D-amino acid metabolic versatility as a common adaptive strategy in the Mariana Trench microbiome

  • 0State Key Laboratory of Microbial Metabolism, School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai, China.

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Summary

This summary is machine-generated.

Microbes in deep-sea trenches can metabolize D-amino acids (D-AAs), challenging the idea that they are always recalcitrant. This suggests D-AA turnover is environmentally dependent in the hadal zone.

Area Of Science

  • Marine microbiology
  • Biogeochemistry
  • Molecular ecology

Background

  • Hadal trenches host microbial communities crucial for recalcitrant dissolved organic matter (RDOM) turnover.
  • The role of microbes in D-amino acid (D-AA) cycling within deep-sea RDOM remains largely unexplored.
  • D-AAs are significant components of deep-sea RDOM and indicators of organic matter recalcitrance.

Purpose Of The Study

  • To investigate the metabolic potential of D-AAs in the hadal zone.
  • To identify microbial taxa involved in D-AA metabolism.
  • To understand the ecological significance of D-AA turnover in extreme deep-sea environments.

Main Methods

  • Curated a D-AA functional gene database for metagenomic analysis.
  • Identified D-AA anabolic and catabolic genes in Mariana Trench water column and sediment samples.
  • Analyzed bacterial and archaeal genomes for D-AA gene presence.
  • Examined the correlation between D-AA genes and central carbon metabolism/ammonia oxidation genes.

Main Results

  • Identified diverse D-AA metabolic genes correlated with central carbon and ammonia oxidation pathways.
  • Found that 93.6% of recovered microbial genomes possess D-AA functional genes.
  • Discovered glutamate racemase in ammonia-oxidizing archaea, suggesting D-glutamate integration into hadal biogeochemical cycles.
  • Observed increased D-AA production and degradation potential with water depth, higher in seawater than sediment.

Conclusions

  • D-AA metabolism is a prevalent ecological function in the deepest ocean, driven by diverse microbial taxa.
  • The ubiquitous presence of glutamate racemase in ammonia-oxidizing archaea highlights their role in hadal D-glutamate cycling.
  • Increased D-AA turnover with depth suggests an adaptive response to extreme hadal conditions, challenging the notion of constant D-AA recalcitrance.

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