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Smith, David C. (2006): Dissolved organic carbon in interstitial waters, Equatorial Pacific and Peru Margin
Leg/Site/Hole:
Related Expeditions:
ODP 201
Identifier:
ID:
2007-008197
Type:
georefid
ID:
10.2973/odp.proc.sr.201.111.2005
Type:
doi
Creator:
Name:
Smith, David C.
Affiliation:
University of Rhode Island, Graduate School of Oceanography, Narragansett, RI, United States
Role:
author
Identification:
Title:
Dissolved organic carbon in interstitial waters, Equatorial Pacific and Peru Margin
Year:
2006
Source:
In: Jorgensen, Bo B. (editor), D'Hondt, Steven L. (editor), Miller, D. Jay (editor), Aiello, Ivano W., Bekins, Barbara, Blake, Ruth E., Cragg, Barry A., Cypionka, Heribert, Dickens, Gerald R., Ferdelman, Timothy G., Ford, Kathryn H., Gettemy, Glen L., Guerin, Gilles, Hinrichs, Kai-Uwe, Holm, Nils G., House, Christopher H., Inagaki, Fumio, Meister, Patrick, Mitterer, Richard M., Naehr, Thomas H., Niitsuma, Sachiko, Parkes, R. John, Schippers, Axel, Skilbeck, C. Gregory, Smith, David C., Spivack, Arthur J., Teske, Andreas P., Wiegel, Juergen, Proceedings of the Ocean Drilling Program; scientific results; controls on microbial communities in deeply buried sediments, eastern Equatorial Pacific and Peru Margin; covering Leg 201 of the cruises of the drilling vessel JOIDES Resolution; San Diego, California, to Valparaiso, Chile; Sites 1225-1231; 27 January-29 March 2002
Publisher:
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
Volume:
201
Issue:
Pages:
Abstract:
This report contains dissolved organic carbon (DOC) concentration data from interstitial waters collected at three open-ocean sites (1225, 1226, and 1231) and four sites cored along the Peru margin (1227, 1228, 1229, and 1230) during Ocean Drilling Program Leg 201. The sites were selected to represent a wide range of habitats for subsurface life based on organic carbon input to the sediments. Subsurface maxima of DOC at the ocean-margin sites is consistent with in situ production of DOC through active hydrolysis of particulate organic carbon. These downhole profiles agree well with the dissolved inorganic carbon (DIC) concentrations indicating complete remineralization of some fraction DOC to DIC. The open-ocean sites exhibit relatively flat downhole profiles, indicating that diagenesis is occurring at a much lower rate at these sites.
Language:
English
Genre:
Serial
Rights:
URL:
http://www-odp.tamu.edu/publications/201_SR/VOLUME/CHAPTERS/111.PDF
Coverage:
Geographic coordinates:
North:3.5000
West:-110.3500
East: -77.5500
South:-12.0500
Keywords:
Hydrochemistry; Oceanography; carbon; concentration; continental margin; cores; diagenesis; dissolved materials; East Pacific; Equatorial Pacific; geochemistry; hydrochemistry; Leg 201; measurement; Ocean Drilling Program; organic carbon; Pacific Ocean; Peru; pore water; sea water; South America;
.
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