1982
DOI: 10.3133/pp1066h
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Palaeocopid and podocopid Ostracoda from the Lexington Limestone and Clays Ferry Formation (Middle and Upper Ordovician) of central Kentucky

Abstract: The Middle through lower Upper Ordovician Lexington Limestone and lower part of the Clays Ferry Formation contain an abundant and diversified ostracode fauna. More than 10,000 specimens belonging to 39 genera and 53 species have been found in 73 collections made by members of the U.

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Cited by 21 publications
(43 citation statements)
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“…All the specimens of W. trinoda possess only three nodes, whereas W. nodosa includes quadrinodose valves as well. Warshauer & Berdan (1982) explained this variation in the number of nodes to be Parenthatia hanamiloslavensis sp. nov. Figure 8D, E, Table 8 Holotype.…”
Section: Scanipisthia Rectangularis (Troedsson 1918)mentioning
confidence: 99%
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“…All the specimens of W. trinoda possess only three nodes, whereas W. nodosa includes quadrinodose valves as well. Warshauer & Berdan (1982) explained this variation in the number of nodes to be Parenthatia hanamiloslavensis sp. nov. Figure 8D, E, Table 8 Holotype.…”
Section: Scanipisthia Rectangularis (Troedsson 1918)mentioning
confidence: 99%
“…Ostracod distribution from Laurentia (Maysvillian-base of Gamachian Stage) is documented from Iowa (Spivey 1939, Levinson 1951, Missouri (Keenan 1951), Minnesota (Burr & Swain 1965, Swain 1987, Kentucky (Warshauer & Berdan 1982), from the Canadian Whittaker Formation (Copeland 1977, Copeland 1989 and Vauréal and Ellis Bay formations of Anticosti Island, Quebec (Bolton 1970;Copeland 1970Copeland , 1973Barnes & McCracken 1981), which are recently considered as probably pre-Hirnantian (more in Meidla et al 2013 and references therein). Williams et al (2001) documented ostracod assemblages of Avalonia (Pusgillian-Rawtheyan Stage) from the Cautley Mudstone Formation of northern England.…”
Section: Palaeobiogeography and Biodiversitymentioning
confidence: 99%
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