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

dc.contributor.authorErbacher, J.
dc.contributor.authorHuber, Brian T.
dc.contributor.authorNorris, R. D.
dc.contributor.authorMarkey, M.
dc.date.accessioned2009-05-13T13:19:38Z
dc.date.available2009-05-13T13:19:38Z
dc.date.issued2001
dc.format.extent191932 bytes
dc.format.extent325–327
dc.format.mimetypeapplication/pdf
dc.identifier0028-0836
dc.identifier.citationErbacher, J., Huber, Brian T., Norris, R. D., and Markey, M. 2001. "<a href="https://repository.si.edu/handle/10088/7417">Increased thermohaline stratification as a possible cause for an ocean anoxic event in the Cretaceous period</a>." <em>Nature</em>, 409, (6818) 325–327.
dc.identifier.issn0028-0836
dc.identifier.urihttp://hdl.handle.net/10088/7417
dc.language.isoen_US
dc.publisherMACMILLAN PUBLISHERS LTD
dc.relation.ispartofNature 409 (6818)
dc.titleIncreased thermohaline stratification as a possible cause for an ocean anoxic event in the Cretaceous period
dc.typearticle
sro.description.unitNMNH
sro.description.unitNH-Paleobiology
sro.identifier.itemID76472
sro.identifier.refworksID10959
sro.identifier.urlhttps://repository.si.edu/handle/10088/7417
sro.publicationPlaceLONDON; PORTERS SOUTH, 4 CRINAN ST, LONDON N1 9XW, ENGLAND

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