georefid:1996-050525SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1029/95PA02087<gco:CharacterString>Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene</gco:CharacterString>1995-01-01publicationgeorefid:1996-050525doi:10.1029/95PA02087Dickens, Gerald R.University of Michigan, Department of Geological Sciences, Ann Arbor, MI, United StatesauthorO'Neil, James R.authorRea, David K.authorOwen, Robert M.authorAmerican Geophysical Union, Washington, DC, United StatespublisherdocumentDigitalPaleoceanography10 (6)965-971completedStratigraphyaliphatic hydrocarbonsalkanesbenthic taxabottom waterC-13/C-12carbonCenozoicdissociationForaminiferageochemical cycleglobalhydrateshydrocarbonsinorganic carbonInvertebrataisotopesmethanemicrofossilsmodelsO-18/O-16organic compoundsoxygenpaleo-oceanographyPaleocenepaleoclimatologyPaleogeneplanktonic taxaProtistastable isotopestemperatureTertiaryupper PaleoceneEnglishgeoscientificInformationapplication/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://www.agu.org/journals/pa/v010/i006/95PA02087/95PA02087.pdfdownload