Organic carbon source tracing and the BCP effect in the Yangtze River and the Yellow River: Insights from hydrochemistry, carbon isotope, and lipid biomarker analyses

IF 8.2 1区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES Science of the Total Environment Pub Date : 2022-03-15 DOI:10.1016/j.scitotenv.2021.152429
Min Zhao , Hailong Sun , Zaihua Liu , Qian Bao , Bo Chen , Mingxing Yang , Hao Yan , Dong Li , Haibo He , Yu Wei , Guanxia Cai
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引用次数: 14

Abstract

Autochthonous organic carbon (AOC) formed by biological carbon pump (BCP) in surface waters may serve as a significant carbon sink. The locations, magnitudes, variations and mechanisms responsible for the terrestrial missing carbon sink by BCP are uncertain, especially in large river systems. In this study, hydrochemical characteristics, carbon isotope compositions of dissolved inorganic carbon (DIC) and organic carbon (OC), n-alkane homologues and C/N ratios of organic matter along the Yangtze River and the Yellow River were investigated to constrain the OC source and the significance of BCP effect. It was found that (1) DIC concentrations in the Yellow River were much higher than those in the Yangtze River, which was controlled primarily by the temperature effect; (2) AOC in the both rivers was characterized by lower C/N ratios and δ13CPOC values. Based on calculation of n-alkanes compounds, the AOC proportions ranged from 29 to 88% (49% on average, with a higher proportion (55%) in the rainy season than in the dry season (46%)) and 19–68% (41% on average; with a lower proportion in the rainy season (31%) than in the dry season (51%)) in the Yangtze River and the Yellow River, respectively, indicating intense aquatic production. Low dissolved CO2 concentration (6.17 μmol/L on average) of the Yangtze River limited the aquatic production and decreased the BCP effect in the dry season, indicated by lower AOC proportion. However, the BCP effect increased in the Yellow River in the dry season mainly due to the increased light penetration; (3) even in high turbidity riverine systems such as the Yellow River, the aquatic photosynthetic uptake of DIC could produce considerable AOC. These findings clearly show the formation of AOC by BCP in both the clear and high turbidity riverine systems, suggesting a potential direction for finding the terrestrial missing carbon sink.

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长江和黄河有机碳源示踪及BCP效应:来自水化学、碳同位素和脂质生物标志物分析的见解
生物碳泵(BCP)在地表水中形成的原生有机碳(AOC)可能是一个重要的碳汇。陆地碳汇丢失的位置、大小、变化和机制是不确定的,特别是在大型河流系统中。本研究通过对长江和黄河沿岸水体化学特征、溶解无机碳(DIC)和有机碳(OC)碳同位素组成、正构烷烃同质物和有机质C/N比值的研究,来约束OC来源和BCP效应的意义。结果表明:(1)黄河DIC浓度明显高于长江,主要受温度效应控制;(2)两河AOC均表现为较低的C/N比值和δ13CPOC值。基于正构烷烃化合物的计算,AOC的比例为29 ~ 88%(平均49%,雨季的比例为55%,旱季的比例为46%)和19 ~ 68%(平均41%);在长江和黄河,雨季的比例(31%)分别低于旱季(51%),表明水产生产强度较大。较低的溶解CO2浓度(平均6.17 μmol/L)限制了长江旱季水产生产,降低了BCP效应,表现为较低的AOC比例。枯水期黄河BCP效应增强,主要是由于透光量增加所致;(3)即使在黄河等高浊度河流系统中,水生光合作用对DIC的吸收也能产生可观的AOC。这些发现清楚地表明,在清澈和高浊度的河流系统中,BCP都形成了AOC,这为寻找陆地缺失的碳汇提供了潜在的方向。
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来源期刊
Science of the Total Environment
Science of the Total Environment 环境科学-环境科学
CiteScore
17.60
自引率
10.20%
发文量
8726
审稿时长
2.4 months
期刊介绍: The Science of the Total Environment is an international journal dedicated to scientific research on the environment and its interaction with humanity. It covers a wide range of disciplines and seeks to publish innovative, hypothesis-driven, and impactful research that explores the entire environment, including the atmosphere, lithosphere, hydrosphere, biosphere, and anthroposphere. The journal's updated Aims & Scope emphasizes the importance of interdisciplinary environmental research with broad impact. Priority is given to studies that advance fundamental understanding and explore the interconnectedness of multiple environmental spheres. Field studies are preferred, while laboratory experiments must demonstrate significant methodological advancements or mechanistic insights with direct relevance to the environment.
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