gemzhub
related to the last post ~Fossilized Pre historic Elephant tooth 🦷🐘
~3.7 KG ~West Java, Indonesia 🇮🇩 ~AVAILABLE.
@earthstory / earthstory.tumblr.com
gemzhub
related to the last post ~Fossilized Pre historic Elephant tooth 🦷🐘
~3.7 KG ~West Java, Indonesia 🇮🇩 ~AVAILABLE.
wightcoastfossils
A 33 million year old molar from the ancient Oligocene mammal Bothriodon, lying amongst the shingle on the Island’s northwest coastline.
Around the size of a large pig, Bothriodon was a member of a bizarre group of mammals that thrived on the Island’s Oligocene coastal plain, the anthracotheres. Ancestors of the modern hippopotamus, anthracotheres first appeared in the Late Eocene in Asia, surviving and thriving until their extinction 2 million years ago! Their fossils are widespread in Oligocene rocks across Europe, Asia and North America and seem to show a close association with ancient wetland environments.
On the Isle Of Wight our Early Oligocene Bouldnor Formation produces the fossils of two different types of anthracothere; the larger Bothriodon and the smaller dog-sized Elomeryx. Their teeth and bones frequently wash up in the shingle and can occasionally be found in-situ within the clays.
These animals probably shared an ecologically similar existence to their descendant the hippopotamus, wading and wallowing in the extensive lakes, ponds and marshlands of the Island’s ancient coastal plain. Their spoon-like incisor teeth perfectly adapted for feeding on the coastal plain’s abundant aquatic plants such as reeds, water lilies and leather ferns. This may in part explain their abundance here, their semi-aquatic lifestyle making carcasses more prone to preservation in the silty muds than the other members of the mammalian fauna.
palaeoart
by Amy Henrici
The new mammoth tooth as viewed from the side. The crown, or exposed part, of the tooth is at the top, and the root is at the bottom.
The Section of Vertebrate Paleontology at Carnegie Museum of Natural History acquires fossils in a variety of ways, most commonly through field work by Section staff, exchanges with other museums, donations, or (very rarely) purchases. The most recent addition to the collection came by way of a donation.
Gary Kirsch discovered the tooth shown above in a sand-gravel bar of a central Ohio stream in 1988 while collecting sediment samples. He had set his sampling equipment on the sand-gravel bar and was moving between the bar and the stream collecting samples. During one of his many forays, Gary noticed an edge of the tooth sticking out of the bar and pulled it out. It was covered in mud, which he quickly cleaned off in the stream to reveal the beautifully preserved tooth, which he identified as that of a mammoth.
Gary recently emailed photographs of the tooth to Assistant Curator of Vertebrate Paleontology Matt Lamanna because he wanted to donate it to the museum. Acceptance of his generous offer required some research: mammoth and Asian elephant teeth are very similar, and because none of the Section staff are experts in fossils of Pleistocene (Ice Age) mammals, we reached out to Pleistocene expert Blaine Schubert at East Tennessee State University, who often uses our collection, to verify Gary’s identification. Blaine was certain that it was a mammoth tooth because an Asian elephant tooth could only have come from a zoo or circus animal, which was highly unlikely. Blaine was curious about how teeth of the two species are distinguished, so he forwarded the photographs to an elephant expert at his university, Chris Widga.
The grinding (i.e., lower, occlusal) surface of the tooth, showing the fairly crenulated tooth enamel.
Chris determined that the tooth is the first (forward-most) molar from the left upper jaw, and because it has fairly crenulated enamel, that it is from a woolly mammoth (Mammuthus primigenius). Through comparison with tooth eruption and wear schedules (sequences) of modern elephants, Chris concluded that the animal was in its late teens to early 20s when it died. In the wild, modern elephants generally live to about their mid-50s, so this single specimen offers a window into mammoth mid-life.
The Section is grateful to Gary for his thoughtful donation. The specimen will be put on temporary display soon in the PaleoLab window on the first floor of the museum for public viewing.
Amy Henrici is the collection manager for the Section of Vertebrate Paleontology at Carnegie Museum of Natural History. Museum employees are encouraged to blog about their unique experiences and knowledge gained from working at the museum.
Fossilized Tapir Teeth. Three molars, an incisor, and a canine tooth.
fossil_librarian Here’s a look at a large tooth from our collection. This is the lower 3rd molar of “Amebelodon” a 4-tusk elephant-like animal that lived in Montana during the Miocene. This specimen was collected in a gravel pit near Deer Lodge in Powell County. 🐘 Necklace by @designosauryeah
Mammoth Tooth This monstrous fossil was found in a gravel pit in Hulín in the Czech Republic. Mammoths used enormous molars like these to chew on hard to process plants, including woody matter. They’re so big that they’re easily preserved, and their presence in places like gravel pits can tell scientists when those pits formed. When these fossil teeth were first recognized and collected in the 18th century, naturalists at the time realized that they were somewhat similar to elephant teeth, but also realized that they didn’t match any known species and it was going to be hard to hide a species making teeth as big as this one. Mammoth teeth like this one were therefore important in the recognition that organisms that had once been on this planet were no longer here – which today we call extinction. -JBB Image credit: https://flic.kr/p/GkuZn2 Reference: https://bit.ly/2H9ozrR
palaeoart This is a quick video I took in the London Natural History Museum last month. This great display showcases the evolution of Proboscidean molars. Tracking from some of the earliest elephant ancestors - the Eocene Moeritherium - to the more recent but extinct Pleistocene Stegodons and Mammoths. This illustrates 40 million years of molar evolution and how teeth adapted to the different vegetation on offer.
A couple of days ago I had the great luck to swim with a Dugong in the Red Sea, Egypt. The dugong is a medium-sized marine mammal. It is one of four living species of the order Sirenia, which also includes three species of manatees. The dugong is the only strictly marine herbivorous mammal. The dugong is easily distinguished from the manatees by its fluked, dolphin-like tail, but also possesses a unique skull and teeth. Its snout is sharply downturned, an adaptation for feeding in benthic seagrass communities. The molar teeth are simple and peg-like unlike the more elaborate molar dentition of manatees. Dugongs are found in warm coastal waters from the western Pacific Ocean to the eastern coast of Africa, they are generally found in warm waters around the coast with large numbers concentrated in wide and shallow protected bays.
This is a real woolly mammoth molar, dredged from the bed of the North Sea!
We can ship this incredible Ice Age fossil worldwide, buy it now on www.SkullStore.ca! You can also browse our products in-person at the Prehistoria Natural History Centre in Toronto! Our address is 1193 Weston Rd and we are open Saturday-Sunday (12-6pm).
Holy cow.