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Homogeneous sulfur isotope signature in East Antarctica and implication for sulfur source shifts through the last glacial-interglacial cycle
Sulfate aerosol (SO(4)(2−)) preserved in Antarctic ice cores is discussed in the light of interactions between marine biological activity and climate since it is mainly sourced from biogenic emissions from the surface ocean and scatters solar radiation during traveling in the atmosphere. However, th...
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| Vydáno v: | Sci Rep |
|---|---|
| Hlavní autoři: | , , , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2019
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6711983/ https://ncbi.nlm.nih.gov/pubmed/31455786 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-019-48801-1 |
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