首页> 外文期刊>The Science of the Total Environment >The sensitivity of the carbon sink by coupled carbonate weathering to climate and land-use changes: Sediment records of the biological carbon pump effect in Fuxian Lake, Yunnan, China, during the past century
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The sensitivity of the carbon sink by coupled carbonate weathering to climate and land-use changes: Sediment records of the biological carbon pump effect in Fuxian Lake, Yunnan, China, during the past century

机译:碳酸盐风化耦合对碳汇的敏感性对气候和土地利用变化的影响:过去一个世纪云南抚仙湖生物碳泵效应的泥沙记录

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Recent studies show that the carbon sink attributable to the weathering of carbonate rocks may have been greatly underestimated if the biological carbon pump (BCP) effect in transferring dissolved inorganic carbon (DIC) to organic carbon (autochthonous OC) by aquatic photoautotrophs is neglected. The uptake of DIC by aquatic photo-autotrophs may reach 0.2 to 0.7 Pg C/a globally, indicating that the carbon sink by the coupled carbonate weathering with aquatic photosynthesis mechanism (CCW) may be an important control in climate change. In order to understand the sensitivity of the CCW carbon sink to changes of climate and land-use, a systematic study of modern trap and 100-year-long core sediments was conducted in Fuxian Lake, (Yunnan, SW China), the second-deepest plateau oligotrophic freshwater lake in China. It was found that (1) the autochthonous OC in the lake sediments was characterized by lower C/N ratios and higher δ~(13)C_(org). By means of an n-alkanes compound calculation, the proportions of autochthonous OC were determined to be in the range, 60-68% of all OC; (2) increase in the autochthonous OC accumulation rate (OCAR_(auto)) was accompanied by an increase in the inorganic carbon accumulation rate (ICAR) in both the trap and core sediments. In particular, the post-1950 OCAR_(auto) was estimated to be about 6.9 times that for the period. 1910-1950; (3) OCAR_(auto) in core sediments increased significantly with global warming and land-use change, from 1.06 g C m~(-2) yr~(-1) in 1910 to 21.74 g C m~(-2) yr~(-1) in 2017. The increasing carbon sink may act as a negative feedback on global warming if the trend holds for all lakes globally. This study is the first to quantify the burial flux of organic carbon generated by the BCP effect in lakes and may contribute to solving the problem of the missing carbon sink in the global carbon cycle.
机译:最近的研究表明,如果忽略了由水生自养生物将溶解的无机碳(DIC)转移到有机碳(自生OC)中的生物碳泵(BCP)效应,则可能大大低估了归因于碳酸盐岩风化的碳汇。水生自养生物对DIC的吸收全球可能达到0.2至0.7 Pg C / a,这表明碳酸盐风化与水生光合作用机制(CCW)耦合引起的碳汇可能是气候变化的重要控制。为了了解CCW碳汇对气候和土地利用变化的敏感性,我们在抚仙湖(中国西南部云南省)进行了系统研究,研究了现代圈闭和长达100年的核心沉积物。中国最深的高原贫营养淡水湖。结果表明:(1)湖泊沉积物中的土体OC具有较低的C / N比和较高的δ〜(13)C_(org)特征。通过正构烷烃化合物的计算,确定了本地OC的比例在所有OC的60-68%的范围内。 (2)原生碳的OC累积速率(OCAR_(auto))的增加伴随着圈闭和岩心沉积物中无机碳的累积速率(ICAR)的增加。特别是,估计1950年后的OCAR_(自动)约为该时期的6.9倍。 1910年至1950年; (3)随着全球变暖和土地利用的变化,核心沉积物中的OCAR_(auto)显着增加,从1910年的1.06 g C m〜(-2)yr〜(-1)增加到21.74 g C m〜(-2)yr在2017年达到〜(-1)。如果全球所有湖泊的碳排放趋势都持续增长,那么碳汇的增加可能会对全球变暖产生负面影响。这项研究是第一个量化由BCP效应在湖泊中产生的有机碳的埋藏通量的方法,可能有助于解决全球碳循环中缺少碳汇的问题。

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