13C/12C composition of marine dissolved organic carbon

被引:39
|
作者
Fry, B [1 ]
Hopkinson, CS
Nolin, A
Wainright, SC
机构
[1] Louisiana State Univ, Coastal Ecol Inst, Baton Rouge, LA 70803 USA
[2] Marine Biol Lab, Ctr Ecosyst, Woods Hole, MA 02543 USA
[3] Rutgers State Univ, Cook Coll, Inst Marine & Coastal Sci, New Brunswick, NJ 08903 USA
基金
美国国家科学基金会;
关键词
dissolved organic carbon; delta C-13 values; sedimentary organic material;
D O I
10.1016/S0009-2541(98)00100-4
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The stable isotopic composition of marine dissolved organic carbon (DOC) was measured with a high temperature, sealed tube combustion technique. The delta(13)C values of DOC ((DOC)-C-13) were approximately -22 parts per thousand for all samples that were collected (1) in a monthly survey conducted in Woods Hole Harbor, (2) in a spatial survey across Georges Bank during a spring bloom period, and (3) in depth profiles near Bermuda, Georges Bank and in the eastern Equatorial Pacific. The (DOC)-C-13 values were uniform in waters of varying DOC content, including low DOC deep waters and high DOC surface waters, indicating little overall isotopic fractionation during formation and degradation of marine DOG. The -22 parts per thousand (DOC)-C-13 values are similar to those observed for average marine particulate and sedimentary organic material, and exclude a large contribution from -27 parts per thousand terrestrial DOC to ocean pools. (C) 1998 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:113 / 118
页数:6
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