Dissolved organic matter distribution in the water column and sediment pore water in a highly anthropized coastal lagoon (Mar Menor, Spain): Characteristics, sources, and benthic fluxes

被引:2
|
作者
Amaral, V. [1 ,2 ]
Santos-Echeandia, J. [3 ]
Ortega, T. [2 ]
Alvarez-Salgado, X. A. [4 ]
Forja, J. [2 ]
机构
[1] Univ Republ, Ctr Univ Reg Este, Dept Interdisciplinario Sistemas Costero Marinos, Rocha, Uruguay
[2] Univ Cadiz, Dept Quim Fis, INMAR, Puerto Real, Spain
[3] Inst Espanol Oceanog IEO CSIC, Ctr Oceanog Vigo, Subida Radio Faro S-N, Vigo 36390, Spain
[4] CSIC, Inst Invest Marinas IIM, Vigo, Spain
关键词
Mar Menor; DOM; Benthic flux; Carbon; oM; Coastal lagoons; FLUORESCENCE SPECTROSCOPY; BIOGEOCHEMICAL DYNAMICS; GROUNDWATER DISCHARGE; CYMODOCEA-NODOSA; NITROGEN; CARBON; ABSORPTION; MEADOWS; CONSEQUENCES; TERRESTRIAL;
D O I
10.1016/j.scitotenv.2023.165264
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Coastal lagoons are among the most productive and biodiverse systems in the world and are important sentinels of climate change. The Mar Menor is one of the largest coastal lagoons in the Mediterranean, providing a variety of ecosystem services and resources to the community. However, in recent decades this lagoon has suffered drastic changes and degradation caused by human activities. We analyzed the concentration of dissolved organic carbon (DOC) and the optical properties of dissolved organic matter (DOM) in the water column and sediment pore water during the summer and winter of 2018 and during eighteen months from 2016 to 2018. Overall, we found that the composition of DOM is mainly related to and enhanced by anthropogenic activities and microbial metabolism. DOM enters the lagoon via urban and agricultural runoff, drainage systems, and wastewater treatment plants. Additionally, strong microbial metabolism in sediments leads to differences in DOM composition between water and sediments. In the water column, humic-like components accounted for 71 % of the total DOM, while protein-like compounds were most abundant in sediment pore water. We observed a strong seasonal variability associated with precipitation and the system collapse in 2016 (phytoplankton bloom), which resulted in the death of 80 % of macrophytes. The sediments act as a source of DOM to the overlying water, likely due to relatively high organic matter content and intense microbial activity, primarily through anaerobic pathways. Benthic fluxes of DOC ranged from 5.24 to 33.30 mmol m-2 d-1, being higher in winter than summer 2018 and decreasing from north to south, likely related to lower residence time in the northern basin, groundwater discharge and accumulation of organic matter from the dead meadows. We estimate a net flux of DOC from the Mar Menor toward the Mediterranean Sea of 1.57 x 107 mol yr-1.
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页数:12
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