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No#1 DESTINATION FOR NEW PALAEONTOLOGY DISCOVERIES FOR SHOW-STOPPING SPACES OUT THERE! (51)

Spinosaurus Dinosaur Teeth

The Moroccan Spinosaurus story is a remarkable one, one which could possibly eclipse even the infamous North American Tyrannosaurus rex! Quite a statement, yet think of a world-shattering discovery of a strange dinosaurian partial skeleton in 1915 by a German palaeontologist Ernest Stromer of a new type of dinosaur, this when world war one was raging on the western front, Stromer working in the Egyptian desert couldn't be more detached from the onslaught of modern warfare. Remarkable bones of a large predatory bipedal theropod dinosaur, the first to be unearthed with an enormous sail feature.Rib like dorsal struts which Ernest Stromer theorised supported a great sail which resided mid-dorsal section on the spine of the great reptilian beast, hence the genera name Spinosaurus. These holotype bones were named the Spinosaurus genus, the holotype fossil being the first physical organism discovered of any species, The discovery which names any new genera, from which the specific genus of the animal is derived and scientifically named, the holotype discovery which is always referred back to on any subsequent discovery. This is then the standard used to determine and describe further discoveries of any other similar bones or skeleton when unearthed, it is of no small consequence to exactly how much physical evidence of any first discovery of bones is made in dinosaurs for example, which names the genera or genus, it could be as little as 20% or less or as much 80% of the skeleton recovered, that first physical specimen is perpetually referred to identify the genus within the genera of type from that point onwards.So when in world war two the Munich museum housing the specimen was bombed by the RAF and all the holotype bones lost forever, it was a major loss to the paleontological world. It wasn't until the last decades of the twentieth century Spinosaurus sp. remains would start to be unearthed and identified as Stormers lost dinosaur and another twenty years before Spinosaurus aegypticus would be reassembled from a partial skeletal discovery in the Sahara hamada.One may ask why the Munich museum didn't protect the bones from the bombing raids? Rather, unfortunately, Stromer was knowingly outspoken about the government of the day and the minister of culture in Germany, considered them unworthy of special treatment and prevented such provision, as a slight against Stromer and his collections housed in the museum.Roll forward to the late twentieth century and the museum of Chicago in the guise of Paul Sereno whom had a great interest in North Africa for many years and started work unearthing dinosaurs from North Africa, from Morocco to Niger, from the deserts of these nations Sereno prised dinosaur skeletons of several types, notably Carcharodotosurus, Delta Dromeus Agilis, Suchomimus and most famously the crocodilian reptile Sarcosuchus. Sereno constantly had in his mind Spinosaurus aegypticus which seemed to evade him even through two decades of determined efforts from around 1996 to 2014 working in the field. Palaeontologists only source of reference were the detailed publications of illustrations and photographs from Stromer's expeditions and his life work on his dinosaur collections, the images of Spinosaurus aegypticus tantalised many in the scientific community involved in dinosaurs and their habitats.Eventually, a very positive message was sent to Sereno's office of a rare Spinosaurus specimen discovery. An Italian fossil dealer had purchased a partial skeleton of what was thought to be Spinosaurus aegypticus, this had found its way to the Museo Storia Naturale di Milano. The finds were sent to Chicago. Herewith the help of Nizam Ibrahim whom recognised features in the bone linking them to similar bones he had seen with fossil merchants in Morocco, the trail was picked up as the two together with David Martill, of Portsmouth University and other international palaeontologists backtracked the course of events of the purchase and sale of the dinosaur bones to the enclave of Arfoud in southern Morocco. This is also The Fossil Stores collecting area of expertise and dealing with fossil diggers and merchants. The Fossil Store central base for the last quarter of a century, in North Africa, is among the outer lying desert regions of Erfoud.After a very frustrating sojourn around the fossil beds, in the vast area of that region of the western desert between Morocco and Algeria no more was learnt about the bones in Italy by Sereno and his team traversing from one fossil dig or dealer to another. They were looking for information, where had the Moroc-Italiano skeleton originated