What controls the mixed-layer depth in deep-sea sediments? The importance of particulate organic carbon flux
| dc.contributor.author | Boudreau, Bernard P. | en_US |
| dc.date.accessioned | 2013-06-19T17:53:24Z | |
| dc.date.available | 2013-06-19T17:53:24Z | |
| dc.date.issued | 2004-03 | en_US |
| dc.identifier.citation | Boudreau, Bernard P. 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.issn | 0024-3590 | en_US |
| dc.identifier.uri | http://hdl.handle.net/10222/26332 | |
| dc.identifier.uri | http://dx.doi.org/10.4319/lo.2004.49.2.0620 | |
| dc.description.abstract | No abstract available. | en_US |
| dc.relation.ispartof | Limnology and Oceanography | en_US |
| dc.title | What controls the mixed-layer depth in deep-sea sediments? The importance of particulate organic carbon flux | en_US |
| dc.type | article | en_US |
| dc.identifier.volume | 49 | en_US |
| dc.identifier.issue | 2 | en_US |
| dc.identifier.startpage | 620 | en_US |
