plant fossils have consisted of micro-fossils such as preserved pollen with the occasional fossil seed.  However, a team of scientists from the Botanical State Collection of Munich as well as Bielefeld and Göttingen Universities have found the first fossils of a proto-carnivorous plant preserved in Baltic amber.  Two leaves, trapped in pine resin over between thirty-five and forty-seven million years ago, have been identified to belonging to the family of flypaper plant traps.  These types of plant produce sticky substances that trap small insects and other Arthropods.

The sticky hairs on the leaves can be clearly made out under a microscope.  The amber was found in a mine near Kaliningrad, the Russian enclave on the Baltic coast.  Amber from this part of the world, referred to as Baltic amber is relatively common and remarkably as amber floats in sea water, from time to time pieces of Baltic amber are washed up on the coast of East Anglia (United Kingdom).

The Fossils of a Carnivore (Roridula spp.)

Leaf remains trapped in amber.

Leaf remains trapped in amber.

Picture Credit: PNAS and University of Göttingen/Alexander Schmidt.

Writing in the Proceedings of the National Academy of Sciences (United States), the research team led by Professor Alexander Schmidt (University oGöttingen), have identified the leaves, with their long-stalked multicellular glands as being reminiscent of extant plant species in the Roridula family.  Plants in the family Roridulaceae are not true carnivorous plants in the strictest botanical sense.  In contrast to the likes of the Venus Fly Trap (Dionaea spp.), Roridula do not trap, kill and digest their animal prey.  These plants are not capable of producing the enzymes required to breakdown the bodies of their victims.  Instead, they rely on a symbiotic relationship between types of carnivorous Heteropteran insects (bugs), that feed on the trapped organisms.  In turn, the nutrient rich excretions from these scavengers are absorbed by the plant through its leaves.

Today, living members of the carnivorous plant Roridula are restricted to southern Africa, however, during the Eocene these plants must have been much more widespread.  For much of the Eocene Epoch, the world was warmer than it is today.  The discovery of these fossils provides a mystery for the research team to solve.  Firstly, it suggests that the flora in the forests that were to produce the tree resin that was to eventually become amber, must have been more diverse than previously thought.  Secondly, it had been thought that the ancestors of the Roridula evolved around 90 million years ago in Africa and these plants evolved in isolation as Africa became separated from other land masses as the southern super-continent of Gondwanaland broke up.

However, as Professor Schmidt points out:

“The new fossils from Baltic amber show that the ancestors of Roridula plants occurred in the northern hemisphere until around 35 million years ago, they were not restricted to South Africa.”

These plants seem to be have been more widespread than previously thought, the fossils also confirm molecular dating that hypothesised that these types of plant had been distinct from other plant families for at least 38 million years.

Everything Dinosaur acknowledges the help of the University oGöttingen in the compilation of this article.

Mary Anning at the Natural History Museum

Being Associated with the Wrong Marine Reptile

As team members from Everything Dinosaur travel around they sometimes get the chance to visit a natural history museum whilst out on their adventures.  There are many splendid museums in this country and elsewhere in the world and it is great fun looking at the various fossils held within the collections.  Occasionally, we come across an exhibit that has inaccurate or out of date information, mistakes do occur and we are always appreciative of the time and trouble curators take over their particular charges.

One such anomaly can be seen in the Fossil marine reptiles gallery in the Natural History Museum London.  There are some spectacular marine reptile fossils on display, Ichthyosaurs, Pliosaurs and their close cousins the Plesiosaurs.  The fossil specimens (most of them are casts) are truly astonishing and this museum (quite rightly in our opinion), does much to acknowledge the contribution of Mary Anning to the nascent science of palaeontology and her work excavating and describing fossils of ancient Jurassic marine vertebrates preserved in the cliffs on the Dorset coast around Lyme Regis.

Information about Mary Anning and her work can be found on various information boards on display.  However, one thing that has always puzzled us is that there is a prominent information board about Mary located on the Rhomaleosaurus cramptoni cast, Mary Anning had nothing to do with this specimen, its discovery or research into it.  In fact, she died about a year before this specimen was found.

Wonderful Marine Reptile Exhibits – but Nothing to Do with Mary Anning

Mary Anning died before this fossil was discovered.

