Beecher's Trilobite Bed is a thin layer within the Late Ordovician Frankfort Shale near Rome, New York, roughly four hundred and fifty million years old, in which trilobites and other arthropods were preserved through pyritization, replacement of their soft tissue and appendages by pyrite, in far greater anatomical detail, including legs, gills and antennae, than trilobite fossils typically allow. First excavated by Yale paleontologist Charles Emerson Beecher in the 1890s, the bed remains one of the primary sources for understanding trilobite limb anatomy.
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Source Beecher's Trilobite Bed (Wikipedia)
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Beecher's Trilobite Bed (Wikipedia)
Caused By: Sedimentation, Sedimentology
The presence of turbidite beds in the surrounding sediments also adds evidence to this theory, as they are often deposited in deep water areas.
Associated With: Ordovician, Lead paragraph
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.
Associated With: Shale, Lead paragraph
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.
Associated With: Ordovician, Lead, age Ordovician
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.
Associated With: Shale, Lead, rock Shale
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.
In Discipline: Stratigraphy, Lead paragraph
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 anato
In Group: Paleozoic Fossil Sites, Lead sentence
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
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