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Emission of dimethylsulfide from Weddell Sea leads
Author(s) -
Zemmelink H. J.,
Houghton L.,
Dacey J. W. H.,
Worby A. P.,
Liss P. S.
Publication year - 2005
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2005gl024242
Subject(s) - dimethylsulfoniopropionate , water column , seawater , dimethyl sulfide , oceanography , stratification (seeds) , sea ice , surface water , environmental science , salinity , sulfur , environmental chemistry , geology , atmospheric sciences , chemistry , phytoplankton , seed dormancy , germination , botany , organic chemistry , dormancy , environmental engineering , nutrient , biology
The distribution of dimethylsulfide (DMS), dimethylsulfoniopropionate (DMSP) and dimethylsulfoxide (DMSO) was examined in lead water in pack ice of the Weddell Sea. Samples were taken by pulling water into a syringe from a series of depths from 0.002 m to 4 m and deeper. Concentrations of DMS, DMSP and DMSO remained low throughout the water column relative to surface water, which was highly enriched. Concentrations of the major sulfur compounds increased by over an order of magnitude during periods with smooth surface water conditions. This increase coincided with a profound stratification of the water column, caused by a decrease in salinity of near surface water. We estimate that the DMS emission from leads and open water in Antarctic sea ice could contribute significantly to the yearly DMS flux from the Southern Ocean.

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