Cold seep sediment prokaryotic lineages exhibit habitat preference.
Lineages involved in geochemical cycling of carbon, sulfur, and nitrogen can also utilize biomacromolecules.
Chitin is characterized as one of the most abundant biomacromolecule and an enduring impact of seep activity.
Coexistence of chitin and nitrogen metabolic pathways suggests chemoorganotroph-driven N cycling in cold seep.
The cold seep derived chitinase exhibits increased activity under conditions of 15 MPa and 4°C.
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| Chen Y., Yang J., Huang X., et al. (2025). Exploring the role of organotrophic microbes in geochemical cycling of cold seep sediments. The Innovation Geoscience 3:100123. https://doi.org/10.59717/j.xinn-geo.2024.100123 |
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Phylogeny and niche prevalence of MAGs derived from sediments of Haima cold seep
Metabolic potentials of MAGs in C, N, S geochemical cycling
Functional profiles of MAGs in organic compound utilization
Potential contribution of chitin to carbon and nitrogen cycling in Haima cold seep
Genomic context of chitin degrading genes and schematic overview of pathways for chitin degradation
Catalytic and structural properties of GH18 chitinase IA32Chi641