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Found 7 results

  1. I have up for offer this little fella. He's not perfect, but he's a cute little ~2cm prone Eldredgeops rana with a nice little coral in association. He's got something weird going on on the right portion of his cephalon into the first few pleurae, but has really nice color and a great personality. I prepped him out to a degree, but I don't want to risk losing any more of his already damaged glabella. I'm offering him up in trade for another equally disrupted trilobite. Message me with any interest!
  2. Ambocoelia umbonata (Conrad 1842)

    Found as surface float near the top of the Windom exposure, a few feet below the Genundewa Limestone at Penn-Dixie Quarry in Hamburg, NY. A very common fossil in Hamilton Group sediments. Similar to Emanuella praeumbona, distinguished from E. praeumbona by the hinge width; the hinge of A. umbonata spans the width of the valve, while that of E. praeumbona is narrower. A. umbonata has a nearly flat brachial valve, while that of E. praeumbona shows a convex profile. Full-sized specimens of A. umbonata are also not as large as E. praeumbona. Originally designated Orthis umbonata. A. umbonata has been defined as the type species of Ambocoelia by Hall. References: Wilson, K. A. “Field Guide to the Devonian Fossils of New York” (2014). Paleontological Research Institution Special Publication No. 44. Linsley, D. M. “Devonian Paleontology of New York” (1994). Paleontological Research Institution Special Publication No. 21. Hall, J. Palaeontology of New York v. 4. (1867) Fossilworks. http://fossilworks.org
  3. Emanuella praeumbona (Hall 1857)

    Found as surface float near the top of the Windom exposure, a few feet below the Genundewa Limestone at Penn-Dixie Quarry in Hamburg, NY. Distinguished from Ambocoelia umbonata by the hinge width; the hinge of A. umbonata spans the width of the valve, while that of E. praeumbona is narrower. E. praeumbona also shows a convex profile to the brachial valve, and grew to a larger size. E. praeumbona is common in the Hamilton Group only within the upper layers of the Windom Member. Originally designated Orthis praeumbona, later assigned to Ambocoelia, then reassigned to Emanuella in 1990. References: Hall, J. Palaeontology of New York v. 4. (1867) Fossilworks. http://fossilworks.org Yale Peabody Museum Collections website (http://peabody.yale.edu/collections/invertebrate-paleontology) Brett, C. E. Biostratigraphy and Paleoecology of the Windom Shale Member (Moscow Formation) in Erie County, NY. 1974. State University of New York at Buffalo.
  4. Camarotoechia prolifica (Hall 1867)

    Found as surface float on the scree pile at the Windom exposure. Originally assigned to Rhynchonella prolifica, currently assigned to Camarotoechia. Appears to have been assigned to several genera over time, including Stenocisma and Cupularostrum. Refs: Linsley, D. M. Devonian Paleontology of New York. (1994) Paleontological Research Institution Special Publication 21. Hall, J. Palaeontology of New York v. 4. (1867) Yale Peabody Museum Collections website (http://peabody.yale.edu/collections/invertebrate-paleontology)
  5. Cyrtina hamiltonensis recta Hall 1867

    Found as surface float on the scree pile at the Windom exposure. Refs: Linsley, D. M. “Devonian Paleontology of New York” (1994). Paleontological Research Institution Special Publication No. 21. Hall, J. Palaeontology of New York v. 4. (1867) Yale Peabody Museum Collections website (http://peabody.yale.edu/collections/invertebrate-paleontology)
  6. Cyrtina sp.

    Found as surface float on the scree pile at the Windom exposure. Possible undescribed species of genus Cyrtina. Closely resembles C. hamiltomensis, but surface is smooth and punctate, rather than covered in tiny spicules. Also differs in that extremities are slightly rounded, rather than squared, and height of interarea is equal to the width rather than smaller. References: Ehlers, G. M. Cyrtina Hamiltonensis (Hall) And A New Species Of This Brachiopod Genus From New York. Contributions From The Museum Of Paleontology The University Of Michigan Vol. XVIII, No. 12, pp. 197-204 (1963). Linsley, D. M. Devonian Paleontology of New York. (1994) Paleontological Research Institution Special Publication 21. Wilson, K. A. Field Guide to the Devonian Fossils of New York. (2014) Paleontological Research Institution Special Publication 44. Hall, J. Palaeontology of New York v. 4. (1867) Fossilworks. http://fossilworks.org Yale Peabody Museum Collections website (http://peabody.yale.edu/collections/invertebrate-paleontology)
  7. Ambocoelia umbonata (Conrad 1842)

    Found as surface float on the scree pile at the Windom exposure. A very common fossil in Hamilton group sediments. Similar to Emanuella praeumbona, distinguished from E. praeumbona by the hinge width; the hinge of A. umbonata spans the width of the valve, while that of E. praeumbona is narrower. A. umbonata has a nearly flat brachial valve, while that of E. praeumbona shows a convex profile. Full-sized specimens of A. umbonata are also not as large as E. praeumbona. References: Wilson, K. A. “Field Guide to the Devonian Fossils of New York” (2014). Paleontological Research Institution Special Publication No. 44. Linsley, D. M. “Devonian Paleontology of New York” (1994). Paleontological Research Institution Special Publication No. 21. Hall, J. Palaeontology of New York v. 4. (1867) Fossilworks. http://fossilworks.org
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