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Smithsonian Contributions to Paleobiology
A molluscan fauna consisting of 194 species is described from the Chowan River (upper Pliocene) a... more A molluscan fauna consisting of 194 species is described from the Chowan River (upper Pliocene) and James City (lower Pleistocene) formations at the Lee Creek Mine, Aurora, North Carolina. These two formations are as much as 7 m thick in the mine and unconformably overlie strata that correlate with the Yorktown Formation in its type area. The Chowan River and James City formations are separated by an unconformity. The mollusks of the Chowan River Formation are assigned to the Glycymeris hummi-Turritella perexilis assemblage-zone and the mollusks in the overlying James City Formation are assigned to the Marvacrassatella kauffmani-Astarte berryi assemblage-zone. Although mollusks in these zones lived in a subtropical thermal regime, they include some warm-temperate species not found in contemporaneous deposits farther south. The units represented by these assemblage zones were deposited mostly under open marine conditions at a maximum depth of about 25 m. The Marvacrassatella kauffman...
Analyses of 87Sr/86Sr ratios in the shells of marine bivalve mollusks from the Pollack Farm Site ... more Analyses of 87Sr/86Sr ratios in the shells of marine bivalve mollusks from the Pollack Farm Site in Kent County, Delaware, indicate that the fossils represent an early Miocene assemblage which lived about 17.9 ± 0.5 Ma. Faunal similarities, as well as Sr-isotopic data, support a correlation between the fossils at the Pollack Site and portions of the Kirkwood Formation to the north (New Jersey) and to the south the Fairhaven Member of the Calvert Formation (Maryland), the Pungo River Formation (North Carolina), and the Chipola Formation (Florida). A strong marine-nonmarine link with terrestrial vertebrates of the Hemingfordian North American Land Mammal Age is also suggested. 1 In Benson. R.N., ed., 1998, Geology and paleontology of the lower Miocene Pollack Farm Fossil Site, Delaware: Delaware Geological Survey Special Publication No. 21, p. 21–25. 2 Florida Museum of Natural History, University of Florida, Gainesville, FL 32611 3 Virginia Museum of Natural History, 1001 Douglas Ave...
Tulane Studies in Geology and Paleontology, 2017
Mollusks and foraminifers from the type section of the Raysor Formation in the Coastal Plain of S... more Mollusks and foraminifers from the type section of the Raysor Formation in the Coastal Plain of South Carolina were obtained from collections in the National Museum of Natural History. Smithsonian Institution, Washington, D.C., and the Charleston Museum, Charleston, South Carolina. Analysis of the molluscan taxa shows the unit to be correlative With the Rushmere and Morgarts Beach Members of the Yorktown Formation in Virginia and North Carolina. Planktic foraminifers in the Raysor indicate an equivalency with Blow's (1969) Zone N20 [= Berggren, et al. (1983) Zone PL3]: this equivalency would suggest that the unit is lower upper Pliocene. The Raysor was deposited on a shallow shelf in a setting that was temperate at first, but which quickly warmed to subtropical.
Upper Cretaceous and Cenozoic Geology of the Southeastern Atlantic Coastal Plain: Atlanta, Georgia to Chesapeake, Virginia July 1–9, 1989, 1989
Upper Cretaceous and Cenozoic Geology of the Southeastern Atlantic Coastal Plain: Atlanta, Georgia to Chesapeake, Virginia July 1–9, 1989, 1989
The Paleontological Society Special Publications
Smithsonian Contributions to Paleobiology
A molluscan fauna consisting of 194 species is described from the Chowan River (upper Pliocene) a... more A molluscan fauna consisting of 194 species is described from the Chowan River (upper Pliocene) and James City (lower Pleistocene) formations at the Lee Creek Mine, Aurora, North Carolina. These two formations are as much as 7 m thick in the mine and unconformably overlie strata that correlate with the Yorktown Formation in its type area. The Chowan River and James City formations are separated by an unconformity. The mollusks of the Chowan River Formation are assigned to the Glycymeris hummi-Turritella perexilis assemblage-zone and the mollusks in the overlying James City Formation are assigned to the Marvacrassatella kauffmani-Astarte berryi assemblage-zone. Although mollusks in these zones lived in a subtropical thermal regime, they include some warm-temperate species not found in contemporaneous deposits farther south. The units represented by these assemblage zones were deposited mostly under open marine conditions at a maximum depth of about 25 m. The Marvacrassatella kauffman...
Analyses of 87Sr/86Sr ratios in the shells of marine bivalve mollusks from the Pollack Farm Site ... more Analyses of 87Sr/86Sr ratios in the shells of marine bivalve mollusks from the Pollack Farm Site in Kent County, Delaware, indicate that the fossils represent an early Miocene assemblage which lived about 17.9 ± 0.5 Ma. Faunal similarities, as well as Sr-isotopic data, support a correlation between the fossils at the Pollack Site and portions of the Kirkwood Formation to the north (New Jersey) and to the south the Fairhaven Member of the Calvert Formation (Maryland), the Pungo River Formation (North Carolina), and the Chipola Formation (Florida). A strong marine-nonmarine link with terrestrial vertebrates of the Hemingfordian North American Land Mammal Age is also suggested. 1 In Benson. R.N., ed., 1998, Geology and paleontology of the lower Miocene Pollack Farm Fossil Site, Delaware: Delaware Geological Survey Special Publication No. 21, p. 21–25. 2 Florida Museum of Natural History, University of Florida, Gainesville, FL 32611 3 Virginia Museum of Natural History, 1001 Douglas Ave...
Tulane Studies in Geology and Paleontology, 2017
Mollusks and foraminifers from the type section of the Raysor Formation in the Coastal Plain of S... more Mollusks and foraminifers from the type section of the Raysor Formation in the Coastal Plain of South Carolina were obtained from collections in the National Museum of Natural History. Smithsonian Institution, Washington, D.C., and the Charleston Museum, Charleston, South Carolina. Analysis of the molluscan taxa shows the unit to be correlative With the Rushmere and Morgarts Beach Members of the Yorktown Formation in Virginia and North Carolina. Planktic foraminifers in the Raysor indicate an equivalency with Blow's (1969) Zone N20 [= Berggren, et al. (1983) Zone PL3]: this equivalency would suggest that the unit is lower upper Pliocene. The Raysor was deposited on a shallow shelf in a setting that was temperate at first, but which quickly warmed to subtropical.
Upper Cretaceous and Cenozoic Geology of the Southeastern Atlantic Coastal Plain: Atlanta, Georgia to Chesapeake, Virginia July 1–9, 1989, 1989
Upper Cretaceous and Cenozoic Geology of the Southeastern Atlantic Coastal Plain: Atlanta, Georgia to Chesapeake, Virginia July 1–9, 1989, 1989
The Paleontological Society Special Publications