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Subduction zone forearc serpentinites as incubators for deep microbial life
Serpentinization-fueled systems in the cool, hydrated forearc mantle of subduction zones may provide an environment that supports deep chemolithoautotrophic life. Here, we examine serpentinite clasts expelled from mud volcanoes above the Izu–Bonin–Mariana subduction zone forearc (Pacific Ocean) that...
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| Опубликовано в: : | Proc Natl Acad Sci U S A |
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| Главные авторы: | , , , , , , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
National Academy of Sciences
2017
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| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5410786/ https://ncbi.nlm.nih.gov/pubmed/28396389 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1612147114 |
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