Where: Orange County, New York (41.3° N, 74.1° W: paleocoordinates 41.2° S, 26.8° W)
• coordinate estimated from map
• outcrop-level geographic resolution
When: Central Valley Sandstone Formation, Early/Lower Devonian (419.2 - 393.3 Ma)
• The Central Valley sandstone is of Becraft to Oriskany age, with a suggestion that it may prove to be closer to the Oriskany than to the Becraft.
• group of beds-level stratigraphic resolution
Environment/lithology: marginal marine; lithified, white, cherty/siliceous sandstone
•size and is angular. In addition to the detrital minerals there is a large percentage of white chert. The chert is possibly of secondary
•origin because the fossils scattered throughout the sandstone and the chert are
•silicified. The chert bed at the top of the unit may represent a bed that was replaced during weathering rather than primary chert. No information is available as to the time of silicification.
Size class: macrofossils
Preservation: permineralized, replaced with silica
Primary reference: A. J. Boucot. 1959. Brachiopods of the Lower Devonian Rocks at Highland Mills, New York. Journal of Paleontology 33(5):727-769 [L. Ivany/P. Wall]more details
Purpose of describing collection: biostratigraphic analysis
PaleoDB collection 75466: authorized by Linda Ivany, entered by Patrick Wall on 10.10.2007
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Anthozoa | |
Rugosa indet. horn coral | |
Trilobita | |
Proetida indet. Fortey and Owens 1975 trilobite | |
Odontochile sp. Hawle and Corda 1847 trilobite | |
cf. Dipleura sp. Green 1832 trilobite | |
Rhynchonellata | |
? Camarotoechia sp. Hall and Clarke 1893 | |
Hysterolites sp. von Schlotheim 1820 | |
Strophomenata | |
Chonetes sp. Fischer de Waldheim 1830 | |
Leptostrophia sp. Hall and Clarke 1892 | |
Leptaena ? rhomboidalis Wahlenberg 1818 |