Submerged macrophyte-dominated systems fed by karst groundwater produce a significant autochthonous carbon sink in sediment: A mesocosm experiment study

The inland water portion of the carbon cycle is an essential component of the global carbon cycle and is a promising direction to seek missing carbon sinks. Inland waters fix inorganic carbon to form autochthonous organic carbon (Auto-OC) and accept laterally transferred terrestrial OC. Calculating the carbon sink flux of inland water requires a quantitative estimation of the proportion of the aforementioned processes. In the current study, n -alkanes are used as biomarkers and the dual carbon isotope method (Bayesian mixing model) is applied to estimate the proportions of Auto-OC in the sediment of a simulation site comprising five shallow submerged macrophyte-dominated subsystems. The study results showed that a high proportion of Auto-OC was present in all sediment, regardless of the season or subsystem. However, the proportions were higher in the warm-humid season than in the cold-dry season. Results from a correlation analysis showed that temperature-controlled seasonal variations in the photosynthetic strength of aquatic organisms are the most likely cause of this difference. The average deposition rates of total organic carbon and Auto-OC were high (66.7 and 58.2 g C/m 2 /yr, respectively). Throughout the year, the weighted average percentage of Auto-OC ranged from 76% to 90%, with a mean value of 86% in the five aquatic subsystems. Establishing and maintaining submerged macrophyte-dominated systems have a potential of decreasing carbon dioxide (CO 2 ) evasion and sequestrating more carbon (C) in headwaters. Working for clear submerged macrophyte-dominated lakes is beneficial for increasing carbon sinks. • Autochthonous organic carbon (Auto-OC) in inland waters is a crucial carbon cycle component. • Biomarkers and dual carbon isotopes were used to determine the proportion of Auto-OC. • High proportions and deposition rates of Auto-OC were observed in five artificial, submerged macrophyte-dominated systems. • Submerged macrophyte-dominated system showed substantial carbon sink potential.

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Publication Details

Journal
International Journal of Sediment Research
Published
2024-12-29
DOI
https://doi.org/10.1016/j.ijsrc.2024.12.006
Primary Topic
Aquatic Ecosystems and Phytoplankton Dynamics
Type
article
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article

Submerged macrophyte-dominated systems fed by karst groundwater produce a significant autochthonous carbon sink in sediment: A mesocosm experiment study

Xuejun He, Zaihua Liu, Qian Bao, Haibo He et al.
International Journal of Sediment Research
Aquatic Ecosystems and Phytoplankton Dynamics
article

Submerged macrophyte-dominated systems fed by karst groundwater produce a significant autochthonous carbon sink in sediment: A mesocosm experiment study

Xuejun He, Zaihua Liu, Qian Bao, Haibo He, Dong Li, Hailong Zhang, Min Zhao
article en

Abstract

The inland water portion of the carbon cycle is an essential component of the global carbon cycle and is a promising direction to seek missing carbon sinks. Inland waters fix inorganic carbon to form autochthonous organic carbon (Auto-OC) and accept laterally transferred terrestrial OC. Calculating the carbon sink flux of inland water requires a quantitative estimation of the proportion of the aforementioned processes. In the current study, n -alkanes are used as biomarkers and the dual carbon isotope method (Bayesian mixing model) is applied to estimate the proportions of Auto-OC in the sediment of a simulation site comprising five shallow submerged macrophyte-dominated subsystems. The study results showed that a high proportion of Auto-OC was present in all sediment, regardless of the season or subsystem. However, the proportions were higher in the warm-humid season than in the cold-dry season. Results from a correlation analysis showed that temperature-controlled seasonal variations in the photosynthetic strength of aquatic organisms are the most likely cause of this difference. The average deposition rates of total organic carbon and Auto-OC were high (66.7 and 58.2 g C/m 2 /yr, respectively). Throughout the year, the weighted average percentage of Auto-OC ranged from 76% to 90%, with a mean value of 86% in the five aquatic subsystems. Establishing and maintaining submerged macrophyte-dominated systems have a potential of decreasing carbon dioxide (CO 2 ) evasion and sequestrating more carbon (C) in headwaters. Working for clear submerged macrophyte-dominated lakes is beneficial for increasing carbon sinks. • Autochthonous organic carbon (Auto-OC) in inland waters is a crucial carbon cycle component. • Biomarkers and dual carbon isotopes were used to determine the proportion of Auto-OC. • High proportions and deposition rates of Auto-OC were observed in five artificial, submerged macrophyte-dominated systems. • Submerged macrophyte-dominated system showed substantial carbon sink potential.

International Journal of Sediment ResearchVol. 40(3)
Institute of Geochemistry (CN), University of Chinese Academy of Sciences (CN), Laoshan Laboratory
Openalex Percentile: Top 80%
Aquatic Ecosystems and Phytoplankton Dynamics
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