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DOI | 10.1029/2021GL094869 |
Hydrothermal vents are a source of old refractory organic carbon to the deep ocean | |
George W. Luther | |
2021-08-17 | |
发表期刊 | Geophysical Research Letters |
出版年 | 2021 |
英文摘要 | Based on the C-14 data of Druffel et al. (2021) along the Eastern Pacific Rise, DOC in the deep ocean is old and thus refractory. Their data in combination with previous He-3 data indicate that the source of this aged DOC is from the hot waters emanating from hydrothermal vents along the ridge axis. The isotopic and structural composition of the source DOC is unknown, which requires a concerted effort by the marine organic chemistry community to elucidate these chemical forms. |
领域 | 气候变化 |
URL | 查看原文 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/335969 |
专题 | 气候变化 |
推荐引用方式 GB/T 7714 | George W. Luther. Hydrothermal vents are a source of old refractory organic carbon to the deep ocean[J]. Geophysical Research Letters,2021. |
APA | George W. Luther.(2021).Hydrothermal vents are a source of old refractory organic carbon to the deep ocean.Geophysical Research Letters. |
MLA | George W. Luther."Hydrothermal vents are a source of old refractory organic carbon to the deep ocean".Geophysical Research Letters (2021). |
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