Dissolved Organic Radiocarbon in the Eastern Pacific and Southern Oceans

被引:22
作者
Druffel, Ellen R. M. [1 ]
Griffin, Sheila [1 ]
Lewis, Christian B. [1 ]
Rudresh, Megha [1 ,2 ]
Garcia, Noreen G. [1 ,3 ]
Key, Robert M. [4 ]
McNichol, Ann P. [5 ]
Hauksson, Niels E. [1 ]
Walker, Brett D. [1 ,6 ]
机构
[1] Univ Calif Irvine, Dept Eartn Syst Sci, Irvine, CA 92697 USA
[2] Univ Georgia, Dept Geog, Athens, GA 30602 USA
[3] Scripps Inst Oceanog, La Jolla, CA USA
[4] Princeton Univ, Atmospher & Ocean Sci Program, Princeton, NJ 08544 USA
[5] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA
[6] Univ Ottawa, Dept Earth & Environm Sci, Ottawa, ON, Canada
关键词
C-13; carbon cycle; circumpolar deep water; dissolved inorganic carbon; dissolved organic carbon; radiocarbon; HIGH-MOLECULAR-WEIGHT; CARBON; EXTRACTION; PHASE; STORAGE; SAMPLES; MATTER;
D O I
10.1029/2021GL092904
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We report marine dissolved organic carbon (DOC) concentrations, and DOC Delta C-14 and delta C-13 values in seawater collected from the Southern Ocean and eastern Pacific GOSHIP cruise P18 in 2016/2017. The aging of C-14 in DOC in circumpolar deep water northward from 69 degrees S to 20 degrees N was similar to that measured in dissolved inorganic carbon in the same samples, indicating that the transport of deep waters northward is the primary control of C-14 in DIC and DOC. Low DOC increment C-14 and delta C-13 measurements between 1,200 and 3,400 m depth may be evidence of a source of DOC produced in nearby hydrothermal ridge systems (East Pacific Rise).
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页数:9
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