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高浓度硫酸盐与气候变暖在恒河沉积物-水界面缺氧条件下产生生态系统反馈。

High Concentration of Sulphate Coupled with Climate Warming Generates Ecosystem Feedback Under Sub-Oxic Conditions at Sediment-Water Interface in the Ganga River.

机构信息

Ganga River Ecology Research Laboratory, Environmental Science Division, Centre of Advanced Study in Botany, Institute of Science, Banaras Hindu University, Varanasi, 221005, India.

出版信息

Bull Environ Contam Toxicol. 2023 Sep 14;111(3):40. doi: 10.1007/s00128-023-03790-w.

DOI:10.1007/s00128-023-03790-w
PMID:37707629
Abstract

Here, we quantified sediment phosphorus (P) release in relation to concentrations of dissolved oxygen (DO) and sulphate, and increase in temperature in a major river of India subjected to long-term human perturbations. We found a substantial increase in sediment P release, an ecosystem feedback, at higher concentrations of sulphate, more towards the lower end of DO concentrations. A 2°C warming increased sediment P release upto 25.21% and caused a drop in DO level by 16%. Our findings reconcile the observed sulphate-driven changes in sediment P release across systems, and provide first experimental evidence of warming-induced increases. Our results imply that aquatic ecosystems will undergo self-fertilizing effect as the planet warming interacts with other human perturbations. This has implications for eutrophication linkages and ecosystem functioning.

摘要

在这里,我们量化了印度一条主要河流中与溶解氧 (DO) 和硫酸盐浓度以及温度升高有关的沉积物磷 (P) 释放情况。我们发现,在硫酸盐浓度更高、DO 浓度更低的情况下,沉积物 P 释放大量增加,这是一种生态系统反馈。升温 2°C 使沉积物 P 释放增加了 25.21%,并导致 DO 水平下降了 16%。我们的研究结果解释了在不同系统中观察到的硫酸盐驱动的沉积物 P 释放变化,并提供了变暖引起的增加的第一个实验证据。我们的研究结果表明,随着地球变暖与其他人为干扰相互作用,水生生态系统将经历自我施肥效应。这对富营养化的联系和生态系统功能有影响。

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