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Updated: May 28, 2026

Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O
08:05

Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O

Published on: October 7, 2020

Carbon and nitrogen assimilation in deep subseafloor microbial cells

Yuki Morono1, Takeshi Terada, Manabu Nishizawa

  • 1Kochi Institute for Core Sample Research, Japan Agency for Earth-Marine Science and Technology (JAMSTEC), Nankoku, Kochi 783-8502, Japan. morono@jamstec.go.jp

Proceedings of the National Academy of Sciences of the United States of America
|October 12, 2011
PubMed
Summary

Deep subseafloor microbes are metabolically active, utilizing glucose, pyruvate, and amino acids for growth. Their recovery in vitro is primarily limited by energy availability, not carbon or nitrogen compounds.

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