Microbial Sulfate Reduction Potential in Coal-Bearing Sediments Down to ~2.5 km below the Seafloor off Shimokita Peninsula, Japan

Sulfate reduction is the predominant anaerobic microbial process of organic matter mineralization in marine sediments, with recent studies revealing that sulfate reduction not only occurs in sulfate-rich sediments, but even extends to deeper, methanogenic sediments at very low background concentrati...

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Detalles Bibliográficos
Autores principales: Glombitza, Clemens, Adhikari, Rishi R., Riedinger, Natascha, Gilhooly, William P., Hinrichs, Kai-Uwe, Inagaki, Fumio
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2016
Materias:
Microbiology
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5051215/
https://www.ncbi.nlm.nih.gov/pubmed/27761134
http://dx.doi.org/10.3389/fmicb.2016.01576

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5051215/
https://www.ncbi.nlm.nih.gov/pubmed/27761134
http://dx.doi.org/10.3389/fmicb.2016.01576

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