from. They needed to locate the fossil horizon and be able to carry out further excavations to determine the paleo habit of the region, that was the ultimate goal. From such excavations and study, they would be able to discern much more about the lifestyle of the dinosaur, than by just studying the bones on the laboratory table.At the last moment when all avenues had been exhausted Nizam recognised a fossil merchant, he had had dealings with and through this chance meeting the fossil merchant declared he had sold the skeleton. The dealer led the team to the place of discovery, which after many hours work between all of the palaeontologists produced more evidence of the Spinosaurus aegypticus skeleton now recently residing in the museum of Natural History Chicago. Only fragmentary pieces, a lot of broken bones and some teeth, but enough to identify that in fact, these few remains did belong to the greater part of the skeleton they had in the laboratory, which was now on temporary loan from the Natural History Museum of Morocco. Eventually, computer-generated casts in resin would be made of every bone and the original bones returned to the museum services in Morocco.From this astounding set of discoveries, much has been learnt about Spinosaurus aegypticus. The skeleton was pieced together using the latest technology. Each bone was scanned and fed into computer programmes to create in exact detail three-dimensional replica bones, these bone replicas were orientated to fit together and work out the basic movements of the animal, through this process much was gleaned about Spinosaurs aegypticus. The skeleton was missing many bones, these were introduced into the software programme from many other sources, other museums had bits of Spinosaurus sp. maybe not all Spinosaurus aegypticus, other types of Spinosaurus were very similar, of the same family tree, until about 40% of the skeleton was created.This gave enough of a clue to the size and frame of the Spinosaurus, which was an amazing, 50 feet in length. The size was truly astounding, making this theropod much bigger than T’rex, as had been expected. The other major predator theropod dinosaur Carcharodontosaurus from North Africa is also bigger than T’rex, however, Spinosaurus was breaking records in many different ways. As scientists studied the skeletal anatomy it became apparent this was no ordinary terrestrial dinosaur. The long snout, dorsally positioned nostrils and enlarged procumbent interlocking teeth are adapted for swimming and snaring slippery prey, like fish! The flat elongated toe-claws are similar to some seafaring birds of today and ideal for paddling. the large dorsal sail can be seen when the dinosaur may be submerged, the short femur and solid leg bones are not normally associated with a theropod dashing around terrestrially for prey. This Spinosaurus bones were not hollow to reduce weight but dense, solid bone which could be the ballast for buoyancy in water. the long snout was ideal for catching the enormous fish of the day, up to 5 feet long sawfish and large sharks, these would be more than enough of a meal for a large predatory dinosaur, on top of this a long tail which after study revealed vertebrae where able to move in a lateral motion in the same way crocodilians do. Coupled with manual unguals, claws which could easily gaff fishy prey, this dinosaur was built for fishing! So an enormous dinosaur has been discovered which would have been the top predator of its day around the watery margins and even a proactive hunter swimmer.As Spinosaurus continues to surprise and delight in equal measure, the science explains the Spinosaurid line was developing towards a crocodilian type of dinosaur, all too sad to be extinguished toward the end of the Cretaceous period, otherwise what would have been swimming up the Nile today! There are many influences and occurrences which play a major role in the overall outcome and extraction process's when considering the value of these Dinosaur fossils and the diminishing resource they are, in this region of the world, particularly of this unique deposition in the Continental Red beds of Kem Kem, which has been proposed as a UNESCO world heritage site. Complete undamaged teeth are limited in occurrence, it requires much work searching, digging and collecting, therefore numerous hours in the field to acquire fine examples.Illustrated here are classic Spinosaurus teeth from a classic fossil site which is producing fewer teeth of quality, as fossil beds become overworked, re-worked and very possibly extinguished due to the finite resource of these fossils coupled with political and military unrest in the region, between two of the most powerful North African states, making collecting along the Moroccan and Algerian border exponentially problematic.  

