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Sedimentary biogeochemical record in Lake Gonghai: Implications for recent lake changes in relatively remote areas of China

机译:巩海湖的沉积生物地球化学记录:对中国相对偏远地区最近的湖泊变化的启示

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Owing to rapid socio-economic development and climate warming, lakes even in remote areas have experienced marked changes in the last century. However, there are few studies revealing the multi-faceted biogeochemical changes and disentangling impacts of human and climate in relatively remote lakes in China. In this study we reconstructed historical changes of geochemistry, nutrition, primary production, ecology, and pollution in an alpine lake (Gonghai) in central North China, and revealed coherent changes and drivers in relatively remote Chinese lakes by compiling other records. Results show that Lake Gonghai has experienced considerably biogeochemical changes since the 1980s induced mainly by increased regional human activities, with detected human-related changes occurring in the 1950s-70s. The most important change is a shift of diatom primary producers in the 1980s, caused mainly by an increase of regional atmospheric N and P deposition associated with rapid socioeconomic development. Another remarkable change is the increase of pollution levels since the 1980s, represented by heavy metals, also caused by atmospheric deposition. Compiled sediment records demonstrate similar biogeochemical changes in most lakes from relatively remote areas of China since the 1970s-80s, associated closely with increased inputs of human-induced atmospheric N, P and pollutants, whereas the influence of climate warming is likely limited. This study highlights markedly human-related biogeochemical changes in relatively remote Chinese lakes during the Anthropocene epoch. (C) 2018 Elsevier B.V. All rights reserved.
机译:由于社会经济的迅速发展和气候变暖,上世纪即使​​在偏远地区的湖泊也发生了显着变化。然而,很少有研究揭示出中国相对偏远的湖泊中生物地球化学的多方面变化以及人类和气候的令人费解的影响。在这项研究中,我们重建了华北中部一个高山湖泊(公海)的地球化学,营养,初级生产,生态和污染的历史变化,并通过汇编其他记录揭示了中国偏远湖泊的连贯变化和动因。结果表明,自1980年代以来,贡海湖经历了相当大的生物地球化学变化,这主要是由于区域人类活动的增加所致,在1950年代至70年代发生了与人类有关的变化。最重要的变化是1980年代硅藻初级生产者的转移,这主要是由于与快速的社会经济发展相关的区域大气N和P沉积增加。另一个显着变化是自1980年代以来污染水平的上升,以重金属为代表,也是由大气沉积引起的。汇编的沉积物记录表明,自1970年代至80年代以来,中国相对偏远地区的大多数湖泊都发生了类似的生物地球化学变化,与人为引起的大气氮,磷和污染物的投入增加密切相关,而气候变暖的影响可能是有限的。这项研究强调了人类世间人类时期在相对偏远的中国湖泊中与人类有关的生物地球化学变化显着。 (C)2018 Elsevier B.V.保留所有权利。

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