Lower Jurassic Ostracod Biozonation of the Mochras Borehole
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A Diapsid Faunule from the Lower Jurassic Of
provide a test for the hypothesis of faunal change at the Triassic-Jurassic boundary recently proposed by OLSEN and SUES (1986). They are remarkable for the numerical abundance and quality of preservation of the bones, the lithological diversity of fossil-bearing deposits, and the excellent degree of stratigraphic resolution. The vertebrate remains from the McCoy Brook Formation currently repre...
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ژورنال
عنوان ژورنال: Journal of Micropalaeontology
سال: 1991
ISSN: 2041-4978
DOI: 10.1144/jm.9.2.205