Benthic oxygen fluxes and denitrification rates from high-resolution porewater profiles from the Western Antarctic Peninsula continental shelf

被引:19
|
作者
Hartnett, Hilairy [1 ,2 ]
Boehme, Susan [3 ]
Thomas, Carrie [4 ]
DeMaster, David [4 ]
Smith, Craig [5 ]
机构
[1] Arizona State Univ, Sch Earth & Space Explorat, Tempe, AZ 85287 USA
[2] Arizona State Univ, Dept Chem & Biochem, Tempe, AZ 85287 USA
[3] US EPA, Great Lakes Natl Program Off, Chicago, IL 60604 USA
[4] N Carolina State Univ, Dept Marine Earth & Atmospher Sci, Raleigh, NC 27695 USA
[5] Univ Hawaii, Dept Oceanog, Honolulu, HI 96822 USA
关键词
Benthic flux; Denitrification; Oxygen consumption; Carbon oxidation; Biogeochemistry; Respiration;
D O I
10.1016/j.dsr2.2008.06.002
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Benthic fluxes of dissolved oxygen and nitrate were calculated from high-resolution porewater profiles collected on the continental margin of the Western Antarctic Peninsula. Profiles were collected in four seasons between March 2000 and February 2001 as part of the FOODBANCS program. Oxygen consumption rates ranged from 0.92 to 3.11 mmol O-2 m(-2) d(-1) over the course of the year with an average annual oxygen consumption rate of 1.74 mmol O-2 m(-2) d(-1). The oxygen fluxes follow a trend similar to the particulate carbon export flux with smaller fluxes during the winter and larger fluxes during the spring bloom period. However, the range in oxygen fluxes is substantially smaller than the range in the particulate carbon export. Denitrification rates ranged from 0.66 to 1.46 mmol N m(-2) d(-1), and the average annual denitrification rate was 1.29 mmol N m(-2) d(-1). The 02 consumption and denitrification rates are of similar magnitude to rates measured on other deep (similar to 500 m) continental margins. Denitrification rates are strongly coupled to nitrification rates, with coupled nitrification-denitrification accounting for more than 80% of the total denitrification rate in these sediments. The Antarctic continental-margin sediment denitrification rates correspond to similar to 3-5 Tg N yr(-1), and thus these continental-margin sediments account for roughly 1-2% of the global sediment denitrification signal. (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2415 / 2424
页数:10
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