Museum-quality Spinosaurus fossils for sale by THE FOSSIL STORE for interior fossil Spinosaurus teeth

Fossil Wood Formation

In the case of North America and for want of a better example lets discuss here the great petrified forests of Arizona. These once-great tropical forests experienced a cataclysmic event. Huge trees fossils like the great sequoias of North America today eighty to sixty metres tall were felled and carried off by a great flood. The flood swept the trees away for a great distance, maybe 150-100km eventually depositing thousands of large branchless trunks to a place which is now a desert region. In prehistoric times this was a wetland. The tree trunks had been pretty much stripped of all branches in the rolling action of the flood. The next process and at some point after now partially decayed palaeontologists theorise massive volcanic eruptions took place spewing millions of tons of ash into the atmosphere and down on top of the recumbent forest. The ash layer was several metres deep, as much as eight or nine metres, smoothing the tree trunks, this action took the oxygen out of the environment, whether at that time a shallow lagoon or wetland. This anaerobic environment, or in water an anoxic state, without or with little oxygen restricts microorganisms that normally colonise and break down organic matter. These cannot survive without oxygen and therefore do not get to work to eat away and decay the soft rotting timber. Now the process of petrification can really begin in earnest, the absorption of minerals. Some common silica minerals involved in petrifaction include quartz, calcite, siderite (iron carbonate), and apatite (calcium phosphate), silica’s are amongst the most common minerals in the earth crust. The trees tissues are impregnated by the heavy mineralised water solution, cell by cell the water passing through deposits minerals which eventually crystallise in the tissues of the tree.The final stage is when the cells at the molecular level change and metamorphosis, the remaining organic material, the wood tissues chemically change, the wood ossifies, petrification is taking place, eventually, the petrification of the wood is complete and hardens into stone. This is fossilisation and creates from once soft tissues of living organisms a cast in stone, which displays varying colours which denote the types of mineral content, for instance, red colouration in quartz typically means a concentration of Irons. The image below from our online catalogue illustrates how amazing the transformation of living organic material to petrified stone can be. This amazing tree trunk from Madagascar displays the once-living bark, the many pores and branchlet points, along with the natural creases of the bark clearly seen in their original three-dimensional forms. The green colouration of the bark is due to the mineralisation process and may well denote a heavy concentration of copper, chromium or cobalt.

Museum-quality petrified wood for sale by THE FOSSIL STORE for interior petrified wood display

Shark Teeth Display For Your Interior

Designed and created in-house, The Fossil store brings to you a series of fossil in frames with a signed print. The science is that these teeth are found in a 70 million-year-old fossil bed in the middle of Morocco. A by-product of a state-commissioned mining industry which cuts through arable land. The indigenous family farming communities at this location are the only persons allowed to work and tend the land, the mining region is governed and patrolled as a secure area. The farmers have become fossil hunters and add to their income by selling their finds. The array of well over two thousand amazingly well preserved 70 million-year-old octopus obliquus shark, an ancient mackerel and sand shark tooth display is quite remarkable. The examples here have been finished in a black painted box and glazed frame. Here are other designs and one-off commissions, interior designs which show the versatility of the medium of fossil teeth from this region when used in the frame format. The frames here are finished in white softwood. Browse our catalogue for more ideas and pricing, then contact us to discuss your needs.

Museum-quality fossil diplomystus fish for sale by THE FOSSIL STORE for interior fossil wall design

Ancyloceras Ammonites

Introducing our latest Ancyloceras Heteromorph Ammonite from North Africa, one of a kind and a beautiful presentation for interiors and especially for this ammonoid genus type. With rare inclusions of Nautilus from the Barremian stage, named for the village of Barreme, Alpes de Haute, France. Dating back to the Lower Cretaceous period, approximately 125 million years ago. The story of this unique specimen is one of our recent expeditions to a valley in North Africa where our team selected fine ammonites that our colleagues had excavated and prepared from the fossil limestone layers in the proceeding months before our arrival.As difficult as the extraction process is, the effort is more than worth it, when you see the finished product, you're able to see the calibre of these fine specimens, even we get excited to have them on display in our 'Studio-Lab' and later our Galleries. The inclusion of the nautilus in the commune group is also exceptional for its size, accompanying the Ancyloceras. The wide Nautilus aperture displays very well, amplifying the aesthetically dramatic effect, and if you're a lover of the Nautilus, which is a big trend here at The Fossil Store. We hope you'll love this latest inclusion to our Ammoniodea section under Fossils.

Ammonites for sale

A Gecko lizard captured in time!

