Journal
JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
Volume 125, Issue 3, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2019JG005425
Keywords
photochemistry; bio-refractory DOC; DOM; CDOM; FDOM; oceans
Funding
- Natural Key Research and Development Program of China [2016YFC1401401]
- Natural Science Foundation of China [41376081, 41606098]
- Tianjin Natural Science Foundation [16JCQNJC08000]
- NSFC Open Research Cruise [NORC2017-05]
- China Scholarship Council
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Water samples collected from various depths of the offshore South China and Philippine Seas were exposed to solar-simulated radiation. Photomineralization of dissolved organic carbon (DOC) and photobleaching of chromophoric dissolved organic matter (CDOM) and its humic-like fluorescent constituent (FDOM) were observed in all samples. Protein-like FDOM was, however, either photo-decomposed or photo-produced, depending on the sample's depth. The photobleaching of CDOM and humic-like FDOM was much faster in deep than in shallow water samples while photomineralization displayed a weaker vertical zonation. Prior-irradiated deep water inoculated with surface-water bacteria showed enhanced microbial DOC removal but CDOM production. Results from this study suggest that deep-ocean CDOM and FDOM can barely survive photobleaching during one ocean mixing cycle, but photochemical turnover of the bio-refractory deep DOC is considerably longer than its average radiocarbon age. Coupled photochemical-microbial processes can not only remove part of the bio-refractory deep DOM but also regenerate part of it during ocean overturning circulation.
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