4.7 Article

Sources and compositional characterization of chromophoric dissolved organic matter in a Hainan tropical mangrove-estuary

Journal

JOURNAL OF HYDROLOGY
Volume 600, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.jhydrol.2021.126572

Keywords

CDOM; Dongzhai Harbor estuary; Mangrove; Absorption; EEM-PARAFAC; Biogeochemical process

Funding

  1. National Natural Science Foundation of China [41521001, 41772255]
  2. 111 Program (The State Administration of Foreign Experts Affairs and the Ministry of Education of China) [B18049]
  3. Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) [CUGGC07]
  4. China Geological Survey [DD20190304]

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Chromophoric dissolved organic matter (CDOM) is a key optically active component in estuarine DOM, influencing nutrient and micronutrient biogeochemical processes. Sources of CDOM in tropical mangrove estuaries include terrestrial/anthropogenic inputs, riverine runoff, and mangrove porewater exchange. Understanding CDOM composition and sources is crucial for biogeochemical cycling in mangrove estuaries.
Chromophoric dissolved organic matter (CDOM) is a major optically active component of DOM in estuaries that plays a significant part in maintaining the ecosystem sustainability of mangrove forests via affecting nutrient and micronutrient ((micro)nutrient) biogeochemical processes and pathways. This study was conducted in Hainan Dongzhai Harbor to better understand the sources, composition, and behaviors of CDOM in a tropical mangrove estuary. Water samples were collected from the upper fluvial mangrove zones to the lower marine endmember along the estuarine salinity gradient and analyzed by absorption and fluorescence spectroscopy combined with parallel factor analysis (PARAFAC). DOC, TDN, TDSi, Mn, Ba, and optical characteristics, i.e., a(254), SUVA, HIX, and the abundance of humic-like CDOM, are negatively correlated with salinity. Terrestrial/anthropogenic inputs, riverine runoff, and mangrove porewater exchange are sources of (micro)nutrients and aromatic CDOM into the estuary. In contrast, pH, DO, TDP, S-R, BIX, and tryptophan-like CDOM are positively correlated with salinity. This indicates saltwater dilution, tidal mixing, photo-oxidation, and microbial degradation processes promote the enrichment of low MW autochthonous CDOM and TDP, together with the removal of humic-like substances and other (micro)nutrients in the lower estuary. Overall, these findings have important implications for biogeochemical cycling processes driven by CDOM composition and sources in mangrove estuaries.

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