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In-lake processing counteracts the effect of allochthonous input on the composition of color dissolved organic matter in a deep lake. | LitMetric

In-lake processing counteracts the effect of allochthonous input on the composition of color dissolved organic matter in a deep lake.

Sci Total Environ

State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; University of Chinese Academy of Sciences, Beijing 100049, China.

Published: January 2023

AI Article Synopsis

  • Color dissolved organic matter (CDOM) in lakes is influenced by both external (allochthonous) inputs and internal (autochthonous) production, significantly affecting its composition and cycling.
  • A study was conducted in Lake Fuxian, China, to analyze CDOM during the wet season and compare its characteristics with other lakes, revealing that riverine CDOM had higher levels of humic-like substances while Lake Fuxian's CDOM was mainly protein-like.
  • The findings showed that although CDOM composition varied across various lakes, the quantity increased significantly in deeper lakes with well-vegetated catchments, suggesting that allochthonous inputs impact CDOM but can be moderated by in-lake processing dynamics.

Article Abstract

Color dissolved organic matter (CDOM) plays a key role in lacustrine ecosystems and its composition is commonly mediated by the allochthonous input and autochthonous production. Deep lakes have a strong in-lake processing, which highly affects the sources, composition and cycle of CDOM. Here, the second deepest lake (Lake Fuxian) in China was selected to investigate the effects of allochthonous input and in-lake processing on lacustrine CDOM in deep lakes. Firstly, a detailed survey on CDOM composition across Lake Fuxian in the top water layer and inflowing rivers was carried out in the wet season representing the allochthonous input. In addition, CDOM in Lake Fuxian was compared with those in other lakes with distinct catchment characteristics and lake morphology. The results showed that compared to lacustrine CDOM in Lake Fuxian, the riverine CDOM contained much more humic-like substances, resulting in the humic-like fluorescence intensity peaked at the confluence of rivers into Lake Fuxian. In contrast, CDOM in Lake Fuxian was dominated by the protein-like substance. Comparison of CDOM composition among Lake Fuxian (well-vegetated catchment, deep lakes) with other diverse lakes in China (shallow/deep lakes with poor-vegetated catchment, and shallow lakes with well-vegetated catchment) showed similar CDOM quality in all type lakes, which were dominated by non-humified and autochthonous CDOM. Yet, CDOM quantity increased as the orders of deep lakes within poor-vegetated (Tibetan deep lakes) < the deep lake within well-vegetated catchment (Lake Fuxian) < shallow lakes within poorly-vegetated catchment (Tibetan shallow lakes) < shallow lakes within well-vegetated catchment (lakes along the middle and lower reaches of Yangtze River). Our results evidenced that the effect of allochthonous input on CDOM composition could be counteracted by in-lake processing in deep lakes. For deep lakes, a comprehensive understanding of in-lake processing of CDOM is critical for predicting lacustrine DOM composition and cycle.

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Source
http://dx.doi.org/10.1016/j.scitotenv.2022.158970DOI Listing

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