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  1. This is from a classic locality in Ohio known as Linton, which has been collected by both John S. Newberry and E. D. Cope (the famous paleontologist). This plate is also covered in ostrocods (perhap its' last meal?). In front of the skull (right side of plate), t is a coprolite with some paleoniscoid scales).

  2. This specimen represents one of the precious few complete coelacanths known from Jurassic Solnhofen Limestone. This fossil plate has preserved exquisite detail of the fish's delicate structure, adding greatly to its aesthetic appeal and scientific value.

  3. 5" Early Coelacanth Fossil - Bear Gulch. Caridosuctor is a genus of prehistoric coelacanth, a lobe-finned fish, which lived during the Carboniferous period (Serpukhovian stage, about 318 - 326 million years ago). Fossils of it have been found in the Bear Gulch beds of the Heath Formation in central Montana, These limestone layers constitute one ...

  4. This is a nicely preserved, Lower Triassic (247 million year old) Coelacanth fossil from the Middle Sankamenna Formation of Madagascar. Its preserved inside of a concretion that has been broken open (both halves are included) and is 8.7" in length.

  5. A museum-quality specimen of this rare coelacanth (Whiteia woodwardi) with great color and no enhancement of any kind. Lower Triassic (247 mya)Karoo Formation, Anaborana, Madagsacar. Still Life Fossils offers a curated collection of exceptional fossils that have been expertly selected and thoughtfully prepared.

  6. You can find fossils in Ohio at fossil collecting sites in many state parks like Trammel Fossil Park, Oakes Quarry Park, and Caesar Creek State Park. In general, fossils are found in Paleozoic rock formations and include many species of trilobites, brachiopods, crinoids, and more.

  7. 00903 - Museum Grade 6.88 Inch Association of 2 Rare Mawsonia Coelacanth Quadrate Bones. Sold Out. Newest fossils are offered to suscribers first. † Mawsonia, Mawson and Woodward 1907 (coelacanth) Osteichthyes - Coelacanthiformes - Coelacanthidae.

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