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Is pore water oxygen content decoupled from productivity on the California Margin? Trace element results from Ocean Drilling Program Hole 1017E, San Lucia slope, California

dc.contributor.authorHendy, I. L.en_US
dc.contributor.authorPedersen, T. F.en_US
dc.date.accessioned2013-01-03T19:41:58Z
dc.date.available2013-01-03T19:41:58Z
dc.date.issued2005-12en_US
dc.identifier.citationHendy, I. L.; Pedersen, T. F. (2005). "Is pore water oxygen content decoupled from productivity on the California Margin? Trace element results from Ocean Drilling Program Hole 1017E, San Lucia slope, California." Paleoceanography 20(4): n/a-n/a. <http://hdl.handle.net/2027.42/95250>en_US
dc.identifier.issn0883-8305en_US
dc.identifier.issn1944-9186en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/95250
dc.publisherWiley Periodicals, Inc.en_US
dc.subject.otherRedox Chemistryen_US
dc.subject.otherProductivityen_US
dc.subject.otherIntermediate Wateren_US
dc.titleIs pore water oxygen content decoupled from productivity on the California Margin? Trace element results from Ocean Drilling Program Hole 1017E, San Lucia slope, Californiaen_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelAtmospheric and Oceanic Sciencesen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/95250/1/palo1223.pdf
dc.identifier.doi10.1029/2004PA001123en_US
dc.identifier.sourcePaleoceanographyen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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