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Photochemical and Microbial Degradation of Chromophoric Dissolved Organic Matter Exported From Tidal Marshes
Author(s) -
Logozzo Laura,
Tzortziou Maria,
Neale Patrick,
Clark J. Blake
Publication year - 2021
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
eISSN - 2169-8961
pISSN - 2169-8953
DOI - 10.1029/2020jg005744
Subject(s) - colored dissolved organic matter , dissolved organic carbon , environmental chemistry , estuary , spectral slope , chemistry , biogeochemical cycle , organic matter , environmental science , phytoplankton , oceanography , nutrient , geology , spectral line , physics , organic chemistry , astronomy
Wetlands export chromophoric dissolved organic matter (CDOM) to estuaries, where CDOM is removed and transformed through biotic and abiotic process, subsequently impacting nutrient cycling, light availability, ecosystem metabolism, and phytoplankton activity. We examined the bioavailability and photoreactivity of CDOM exported from four Chesapeake Bay tidal marshes across three seasons and along an estuarine salinity gradient using three incubation treatments: 14‐day microbial (MD), 7‐day combined photochemical/microbial (PB + MD), and 7‐day microbial incubation after photobleaching (MD after PB). CDOM absorption at 300 nm ( a CDOM 300) and dissolved organic carbon (DOC) concentrations showed strong seasonality, with minima in winter, but CDOM quality (absorption spectral slopes, fluorescence component ratios) was less variable seasonally. PB + MD over 7 days decreased a CDOM 300 (−56.0%), humic‐like fluorescence (−67.6%), and DOC (−17.8%), but increased the spectral slope ratio S R (= S 275–295 /S 300–350 ) (+94.8%), suggesting a decrease in CDOM molecular weight. Photochemistry dominated the PB + MD treatment. Photoreactivity was greater during the winter and in marsh/watershed versus down‐estuary sites, likely due to less previous light exposure. Prior photobleaching increased the bioavailability of marsh‐exported CDOM, resulting in a greater loss of a CDOM 300 and DOC, and a greater increase in humic‐like fluorescence (−6.0%, −5.9%, and +18.4% change, respectively, over 7‐day MD after PB incubations, vs. −2.8%, −5.5%, and +2.6% change, respectively, over 14‐day MD incubations). CDOM exported from a marsh downstream of a major wastewater treatment plant showed the greatest photoreactivity and bioavailability. This highlights the significance of human activity on estuarine CDOM quality and biogeochemical cycles.