A remarkable story of a little gecko that travelled halfway around the world in miles and through hundreds of thousands of years. Our story begins with a transatlantic flight to the largest, if not greatest fossil show in the world in Arizona, each spring for one-month thousands of fossil dealers, collectors, buyers and sellers gather to exchange fossils and catch up with the latest news relating to the palaeontological industry. The fossil store team while attending this venue in 2003, spotted an Australian colleague offering for sale a rare piece of Madagascan copal. As soon as we held and studied the piece of copal which contained a fossilised gecko our heart rates started to react. We are sure It is the same with all disciplines when you find the ‘el dorado’ in your search, your emotions react accordingly. Having had good fortune with similar exceedingly rare pieces ( the first picture of this blog we sold through a London auction house), we immediately negotiated for the gecko. Travelling with another colleague at the time who showed an interest, we agreed to market the piece through his outlet in Harrods of Knightsbridge, in the city of London.On returning home we needed to authenticate the gecko. Our experience and gut feelings assured us to buy the gecko for our online catalogue, however for a resale to a VIP at Harrods we needed written authentication. Here we requested the help of Andrew Ross (department head of the Natural History Museum insects in amber and copal collection), to concur with the identification of the gecko in copal, and that in fact, it was completely genuine, which he did. Later with the help of colleagues and friends with photographic skills ( particularly Peter Green, Surrey, England), we produced a glossy report on the findings and prehistoric history of the little gecko which had travelled from Madagascar to Australia, the United States of America and now to the United Kingdom to be offered for sale at the flagship store Harrods. A meeting was arranged between the Harrods team and the museum buyer from the museum of Qatar, whom at the time were seeking fine and rare fossils for the museum collection. The piece so delighted them they purchased it for the permanent collection.Now the little fellow was on his way again. I often think about the journey of this amazing reptilian, through time and the events which led to its incarceration in the tomb of glutenous tree sap which hardened and lay for millennia, to finally be unearthed cut and polished revealing a perfect amber, coloured window into the ancient tropical forest. To find good inclusions is a rare event, to find a large complete creature the size of this gecko around 70mm in fossil tree resin s extremely rare.The tails of lizards are reasonably commonly found, they break off when the reptilian is in danger, when a gecko gets trapped in the sticky goo the first thing to come away is the tail sure enough, as we know in modern gecko’s the tail is replaceable, in fact the gecko uses this unique adaption to avoid capture by larger predators. The tantalising question one may first ask oneself is why did the lizard risk a sticky end? The answer seemingly lies in the amount of tree sap. When the trees of these prehistoric periods produced resin (sap) it seemingly was in great quantities. Oak husk hairs in baltic amber are common, seeds of fauna and other plant leaf debris is also commonly found in copal and amber, add to these, fruit flies, crane flies, damselflies, weevils, feathers of small birds, butterflies and many other manor of insect and arthropods which inhabit the forests along with anything that the wind can carry up into the canopy and flutter against a tree trunk.The myriad of inclusions became a venus trap of sorts for small spiders, these became trapped and a meal for larger spiders, trapped in the resin which coated bark or hung from branches like stalactites, a smorgasbord of life. Enter our hungry gecko, seeking an easy meal he too became another trapped victim of the sticky sap. Once caught the tree continued producing the sap which like some formaldehyde syrup layered over all the creatures stuck fast. If this occurred quickly enough, the trapped became entombed before other insects or bacteria could spoil them. This is what collectors are hoping to find, a good clean unspoilt and complete lizard specimen.

Lizard in copal

Dinosaur Claws!

