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Increased thermohaline stratification as a possible cause for an ocean anoxic event in the Cretaceous period

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dc.contributor.author Erbacher, J. en
dc.contributor.author Huber, Brian T. en
dc.contributor.author Norris, R. D. en
dc.contributor.author Markey, M. en
dc.date.accessioned 2009-05-13T13:19:38Z
dc.date.available 2009-05-13T13:19:38Z
dc.date.issued 2001
dc.identifier.citation Erbacher, J., Huber, Brian T., Norris, R. D., and Markey, M. 2001. "<a href="https%3A%2F%2Frepository.si.edu%2Fhandle%2F10088%2F7417">Increased thermohaline stratification as a possible cause for an ocean anoxic event in the Cretaceous period</a>." <em>Nature</em>. 409 (6818):325&ndash;327. en
dc.identifier.issn 0028-0836
dc.identifier.uri http://hdl.handle.net/10088/7417
dc.format.extent 191932 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.relation.ispartof Nature en
dc.title Increased thermohaline stratification as a possible cause for an ocean anoxic event in the Cretaceous period en
dc.type Journal Article en
dc.identifier.srbnumber 76472
rft.jtitle Nature
rft.volume 409
rft.issue 6818
rft.spage 325
rft.epage 327
dc.description.SIUnit NMNH en
dc.description.SIUnit NH-Paleobiology en
dc.citation.spage 325
dc.citation.epage 327


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