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Cobban, W. A., Kennedy, W. J. (1990) Upper Cenomanian ammonites from the Woodbridge Clay Member of the Raritan Formation in New Jersey. Journal of Paleontology, 64 (5) 845-846 doi:10.1017/s0022336000019053

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Reference TypeJournal (article/letter/editorial)
TitleUpper Cenomanian ammonites from the Woodbridge Clay Member of the Raritan Formation in New Jersey
JournalJournal of Paleontology
AuthorsCobban, W. A.Author
Kennedy, W. J.Author
Year1990 (September)Volume64
Issue5
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0022336000019053Search in ResearchGate
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Mindat Ref. ID415060Long-form Identifiermindat:1:5:415060:6
GUID0
Full ReferenceCobban, W. A., Kennedy, W. J. (1990) Upper Cenomanian ammonites from the Woodbridge Clay Member of the Raritan Formation in New Jersey. Journal of Paleontology, 64 (5) 845-846 doi:10.1017/s0022336000019053
Plain TextCobban, W. A., Kennedy, W. J. (1990) Upper Cenomanian ammonites from the Woodbridge Clay Member of the Raritan Formation in New Jersey. Journal of Paleontology, 64 (5) 845-846 doi:10.1017/s0022336000019053
In(1990, September) Journal of Paleontology Vol. 64 (5) Cambridge University Press (CUP)
Abstract/NotesThe woodbridge Clay Member of the Raritan Formation of New Jersey yields the oldest marine fauna known from the Upper Cretaceous of the United States Atlantic seaboard. This fauna is dominated by bivalves and gastropods (Richards, 1943; Stephenson, 1954), which have sufficient elements in common with the Cenomanian Woodbine Formation of Texas to suggest a Cenomanian age (Stephenson, 1954, p. 26), and this has been supported by data from megascopic plant remains and pollen (see review in Christopher, 1977; Doyle and Robbins, 1977, and references therein). The discovery, by N. F. Sohl, of two ammonite fragments in the Woodbridge Clay Member provides the first evidence for the assignment of the member within the Cenomanian Stage. The specimens came from sideritic concretions in the Woodbridge Member at the claypit of the Sayreville-Fisher Brick Company at Sayreville, Middlesex County, New Jersey (USGS Mesozoic locality 29584). General descriptions of the Raritan succession are given in Owens and Sohl (1969), Owens et al. (1977), and Owens (1983).


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