Discovered in the fossil deposits situated at the Tegana formation, Kem Kem, southeastern Morocco. Now the arid landscape of the western Sahara desert, formerly a vegetation rich swam region of the warm Cretaceous. An exceedingly rare and Important Spinosaurid dinosaur fossil conserved for scientific study, display or museum exhibit.The fossilised dinosaur claw tissues exhibit an as found condition, which includes fine blood vessels and nerve grooves over the surface of the claw. Excavators use certain methods to strengthen and reinforce all varieties of fossil dinosaur bones to aid the fragile bones removal and transportation to the laboratories of Europe. The rare dinosaur fossil claw now conserved enabling a good presentation view for study, the distal point having some erosion damage in the bedding plane (see our images above), otherwise the claw displaying well-preserved morphology, particularly the blood vessels posteriorly. The curvature of the claw evokes a sense of speed and ferocity, the Spinosaurid was we now know the largest bipedal theropod hunter of its age, a ferocious hunter among the semi-aquatic landscape of what is modern-day Morocco. Spinosaurids range spans from the west to the easternmost parts of North Africa. The story of Spinosaurus aegyptiacus's discovery is as intriguing as the dinosaur itself. Discovered by fossil collector Richard Markgraf in Egypt at the site of El-Bahariya during 1912 in Upper Cretaceous rocks, believed to date to the Cenomanian age around 100 to 93.9 million years ago. Described by the eminent German palaeontologist Ernst Freiherr Stromer von Reichenbachinin in 1915 as world war raged in Europe. Thence housed in the museum of Paläontologische Staasssammlung in Munich up until being destroyed in the second world war by the allied bombers in April 1944. Even though Stromer pleaded to have his precious bones removed to a safe haven. The story of Spinosaurus is as rich as a Hollywood script. Due to the loss of Stromer's partial skeleton, Spinosaurus took a back seat in the Saurischian Dinosaur story until recently with the rediscovery of partial skeletons in Africa. Paul Sereno of the museum of Chicago and his team have made great advances in understanding the remains, with the aid of Stromer's original drawings and accumulated knowledge. Almost 100 years after Stromer identified Spinosaurus, a replica skeleton was unveiled in New York in 2016, to the delight of the media, the largest skeleton of any bipedal carnivore took centre stage. We now understand so much more about Spinosaurus, it had a semi-aquatic lifestyle seeking out large shark type Pristis sawfish, the sawfish had many razor piercing rostral teeth, set in long rostrums. These rostrums were similar to modern-day narrow snouted sawfish. Spinosaurus at over 50 feet long would hunt Pristis shark-like fish, which grew to over 20 feet long. The fish-eating dinosaur would bite down while using its tremendously powerful feet and hand claws to grapple, slash and rip the fish apart. Discovering fossils of this quality is a very rare occurrence and a very exacting and time-consuming process, which requires good local knowledge of the terrain of the desert and considerable technical skill when excavating, if not carried out in a proper fashion fossil can often be badly damaged or completely destroyed. Collected in the continental red fossil formation, Continental intercalaire, at Tegana formation, the province of de Kasr-es-Souk, Kem Kem. The fossil beds are situated in the Moroccan western desert, this area is the northern Sahara of Africa. The Hamada, a raised plateau, is a distinct topographical feature of this region. Here recently the localised political situation has changed, the fossil beds have become overworked, re-worked and the fear is they will become extinguished. Coupled with political and military unrest in the region makes collecting extremely fraught. Less material of a high standard of preservation is being discovered. The Military of both states are active in the region, which is in dispute politically and areas of once accessible Sahara are now impassable. Along with their once productive fossil beds. Older tailings are being re-excavated in the hope better material will be found. These processes are currently making the best fossils more desirable and more valuable. Genus: Dinosauria, Theropoda, Spinosauridae, Spinosaurus Aegyptiacus sp. Stromer,1915.Origin: Tegana formation, province 'De Ksar-es-Souk', Kem Kem deposits, Morocco, North Africa.Age: Mesozoic era, Cretaceous period, Cenomanian to Turonian stages 100 to 89 million years ago. Claw mesial curvature length : 11.6 cmClaw length : 10.0cm Approximate weight: 0,036 g

Dinosaur Fossil Claws

The Latest Editions this January

Claro 2016!! We turn into a fresh chapter, crisp spring air to come brings clarity and we are buzzing with clear idea's to bring in the 'New Year' with selected products for your home interior, gifts for loved ones or friends. Select from Quartz bowls to fossil statement pieces, browse through our catalogue to discover an array of unique fossil and mineral objects procured from around the globe. Our range of magnificent bowls and dishes handcrafted from rock crystal and quartz (peek quartz). Each and every piece is unique containing its own footprint of inclusions, inflexions and imperfections in the now solid formed minerals grown with time and pressure over millions of years. So keep checking back with us as new lines will continue to be introduced to our collections especially in the coming months! 

January sale fossils and minerals

Excavating trilobites!

