Beecher's Trilobite Bed
| Beecher's Trilobite Bed Stratigraphic range: Late Ordovician (Caradoc, c.445 Ma) |
|
|---|---|
| Type | Geological formation |
| Unit of | Frankfort Formation |
| Area | Small quarry only |
| Thickness | 3-4 cm |
| Lithology | |
| Primary | Shale |
| Location | |
| Coordinates | 43°15.2′N 75°24.5′W / 43.2533°N 75.4083°W |
| Region | Oneida Co., New York. |
| Country | USA |
| Extent | Very limited |
| Type section | |
| Named for | Charles Emerson Beecher |
Beecher's Trilobite Bed is a Konservat-Lagerstätte of Late Ordovician (Caradoc) age located within the Frankfort Shale in Cleveland's Glen, Oneida County, New York, USA. Only 3-4 centimeters thick, Beecher's Trilobite Bed has yielded numerous exceptionally preserved trilobites with the ventral anatomy and soft tissue intact, the soft tissue preserved by pyrite replacement. Pyritisation allows the use of X-rays to study fine detail of preserved soft body parts still within the host rock. Pyrite replacement of soft tissue is unusual in the fossil record; the only Lagerstätten thought to show such preservation were Beecher's Trilobite Bed, the Devonian Hunsrück Slates of Germany, and the Jurassic beds of La Voulte-sur-Rhône in France, although new locations are coming to light in New York state.
Originally discovered in 1892 by William S. Valiant, the site was thoroughly excavated from 1893 to 1895 by Charles Emerson Beecher (after whom the location is named) of Yale University, after which time the location was thought to be exhausted of fossils and excavations ceased. Beecher published three papers describing a trilobite larval form, trilobite limbs and trilobite ventral anatomy from material collected from the site he established. Beecher died unexpectedly in 1904; much material, as well as details of the location, was lost. Research was subsequently limited to study of material collected during the original excavations that had been distributed to various institutions.
Amateur fossil collectors Tom E. Whiteley (also responsible for rediscovering the Walcott-Rust quarry) and Dan Cooper rediscovered the location in 1984 and from 1985 academic excavations and studies (re)-commenced. At least 4 other fossil bearing horizons exhibiting similar preservation have subsequently been found at the original site. The small quarry at the site is currently closed to public access, being on private land and administered by Yale Peabody Museum as part of ongoing research projects.
The original Beecher's Trilobite Bed is found within a thick succession of fine grained turbidite beds, the fossiliferous bed is about 40 mm thick lying on a scoured mudstone surface with remnants of burrows. Well preserved fossil remains are found 7–10 mm above the base parallel to the bedding plane, strongly aligned by the current, with as many facing up as down. Chemically, the bed contains high iron coupled with low organic carbon and low organic sulphur.
...
Wikipedia