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The paleoclimatic footprint in the soil carbon stock of the Tibetan permafrost region
Tibetan permafrost largely formed during the late Pleistocene glacial period and shrank in the Holocene Thermal Maximum period. Quantifying the impacts of paleoclimatic extremes on soil carbon stock can shed light on the vulnerability of permafrost carbon in the future. Here, we synthesize data from...
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| 出版年: | Nat Commun |
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| 主要な著者: | , , , , , , , , , , , , , , , , , , , , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Nature Publishing Group UK
2019
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| 主題: | |
| オンライン・アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6744502/ https://ncbi.nlm.nih.gov/pubmed/31519899 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-12214-5 |
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