Finding these invertebrates is not easy work, the local fossil diggers often armed with only hand tools, crowbars, picks, cold chisels and heavy lump hammers, work away at rock faces sometimes in deep trenches hewn out of the mountains and in the desert. The local knowledge which excavators hold and Berber villages they invariably inhabit in the searches of the sparse desert regions, help these fossil hunters hone their techniques and skill for the recognition of trilobites and the patience needed to work in the harsh environments and basic conditions. Often diggers will leave their village homes for several days bivouacking in hot desert oasis and nights in cold mountain huts in the search of the invertebrates. The locations of productive trilobite sites are kept secret as much as possible, however in this land that is not too long! local grapevines trickle the news of new finds and the teams of local diggers layout unmarked claims and set to work. some of these sites are 200-100km into the desert. The terrain such that machinery cannot easily be taken to the source. The fossil hunters have meagre means to supply expensive compressors to drive tools, so all is achieved with man-power only. Work in the heat is lengthy and arduous and the author has often admired the tenacity of these local men eking out an income in uncomfortable positions often for comparatively little gain when considers the weeks and months required to clear tonnes of rock for one 500 gram pebble containing a fossil trilobite. How does one find the fossil trilobites in the fossil-bearing rock? At the fossil site, the fossil bedding seam is broken up into smaller constituent parts, these rocks can be now dinner plate-sized to hand-sized boulders or large pebbles, with a well-practised blow these are cracked in half. This splits not only the rock but also the arthropod in two. If in fact, it is a whole arthropod specimen. All too often it is not, just the glabella, thoracic segment or pygidium (head, body part or tail sections). If it’s a lucky discovery of a full carapace (exoskeleton), of a trilobite the whole boulder is very carefully glued back together. The arthropods body parts are darker than the limestone matrix which entombed it can be easily identified. The chitin carapace which has calcified during the fossil process (per mineralisation), absorbing minerals from the once surrounding seabed silts, can be distinguished and therefore can be located in the pieces of rock. Back in the workshop or laboratory with specialist pneumatic tools and air abrasive techniques with tools driven by compressed air, work begins on the outer surface of the rock very carefully and slowly. Sometimes over days and weeks, broken down mechanically bit by bit. The limestone boulder is by attrition reduced to the desired form. The final process is often to carefully polish the arthropods carapace using fine silicates using a miniature air abrasive or blasting tool. This naturally enhances the colour giving (in the case of black Devonian trilobites), a very bright black sheen over the surface of the carapace and all its pustules, bumps and lumps, along with the segments and lobes of the thoracic body making the arthropod 'jump out' as if still alive in a three dimensional way which is technically referred too as ‘fully inflated’. We hope you enjoyed this brief account of trilobite hunting, we shall post more so keep revisiting our blogs to read more reports and news.

Spiny trilobites

Ammonite Decor Designed For Interior Spaces

Since our humble beginnings; THE FOSSIL STORE™ was the first to present ammonites on mounted stands in'92 and others followed our trend in the '00's. THE FOSSIL STORE™ selections can be seen globally in some of the most iconic buildings from corporations, too royalty and private collectors. It is coming up to the 25th anniversary of our statement line, when we first introduced the Mantelliceras ammonites on limsestone bases, Devonian marble and bronze bases. From the very first edition, we have evolved to these fine piece which we shall discuss here. We feel if you haven’t seen these in person, an explanation of how unique and wonderful these statements are is well deserved. It is not always easy investing in a product online so we would like to present you with our thoughts, facts and more information on these designs. Our unique swivel pin is an ingenious device which enables the heavy Ammonites to be safely seated and also enjoy normally a 360-degree accent. This technical design gave us a standard of mounting above anything previously created.  Our limestone bases are hewn from Portland, mostly, a British Jurassic sedimentary stone. The limestone quarries on Portland have been producing stone and fossils since the Roman occupation of Britain. The cream colour compliments the limestone ammonites of North Africa perfectly. Ammonites date back to the Jurassic and Cretaceous periods from the Atlas Mountain range which is found on the western coastline of North Africa. The black fossil marble with inclusions of many other fossils is from the western Sahara desert, once the desert floor was an ocean bed, the crustacea that swam in the oceans eventually died and their shells were fossilised in the soft silts, this hardened over aeons and became the marble we use today. These marbles are limestones. Limestones are sedimentary rocks. The beauty of the Ammonite form is easily apparent. The Greeks first termed the Egyptian god Ammon, named for his rams horned ears, this a similar form as the Archimedean spiral whorls of the ammonites. Our most decorative ammonites have been cleaned, eradicating the usual iron brown staining, typical of a fossil bed in that region. This cleaning process highlights the creamy tone of the limestone beneath. The surface of the once mineralised shell has a strong ribbing structure. Under the outer shell, the ammonite cephalopod would have lived forming the internal chambers as it grew through its life cycle. Its is suggested the life cycle of the ammonites could have been similar to the modern-day nautili, around 13 chambers a year are added to the internal shell of nautili, it is easily possible to find fossilised ammonite shells commonly attaining around 100 chambers, however it is thought the ammonites could have lived much longer than 20 years. The flagship base is the bronze finished model. With the help of Olga Polizzi, Forte group, a then client of William Yeoward, London. Olga kindly pointed us in the direction of Peter Camden Woodley whom at the time carried much work out for museum exhibits and purveyors of fine art and antiquities. We were delighted to have Peter create our bases in those early days. Since our ammonites have featured in Olga Polizzi’s flagship hotel the Tresanton, St.Mawes, Cornwall.

