Evidence for massive emission of methane from a deep‐water gas field during the Pliocene
Geologic hydrocarbon seepage is a natural atmospheric source of methane, considered to prevail in terrestrial and shallow‐water areas; deep‐water methane seepage is expected to have no atmospheric impact, as gas is typically consumed throughout the water column. Here, we present evidence for a sudde...
| Những tác giả chính: | , , , |
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| Định dạng: | Journal article |
| Ngôn ngữ: | English |
| Được phát hành: |
National Academy of Sciences
2020
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