首页|1848-2019年大兴安岭卧牛湖湖泊环境演变及其驱动因素

1848-2019年大兴安岭卧牛湖湖泊环境演变及其驱动因素

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湖泊生态环境演变过程和驱动机制研究对湖区生态系统的恢复至关重要.本文针对东北近现代湖泊生态环境重建研究相对不足的现状,以阿尔山浅水湖泊——卧牛湖为研究对象,在210Pb和137Cs建立的精确年代基础上,通过沉积岩芯的正构烷烃、粒度、总有机碳(TOC)、总氮(TN)和碳氮比(C/N)等多指标分析,结合流域现代监测和历史资料,重建了 1848-2019年来卧牛湖生态环境(包括藻类、水生植物等)的演化过程,并评价了多种环境压力对湖泊生态演变的影响.20世纪40年代之前,湖泊生态环境处于自然演化阶段,20世纪40年代之后,人类开始通过农业施肥和用水灌溉对湖泊环境产生影响,并在20世纪90年代显著加强,导致短链正构烷烃指示的藻类生物急剧上升.冗余分析和方差分解分析结果显示,在20世纪40-90年代,营养因子、气候因子和流域侵蚀共同作用影响湖泊生态环境演化;20世纪90年代以来,人类活动和营养因子成为湖泊生态环境变化的主控因子,人为干扰对湖泊环境影响显著加强,多种压力的胁迫作用导致了湖泊向富营养化状态的转变.
Environmental evolution and driving factors of Woniu Lake in the Da Hinggan Mountains in 1848-2019
Over the past 2 centuries,the lakes of the Northeast Plain and mountainous regions have been sub-jected to the dual impacts of climate change and human activities,leading to a series of ecological degradation issues.Understanding the historical evolution and driving mechanisms of lake ecological environments is cru-cial for the restoration of lake ecosystems in the future.However,there is a research gap in the reconstruction of the ecological environment of modem lakes in Northeast China.To address this,we utilize sediment n-al-kanes,grain size,total organic carbon(TOC),total nitrogen(TN),and carbon-to-nitrogen ratio(C/N)to invest-igate the evolutionary patterns of Woniu Lake over the past 200 years based on 210Pb and 137Cs dating.By integ-rating modem monitoring data and historical records of the basin,we further evaluate the driving factors be-hind various environmental pressures on the lake's evolution.The results showed that the environmental evolu-tion of Woniu Lake is broadly consistent with regional socio-economic transitions.Prior the 1940s,Woniu Lake was in a natural evolutionary phase with low and stable productivity,and its organic matter was primarily derived from external sources.Aquatic plant biomass was low,and the lake was in a relatively weak hydro-dynamic conditions.The watershed environment was stable,with forest coverage dominant and minimal hu-man impact.However,from the 1940s to the 1990s,human activities such as agricultural irrigation and defor-estation exacerbated the decline in lake water levels and the input of external nutrients,resulting in elevated primary productivity and enhanced contributions from autochthonous organic matter,with organic matter in-puts mainly from large aquatic plants.This led to a degradation of the lake's ecological environment,but without any significant state changes.After the 1990s,the algal productivity indicated by short-chain n-alkanes of Woniu Lake sharply increased due to the rapid development of modem industry and urbanization in the basin,leading to a transition to eutrophication.Redundancy analysis and variation partitioning analyses showed that nutrient factors played a key role in influencing the ecological evolution of Woniu Lake,independently ac-counting for 30.3%of the variance,alongside climate factors and watershed erosion from the 1950s to the 2020s.Since the 1990s,human activity factors became predominant over natural environmental factors and,in interaction with nutrient factors,became the main control of the short-term organic matter sources in Woniu Lake.The significant enhancement of human interference has led to the lake's transition to eutrophication un-der the combined stress of multiple pressures.

Aershan Areathe Da Hinggan Mountainslake ecological environment evolutionn-alkanesNortheast ChinaWoniu Lake

李启航、张灿、赵成

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南京大学地理与海洋科学学院,江苏南京 210023

中国科学院南京地理与湖泊研究所湖泊与环境国家重点实验室,江苏南京 210008

阿尔山地区 大兴安岭 湖泊生态环境演变 正构烷烃 东北地区 卧牛湖

国家自然科学基金项目国家自然科学基金项目

4217115142007401

2024

地理科学
中国科学院 东北地理与农业生态研究所

地理科学

CSTPCDCSSCICHSSCD北大核心
影响因子:3.117
ISSN:1000-0690
年,卷(期):2024.44(7)