Industrial-era decline in Arctic methanesulfonic acid is offset by increased biogenic sulfate aerosol
Industrial-era decline in Arctic methanesulfonic acid is offset by increased biogenic sulfate aerosol
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DOI:
10.1073/pnas.2307587120
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发表时间:
2023-11
影响因子:
11.1
通讯作者:
U. Jongebloed;Andrew J Schauer;J. Cole‐Dai;C. Larrick;William C. Porter;L. Tashmim;S. Zhai;Sara Salimi;Shana R Edouard;L. Geng;B. Alexander
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文献类型:
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作者:
U. Jongebloed;Andrew J Schauer;J. Cole‐Dai;C. Larrick;William C. Porter;L. Tashmim;S. Zhai;Sara Salimi;Shana R Edouard;L. Geng;B. Alexander
Significance Decreasing methanesulfonic acid (MSA) concentrations across Greenland ice cores have suggested declining North Atlantic phytoplankton abundance, with implications for ocean ecosystems and climate. MSA is used to infer phytoplankton abundance because phytoplankton emits dimethyl sulfide (DMS), which is oxidized to MSA and sulfate. However, atmospheric chemistry controls how much DMS is converted to MSA vs. sulfate. Here, we measure DMS-derived sulfate compared to MSA in a Greenland ice core over the industrial era. We show that total biogenic sulfur, the sum of MSA and DMS-derived sulfate, is relatively steady over the industrial era, but MSA declines because anthropogenic pollution affects the ratio of MSA vs. DMS-derived sulfate. Therefore, interpreting MSA as a proxy for DMS emissions must consider atmospheric chemistry.