Where: New York (43.2° N, 76.8° W: paleocoordinates 25.6° S, 45.7° W)
• coordinate based on political unit
• local area-level geographic resolution
When: Williamson Shale Formation, Telychian (438.5 - 433.4 Ma)
• Age based on correlation chart, Fig. 44.2. Found in both Williamson Shale and Willowvale Shale, which are lateral equivalents.
• formation-level stratigraphic resolution
Environment/lithology: offshore; gray, green shale and siltstone
•
•2003:04:06 SEP Environmental/tectonic/sequence call based on description and Brett et al. (1998). Bulletin New York State Museum 491:89-143. "Williamson-Willowvale interval has been interpretted as the early (maximum) highstand of Sequence IV" (p.107). Also by Lin and Brett (1988). Stratigraphy and disconformable contacts of the Williamson-Willowvale interval; revised correlations of the late Llandovery (Silurian) in New York State. Northeastern Geology.10(3):241-253.
Primary reference: C. E. Brett. 1999. Wenlockian fossil communities in New York State and adjacent areas: Paleontology and Paleoecology. In A. J. Boucot, J. D. Lawson (eds.), Paleocommunities: A Case Study from the Silurian and Lower Devonian 592-637 [M. Foote/K. Koverman/J. Alroy]more details
Purpose of describing collection: paleoecologic analysis
PaleoDB collection 26865: authorized by Michael Foote, entered by Michael Foote on 06.11.2002
Creative Commons license: CC BY (attribution)
Taxonomic list
Chlorophyceae | |
Rhynchonellata | |
Atrypa "reticularis" Linnaeus 1758 | |
Dicoelosia sp. King 1850 | |
Dalejina sp. Havlicek 1953 | |
Resserella sp. Bancroft 1928 | |
Strophomenata | |
Leptaena sp. Dalman 1828 | |
"Eoplectodonta transversalis" = Eoplectodonta (Eoplectodonta) transversalis
"Eoplectodonta transversalis" = Eoplectodonta (Eoplectodonta) transversalis Wahlenberg 1818 | |
Bryozoa | |
| |
Stenolaemata | |
Fenestrata indet. Elias and Condra 1957 | |
Anthozoa | |
Palaeocyclus sp. Milne-Edwards and Haime 1849 horn coral |