GSTDTAP  > 气候变化
DOI10.1029/2021GL094869
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
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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
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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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