Sunlight stimulates microbial respiration of organic carbon October 17, 2017
Sunlight and microbes interact to degrade dissolved organic carbon (DOC) in surface waters, but scientists cannot currently predict the rate and extent of this degradation in either dark or light conditions. A recent study helps explain how sunlight alters organic matter composition.
The rates microbes can process DOC is likely governed by a combination of the abundance and instability of DOC exported from land to water and produced by photochemical processes, and the capacity and timescale that microbial communities have to adapt to metabolize DOC that has been exposed to sunlight. This new information could help develop more accurate methods for assessing past climate.
Photochemical processing of DOC likely supplies about one-third of the CO2 released from surface waters in the Arctic, by either directly mineralizing DOC to CO2 or indirectly altering DOC chemical composition and, in turn, rates of microbial respiration. At present, scientists cannot predict the rate and extent of this degradation in either dark or light conditions. A team of researchers from University of Michigan, Woods Hole Oceanographic Institution, Oregon State University, and EMSL, the Environmental Molecular Science Laboratory, a DOE Office of Science user facility, combined advanced characterization techniques to characterize microbial and DOC composition.
The researchers characterized outputs of short-term photochemical experiments using Fourier-Transform Ion Cyclotron Resonance mass spectrometry at EMSL along with measures of microbial activity, community composition, and gene expression. In dark conditions, they found microbes native to deep permafrost, or surface organic layer soils, degraded the DOC that was most abundant in either soil.
Read more at: https://phys.org/news/2017-10-sunlight-microbial-respiration-carbon.html#jCp