Biogeochemical cycle of methanol in anoxic deep-sea sediments

Katsunori Yanagawa, Atsushi Tani, Naoya Yamamoto, Akihiro Hachikubo, Akihiro Kano, Ryo Matsumoto, Yohey Suzuki

Research output: Contribution to journalArticle

12 Citations (Scopus)

Abstract

The biological flux and lifetime of methanol in anoxic marine sediments are largely unknown. We herein reported, for the first time, quantitative methanol removal rates in subsurface sediments. Anaerobic incubation experiments with radiotracers showed high rates of microbial methanol consumption. Notably, methanol oxidation to CO2 surpassed methanol assimilation and methanogenesis from CO2/H2 and methanol. Nevertheless, a significant decrease in methanol was not observed after the incubation, and this was attributed to the microbial production of methanol in parallel with its consumption. These results suggest that microbial reactions play an important role in the sources and sinks of methanol in subseafloor sediments.

Original languageEnglish
Pages (from-to)190-193
Number of pages4
JournalMicrobes and environments
Volume31
Issue number2
DOIs
Publication statusPublished - Jun 25 2016

All Science Journal Classification (ASJC) codes

  • Ecology, Evolution, Behavior and Systematics
  • Soil Science
  • Plant Science

Fingerprint Dive into the research topics of 'Biogeochemical cycle of methanol in anoxic deep-sea sediments'. Together they form a unique fingerprint.

  • Cite this

    Yanagawa, K., Tani, A., Yamamoto, N., Hachikubo, A., Kano, A., Matsumoto, R., & Suzuki, Y. (2016). Biogeochemical cycle of methanol in anoxic deep-sea sediments. Microbes and environments, 31(2), 190-193. https://doi.org/10.1264/jsme2.ME15204