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The distribution of methylated sulfur compounds, DMS and DMSP, in Canadian subarctic and Arctic marine waters during summer 2015
被引:23
|作者:
Jarnikova, Tereza
[1
]
Dacey, John
[2
]
Lizotte, Martine
[3
]
Levasseur, Maurice
[3
]
Tortell, Philippe
[1
,4
,5
]
机构:
[1] Univ British Columbia, Dept Earth Ocean & Atmospher Sci, 2022 Main Mall, Vancouver, BC V6T 1Z3, Canada
[2] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA
[3] Univ Laval, Dept Biol Quebec Ocean, Quebec City, PQ, Canada
[4] Univ British Columbia, Dept Bot, 6270 Univ Blvd, Vancouver, BC V6T 1Z4, Canada
[5] Univ British Columbia, Peter Wall Inst Adv Studies, 6330 Crescent Blvd, Vancouver, BC V6T 1Z4, Canada
基金:
加拿大自然科学与工程研究理事会;
关键词:
DIMETHYL-SULFIDE;
SEA-ICE;
DIMETHYLSULFONIOPROPIONATE DMSP;
OCEANIC PHYTOPLANKTON;
NORTHWEST ATLANTIC;
ATMOSPHERIC SULFUR;
DISSOLVED DMSP;
CHLOROPHYLL-A;
ROSS SEA;
BLOOM;
D O I:
10.5194/bg-15-2449-2018
中图分类号:
Q14 [生态学(生物生态学)];
学科分类号:
071012 ;
0713 ;
摘要:
We present seawater concentrations of dimethyl sulfide (DMS) and dimethylsulfoniopropionate (DMSP) measured across a transect from the Labrador Sea to the Canadian Arctic Archipelago during summer 2015. Using an automated ship-board gas chromatography system and a membrane-inlet mass spectrometer, we measured a wide range of DMS (similar to 1 to 18 nM) and DMSP (similar to 1 to 150 nM) concentrations. The highest DMS and DMSP concentrations occurred in a localized region of Baffin Bay, where surface waters were characterized by high chlorophyll a (chl a) fluorescence, indicative of elevated phytoplankton biomass. Across the full sampling transect, there were only weak relationships between DMS(P), chl a fluorescence and other measured variables, including positive relationships between DMSP V chl a ratios and several taxonomic marker pigments, and elevated DMS(P) concentrations in partially ice-covered areas. Our high spatial resolution measurements allowed us to examine DMS variability over small scales (< 1 km), documenting strong DMS concentration gradients across surface hydrographic frontal features. Our new observations fill in an important observational gap in the Arctic Ocean and provide additional information on sea-air DMS fluxes from this ocean region. In addition, this study constitutes a significant contribution to the existing Arctic DMS(P) dataset and provides a baseline for future measurements in the region.
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页码:2449 / 2465
页数:17
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