Biotic response to a Middle Ordovician palaeoceanographic event in eastern North America

M. E. Patzkowsky; S. M. Holland

doi:10.1130/0091-7613(1993)021<0619:BRTAMO>2.3.CO

Biotic response to a Middle Ordovician palaeoceanographic event in eastern North America

M. E. Patzkowsky
, S. M. Holland

Geosciences

Research output: Contribution to journal › Article › peer-review

94 Scopus citations

Abstract

A sequence stratigraphic framework is used to document a major extinction and migration episode that occurred in the Middle and Late Ordovician of North America. This event is characterized in eastern North America by coordinated changes in faunal assemblages, carbonate lithologies, siliciclastic influx, and phosphatization. These changes are ascribed to a regional paleoceanographic event brought on by thrust-driven flexural subsidence and sea-level fluctuations that lowered water temperature and increased turbidity and nutrient input. -from Authors

Original language	English (US)
Pages (from-to)	619-622
Number of pages	4
Journal	Geology
Volume	21
Issue number	7
DOIs	https://doi.org/10.1130/0091-7613(1993)021<0619:BRTAMO>2.3.CO
State	Published - Jan 1 1993

All Science Journal Classification (ASJC) codes

Geology

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10.1130/0091-7613(1993)021<0619:BRTAMO>2.3.CO

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abstract = "A sequence stratigraphic framework is used to document a major extinction and migration episode that occurred in the Middle and Late Ordovician of North America. This event is characterized in eastern North America by coordinated changes in faunal assemblages, carbonate lithologies, siliciclastic influx, and phosphatization. These changes are ascribed to a regional paleoceanographic event brought on by thrust-driven flexural subsidence and sea-level fluctuations that lowered water temperature and increased turbidity and nutrient input. -from Authors",

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AB - A sequence stratigraphic framework is used to document a major extinction and migration episode that occurred in the Middle and Late Ordovician of North America. This event is characterized in eastern North America by coordinated changes in faunal assemblages, carbonate lithologies, siliciclastic influx, and phosphatization. These changes are ascribed to a regional paleoceanographic event brought on by thrust-driven flexural subsidence and sea-level fluctuations that lowered water temperature and increased turbidity and nutrient input. -from Authors

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Biotic response to a Middle Ordovician palaeoceanographic event in eastern North America

Abstract

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