East Witton Lodge. (Carboniferous of the United Kingdom)

Where: England, United Kingdom (52.8° N, 1.4° W: paleocoordinates 2.2° S, 6.7° E)

• small collection-level geographic resolution

When: E2 zone, Cockhill Marine Band Formation, Arnsbergian (327.0 - 323.7 Ma)

• "the complete fossiliferous horizon is more suitably termed the 'Cockhill Marine Band'...the term 'Cockhill Limestone' is retained but restricted to the band of fossiliferous limestone or limestone nodules where present."

• member-level stratigraphic resolution

Environment/lithology: marine; lithified, concretionary, shelly/skeletal, calcareous, carbonaceous mudstone and wackestone

• Paleoenvironment could possibly be paralic or deltaic. There are a lot of preserved wood fragments and other plant remains. It was definitely near-shore, also definitely marine (according to the authors).
• fossiliferous black shale...carbonaceous shale...medium grained sandstone...orange mud...gingerbread crinoidal sandstone...nodular limestone in black calcareous mudstone

Primary reference: A. A. Wilson and A. T. Thompson. 1959. Marine bands of Arnsbergian age (Namurian) in the south-eastern portion of the Askrigg Block, Yorkshire. Proceedings of the Yorkshire Geological Society 32(3):45-68 [J. Alroy/M. Sommers/M. Uhen]more details

Purpose of describing collection: biostratigraphic analysis

PaleoDB collection 8433: authorized by John Alroy, entered by Mike Sommers on 12.07.2000

Creative Commons license: CC BY (attribution)

Taxonomic list

unclassified
  -
Crinoidea
  -
Crinoidea indet. Miller 1821 Sea lily
ossicles
Ostracoda
 Platycopida - Cavellinidae
Cavellina sp. Coryell 1928 ostracod
 Podocopida - Bairdiidae
Bairdia sp. M'Coy 1844 ostracod