Geology And Paleontology Of The Lower Miocene Pollack Farm Fossil Site Delaware

Author(s)Benson, R.N.
Date Accessioned2008-11-06T20:43:02Z
Date Available2008-11-06T20:43:02Z
Publication Date1998
AbstractThe Pollack Farm Site near Cheswold, Delaware, is named for a borrow pit excavated during highway construction. The excavation exposed a portion of the Cheswold sands of the lower Miocene Calvert Formation. Two sand intervals (Cheswold C-3 and C-4) yielded a diverse assemblage of land and marine vertebrate remains and more than 100 species of mollusks. An isolated occurrence of a sandy silt (the radiolarian bed) stratigraphically between the two macrofossil-bearing units yielded only siliceous microfossils—radiolarians, diatoms, and sponge spicules.en
URLhttp://udspace.udel.edu/handle/19716/3590
dc.languageen_USen_US
PublisherNewark, DE: Delaware Geological Survey, University of Delawareen
Part of SeriesSpecial Publication;21
KeywordsPollack Farmen
KeywordsCheswold, Delawareen
Keywordslower Miocene Calvert Formationen
Keywordsmollusksen
Keywordsdiatomsen
Keywordssponge spiculesen
Keywordssiliceous microfossils—radiolariansen
TitleGeology And Paleontology Of The Lower Miocene Pollack Farm Fossil Site Delawareen
TypeBooken
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