Bridgeton - Kirkwood Formation: Early/Lower Miocene, New Jersey

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Gastropoda - Neotaenioglossa - Calyptraeidae
Calyptraea aperta (Solander 1766)
recombined as Calyptraea (Trochita) aperta
Crepidula fornicata (Linnaeus 1758)
Crucibulum costatum (Say 1820)
recombined as Crucibulum (Dispotaea) costata
Bivalvia - Nuculida - Nuculidae
Nucula proxima Say 1820
recombined as Nucula (Nucula) proxima
Bivalvia - Carditida - Crassatellidae
Eucrassatella melina (Conrad 1832)
recombined as Marvacrassatella melina
Bivalvia - Carditida - Carditidae
Cardita arata (Conrad 1832)
recombined as Carditamera arata
Bivalvia - Carditida - Astartidae
Astarte distans Conrad 1862
Bivalvia - Cardiida - Ungulinidae
Diplodonta shilohensis Dall 1900
Bivalvia - Cardiida - Cardiidae
Cardium patuxentium Glenn 1904
synonym of Chesacardium craticuloides
Bivalvia - Mytilida - Mytilidae
Modiola inflata Tuomey and Holmes 1856
synonym of Modiolus ducatellii
Bivalvia - Arcida - Glycymerididae
Glycymeris parilis (Conrad 1843)
Bivalvia - Arcida - Arcidae
Arca centenaria Say 1824
recombined as Striarca centenaria
Bivalvia - Ostreida - Malleidae
Melina maxillata (Lamarck 1819)
recombined as Isognomon maxillata
Lingulata - Discinida - Disciniidae
Discinisca lugubris (Conrad 1834)
see common names

Geography
Country:United States State/province:New Jersey County:Cumberland
Coordinates: 39.4° North, 75.2° West (view map)
Paleocoordinates:39.6° North, 70.8° West
Basis of coordinate:based on nearby landmark
Geographic resolution:local area
Time
Period:Neogene Epoch:Miocene
10 m.y. bin:Cenozoic 5
Key time interval:Early/Lower Miocene
Age range of interval:23.03000 - 15.98000 m.y. ago
Stratigraphy
Formation:Kirkwood
Local section:Bridgeton
Regional section:Cumberland
Stratigraphic resolution:member
Stratigraphy comments: No lithostratigraphic details or stratigraphic relationships provided in text. Equivalent in age and slightly older than the Calvert Formaiton of Maryland and Virginia. Overlain by the Cohansey Sand with a time transgressive contact, Kirkwood Formation is Burdigalian-Langhian in age.
Lithology and environment
Primary lithology: unlithified argillaceous,silty mudstone
Secondary lithology:pebbly sandstone
Includes fossils?Y
Includes fossils?Y
Lithology description: No lithologic data reported in text. Clayey to silty mudrock, massive sand, and thin pebble lenses.
Environment:coastal indet.
Geology comments: No geologic or paleoenvironmental data reported in text. Deposited in a sublittoral to nearshore environments
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Collection methods and comments
Collection methods:field collection,survey of museum collection
Reason for describing collection:taxonomic analysis
Museum repositories:USNM
Collection method comments: Collections reposited in USNM and USGS collections. From Richards and Harbison (1942: "Whitfield frequently speaks of a "stony layer" near Bridgeton and many of the fossulks in the various museums labelled "Bridgeton" are in the sandstone phase of the Kirkwood. The exact locality of the fossils was not given and no exposures can be found in the vicinityyu of Bridgeton today."
Taxonomic list comments:Exhaustive for Gastropoda, Bivalvia and Scaphopoda. Nomenclature is somewhat antiquated but provided to species resolution and authoritative.
Metadata
Database number:59337
Authorizer:A. Hendy Enterer:A. Hendy
Modifier:A. Hendy Research group:marine invertebrate
Created:2006-03-26 12:02:23 Last modified:2013-11-25 13:37:23
Access level:the public Released:2006-03-26 12:02:23
Creative Commons license:CC BY
Reference information

Primary reference:

17100. H. G. Richards and A. Harbison. 1942. Miocene invertebrate fauna of New Jersey. Proceedings of the Academy of Natural Sciences of Philadelphia 94:167-250 [A. Miller/A. Hendy]

Secondary references:

16984 J. A. Gardner. 1943. Mollusca from the Miocene and Lower Pliocene of Virginia and North Carolina. Part 1. Pelecypoda. United States Geological Survey Professional Paper 199(A):1-178 [A. Miller/A. Hendy/S. Ávila]