Ammonites on bronze stand

Fossil marble & Mineral bowls

Introducing something a little different for dining on those special occasions, also one of our favourite and trending lines is our unique collection of quartz and agate bowls, not forgetting the beautiful fossilised and mineralised marble ammonite bowls. The Devonian limestone is hewn from time, or more precisely the Sahara desert, displays within the sedimentary rock a myriad of fossil crustaceans, from Nautilus, Orthoceras and goniatites these marine creatures once swam in the vast oceans of this world and have now formed the base rock of the Atlas mountains at the tip of Africa. Now great blocks of marble are carved into fine handcrafted objects which we hope will delight you. Crafted from these immense block fault lines become apparent, they create a window into the past, in the fault, one can observe the movement of the earth itself. Also highly decorative, making these a nice statement piece and frozen within the marble you can only imagine a timeless sea with an insight into the internal structures of the creatures which can be clearly observed.

Mineral bowls

New Fossil Heteromorphs

New arrivals of fossil heteromorphs and whilst many Ammonoids have retained their spiral form, there are those which have desired other paths to survive natures wrath by uncoiling their spiral over many millions of years, like the Ancyloceras and Audoliceras heteromorph ammonites. Both rare and beautiful in their own right, these ammonites can top the chain when it comes to aesthetics. These wonderous specimens can be found beneath the ground in North Africa however to find one simetrically intact is another dimension altegether. New arrivals of fossil heteromorphs date back to the Mesozoic era, early Cretaceous, Barremian stage, approximately 115 million years ago. Originating from Agadir in Morocco, North Africa. These new arrivals of fossil heteromorphs are genuine fossils have always been difficult to find and it is only becoming more difficult with every year that passes. Many genus types offered on the market today are pieces of several ammonites combined, reconstituted with matrix and similar looking limestone rock found in the same location of the specimens. Our specimens are not artificially re-constructed, we highly dissaprove of this and only invest in the highly esteemed collections available making our sellections all the more desirable. We're excited to introduce our new arrivals of fossil heteromorphs and you can see these under our Ammonoid section from the fossil menu on our website.

