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dc.contributor.authorBoudreau, BPen_US
dc.date.accessioned2013-06-19T17:53:24Z
dc.date.available2013-06-19T17:53:24Z
dc.date.issued2004-03en_US
dc.identifier.citationBoudreau, BP. 2004. "What controls the mixed-layer depth in deep-sea sediments? The importance of particulate organic carbon flux." Limnology and Oceanography 49(2): 620-622.en_US
dc.identifier.issn0024-3590en_US
dc.identifier.urihttp://hdl.handle.net/10222/26332
dc.identifier.urihttp://dx.doi.org/10.4319/lo.2004.49.2.0620
dc.description.abstractNo abstract available.en_US
dc.relation.ispartofLimnology and Oceanographyen_US
dc.titleWhat controls the mixed-layer depth in deep-sea sediments? The importance of particulate organic carbon fluxen_US
dc.typearticleen_US
dc.identifier.volume49en_US
dc.identifier.issue2en_US
dc.identifier.startpage620en_US
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