4.6 Review

Microbial degradation of various types of dissolved organic matter in aquatic ecosystems and its influencing factors

Journal

SCIENCE CHINA-EARTH SCIENCES
Volume 66, Issue 2, Pages 169-189

Publisher

SCIENCE PRESS
DOI: 10.1007/s11430-021-9996-1

Keywords

Dissolved organic matter (DOM); Microbes; Bioavailability; Bioreactivity; Intrinsic factors; Environmental factors; Nanoplastics

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Interactions between chemodiverse dissolved organic matter (DOM) and biodiverse microbes are influenced by numerous intrinsic and extrinsic factors, which are still not well understood. This study provides a comprehensive update and bridging of the interdisciplinary theme. Different ecosystems, such as algal-dominated aquatic ecosystems and ecosystems supplied by soil and vascular plants, have different types of DOM and microbial communities. Various microorganisms show evidence of being able to process different types of organics, but the chemical structure and bonds of the organics vary. Both intrinsic factors (such as DOM composition and structure) and extrinsic factors (such as sunlight and dissolved oxygen) play important roles in the interactions between DOM and microbes.
Interactions between chemodiverse dissolved organic matter (DOM) and biodiverse microbes are governed by a myriad of intrinsic and extrinsic factors which are not well understood. Here, we update and bridge the gap of this interdisciplinary theme comprehensively. At an ecosystem level, aquatic ecosystems dominated by algae-sourced DOM (e.g., eutrophic lake or coastal upwelling areas) harbor more biolabile DOM, such as directly assimilable monomers and readily hydrolysable biopolymers. However, other ecosystems prevailed by DOM supply from soil and vascular plants (e.g., river or wetland) have more biorefractory DOM, such as low molecular weight (LMW) residue of aliphatic C skeletons and geopolymers. A variety of heterotrophic bacteria, archaea, fungi, phagotrophic protists, and even photoautotrophic phytoplankton shows genomic and/or culturing experimental evidence of being able to process a diverse type of organics. The various biodegradable organics have different chemical structures and chemical bonds such as carbohydrates, amino acids, proteins, lignins, lipids, carboxylic acids, humic acids, hydrocarbons, and nanoplastics. Meanwhile, bio-production of metabolism intermediates and/or biorefractory organics (e.g., carboxyl-rich alicyclic molecules, CRAM) is observed despite general decay of bulk dissolved organic carbon (DOC) during bioassay experiments. In particular, emerging evidence shows that archaea contribute significantly to biomass in the marine mesopelagic zone and subsurface environments and their abundance often increases with depth in sediments. Furthermore, not only intrinsic factors (e.g., DOM composition and structure), but also extrinsic ones (e.g., sunlight and dissolved oxygen) play important roles in interplays between DOM and microbes.

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