Mary Anning died before this fossil was discovered.

Picture Credit: Everything Dinosaur/Rebor

The specimen in the photograph is not a fossil but a cast, a copy of the fossil which was made very probably in the late 19th Century by the American Henry Augustus Ward, who set up one of the world’s first fossil dealers and provider of museum replicas and casts.  The animal that the cast represents is called Rhomaleosaurus cramptoni.  It is pronounced Row-ma-lee-oh-sore-us.  It is mounted on the wall of the fossil marine reptiles gallery in the Natural History Museum, but we are aware of similar casts of the same fossil specimen in Monash University (Victoria, Australia), Cornell University, (New York USA), University of Illinois,  and the Bath Royal Literary and Scientific Institution (Bath, Somerset).

The actual fossil is part of the National Museum of Ireland (Natural History), Dublin, Ireland, we don’t think it is on current display.  The code for the specimen is NMING F8785 (all significant fossils are given a unique identifier, this helps when searching for information on a particular specimen).

A Model of the Fearsome Rhomaleosaurus cramptoni

A super model of a marine reptile.

A super model of a marine reptile.

Picture Credit: Everything Dinosaur

Rhomaleosaurus means “strong lizard” an appropriate name for this fearsome predator that grew to more than six metres in length and might have weighed as much as 1,000 kilogrammes.

Fresh Rockfalls at Monmouth Beach (Lyme Regis)

Warnings for Fossil Hunters at Lyme Regis

The cliffs that surround the picturesque town of Lyme Regis in Dorset on England’s famous “Jurassic Coast” are very treacherous.  Rockfalls and landslips are a relatively common occurrence and team members at Everything Dinosaur, have done much to help inform and to warn visitors to the area of the potential hazards.  Fossil collecting or simply exploring the beaches can be a lot of fun, but the recent cliff fortification and shore stability measures put in place by the local council will not solve the problem of the unstable geology of the area.   The cliffs are composed of relatively loose sediment, that when saturated after heavy rain or somewhat dried out after a prolonged spell without too much precipitation, are prone to rockfalls.  It is always advisable to stay well away from the base of the cliffs, fossil collecting on a falling tide helps, as this gives an increasing distance between the sea and the cliffs.

Dangerous Cliffs at Lyme Regis

Good idea to go fossil collecting on a falling tide and to keep away from the steep cliffs.

Good idea to go fossil collecting on a falling tide and to keep away from the steep cliffs.

Picture Credit: Everything Dinosaur

Recently, we were sent some photographs by Lyme Regis fossil expert, Brandon Lennon.  The photographs showed a rockfall that had taken place on Monmouth beach (to the west of Lyme Regis).  Brandon explained that he had observed a number of cliff falls this year and that he expected more to occur as the autumn weather sets in.   This particular rockfall had occurred on that area of the beach famous for its extensive ammonite and nautiloid fossils preserved within the blue lias limestones – an area known as the “Ammonite Pavement” or the “Ammonite Graveyard”.

Recent Rockfall at Monmouth Beach

Rockfall onto the Ammonite Pavement on Monmouth Beach.

Rockfall onto the Ammonite Pavement on Monmouth Beach.

Picture Credit: Everything Dinosaur

A supervised, fossil collecting walk is one of the best ways to explore the beaches around Lyme Regis, for further information on such tours: Fossil Walks in the Lyme Regis Area

Perhaps if you are lucky enough to go on a field trip with Brandon to Monmouth beach, you might be able to hear the theories that have been proposed to help explain why so many large ammonite fossils are found together at this spot.

Everything Dinosaur was sent a beautiful piece of fossilised wood from nearby Portland.  The specimen still had the bark preserved on it and when polished in section, growth rings could still be made out. We think that the fossil represents an Araucaria spp. (monkey puzzle tree).  This fossilised wood dates from the Upper Jurassic.  Fossil wood can occasionally be found on the beaches of Lyme Regis and nearby Charmouth, but this is usually much older dating mainly from the Lower Jurassic.

A Polished Section of Fossilised Wood

A polished section of fossilised wood.

A polished section of fossilised wood.

Picture Credit: Everything Dinosaur

Remember if fossil collecting, be careful out there.

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