Ancyloceras ammonites for sale

Ammonite Extinctions

Ammonite extinctions, Ammonites are one of the most recognisable fossils of our prehistory, Ammonoids reigned supreme in their habitat for hundreds of millions of years, surviving from the Devonian period 417-354,000,000 years through many extinction events, their final demise coinciding with the extraordinary 'KT boundary' Ammonite extinction event at the end of the cretaceous period approximately 65,000,000 years. Throughout these evolving stages of this Cephalopoda group, several extinctions would redefine the habits of the marine invertebrate which would develop into the most strange shaped phragmocone (shells), and also great sizes, by the end of the Cretaceous. The largest types recorded up to 8 feet 6 inches (2.6m), Pachydiscus seppenradensi was discovered in a limestone quarry near the town of Munster Germany C.1895, of Campanian stage, late (upper) Cretaceous Period, around 83-72 m.y.a;  discovered by Theodore Nopco. Theodore sold the ammonite to Professor Dr Hermann Landois (for 125 gold Marks, the average annual salary at the time was 650 Marks), the Dr. founder of the Westphalian Provincial Museum of Natural History. The now fossilised specimen weighs about 3500kg! It is believed that perhaps even larger ammonite lived. It is also theorised ammonites of this monumental size may have lived a more sedate deep water-shelf life, whereas their smaller cousins were pelagic. The ammonite group evolved during the Devonian period, named after the county, Devon in England. The first major blow to the ammonite group was during the Frasnian stage. The Kellwasser event, close to the Frasnian – Fammenian boundary (375 mill yrs ago) and often referred to as the ‘Devonian extinction/Ammonite extinction’ event. Later in the period, again in the Famennian stage, another event saw the demise of not only marine life, but the Hangenberg event also affected marine and land environments. Ammonites became so diverse after the initial Ammonite extinction in the Frasnian stage, due to the lack of competition perhaps, they filled the oceans and ranged globally. Interestingly palaeontologists and geologist found the ammonite a useful aid for dating rock strata, rather than the other way around, this primarily due to the proliferation of ammonites. It wasn’t always so, in the early days of the science of Stratigraphy. William Smith and John Hutton (both scholars equally termed the father of modern-day geology, at various times), noted in the late eighteen century, as they studied the geology of Britain, the importance of the inclusions of fossils in the rock layers. Over the last two centuries many same type ammonites have been found in the rock formations of several continents, thus it has transpired rather than date the rock, then date the fossils contained therein, the fossils have come to define the date of each rock layer, making identification of the age of rock layers expedient for modern-day geologists and historically aiding the formulation of tectonic plate movements. After the Devonian extinction event, the Permian period erupted with more bad news for the ammonite population. In this period two major extinction events are noted, firstly ‘Olsens Gap’ (around 270 - 260 mill yrs ago), it has been difficult to ascertain exactly how long the gap occurred being close to the second major event and so theorist have accessed that more than one event rolled over millions of years, as pulses, these pulses continue through the period several times through the fossil record. An even greater mass Ammonite extinction took place extinguishing almost all the Ammonites, including the goniatites. The ‘Great Permian Extinction’ signalled the end of other life forms including the trilobites, a major invertebrate group. The event was almost for life on our planet, a total extinction event, approximately 96% of marine life, 83% of genera became extinct. A deteriorating climate, anoxic oceans, with possible impact and volcanic events which over millions of years contributed to the catastrophe. It is estimated it took up to 30 million years for life on earth to recover from this apocalyptical period. However, the great survivor ammonites did survive along with brachiopods and nautiluses and of course the reptiles along with several other groups. Some of the main ammonite groups to survive are the Ceratitina and Phylloceratina which prospered and diversified through the Triassic period. Post the ‘Great Dying’, the Triassic again was no friend to the ammonites. By the early Triassic in the Olenekian stage approx 249-247 m.y.a., another extinction event altered life patterns, the Smithian-Spathian extinction occurred. Around the tropics, many species disappeared as surface temperatures reached an estimated 40°C. Later by the end of this period of time, the boundary of the Triassic - Jurassic Period saw once again a major extinction event close the age. No slow degradation this time an abrupt 10,000-year event. Now was the age of the Dinosaurs to enter the stage and proliferate terrestrially, while in the oceans our friends the ammonites lost one major group Ceratitina, however, the family of ammonites survived to once more diversify throughout the Jurassic like never before. The ages of the Jurassic and Cretaceous would define the ammonites like no other period before, up until the infamous KT boundary. KT meaning the Cretaceous-Tertiary, 'K' scientifically is the symbol for the Cretaceous (named Cretaceous after the Belgian geologist Jean d’Omalius d’Halloy C.1822 after his work identified it from chalk strata of the Paris basin), the K is from the German language, derived from the Latin 'creta' (chalk) and in German 'kreide' (chalk), so named the infamous ash layer found around the world donating the abrupt Ammonite extinction-level event.

Cleoniceras Ammonite Opalescent Shell