Deep-sea gas hydrate mounds and chemosynthetic fauna discovered at 3640 m on the Molloy Ridge, Greenland Sea
Abstract Methane seepage at the seafloor can form gas hydrate and sustain chemosynthetic communities of deep-sea animals. Most known hydrate seeps occur shallower than 2000 m on continental slopes, whereas hydrothermal vents are found at greater depths along active spreading centres. Here we report...
محفوظ في:
| المؤلفون الرئيسيون: | , , , , , , , , |
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| التنسيق: | Artigo |
| اللغة: | Inglês |
| منشور في: |
Nature Portfolio
2025-12-01
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| سلاسل: | Nature Communications |
| الوصول للمادة أونلاين: | https://doi.org/10.1038/s41467-025-67165-x |
| الوسوم: |
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