气候变化领域集成服务门户(CCPortal): Aquatic ecosystem responses to environmental and climatic changes in NE China since the last deglaciation (similar to 17, 500 cal yr BP) tracked by diatom assemblages from Lake Moon

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DOI	10.1016/j.quascirev.2021.107218
	Aquatic ecosystem responses to environmental and climatic changes in NE China since the last deglaciation (similar to 17, 500 cal yr BP) tracked by diatom assemblages from Lake Moon
	Chen, Jie; Liu, Jianbao; Ruhland, Kathleen M.; Smol, John P.; Zhang, Xiaosen; Zhang, Zhiping; Zhou, Aifeng; Shen, Zhongwei; Chen, Fahu
通讯作者	Liu, JB (通讯作者)
发表日期	2021
ISSN	0277-3791
EISSN	1873-457X
卷号	272
英文摘要	The scarcity of research in NE China on lake ecosystem responses to large-scale climate oscillations since the last deglaciation limits our abilities for informing conservation practices and policies in the context of recent global warming. Here, a high-resolution, sedimentary diatom record covering the past similar to 17,500 years was retrieved from Lake Moon, a small, hydrologically closed crater lake in the remote central part of the Great Khingan Mountain Range in NE China. We compare diatom changes with geochemical data from the same core, and with regional palynological and dust deposition records, to better understand the influences of long-term environmental and climatic variability on aquatic ecosystems in this climatically sensitive region. Several abrupt and pronounced shifts in dominance among diatom taxa corresponded to marked fluctuations in the climate regime since the last deglaciation. During the close of the Last Glacial Period, a series of short-lived diatom shifts that were indicative of an increase in nutrients, signaled the transition from the cold period of the Heinrich event 1 (similar to 17,500-similar to 14,700 cal yr BP) to the warmer Bolling - Allerod interstadial period (similar to 14,700-similar to 12,900 cal yr BP). The onset of the cold Younger Dryas period was marked by a brief rise to dominance of benthic taxa (similar to 12,900-similar to 11,800 cal yr BP), followed by a pronounced lake ecosystem shift to a new trophic state at the Pleistocene-Holocene transition (similar to 11,800-similar to 9900 cal yr BP), evidenced by an abrupt rise to dominance of several eutrophic diatom indicators (e.g. Cyclostephanos dubius, Aulacoseira ambigua and Stephanodiscus parvus). This nearly complete compositional turnover was indicative of an increase in phosphorus supply to the lake with the onset of a warmer and moister climate and an increased frequency of strong dust storms. During the mid-Holocene (similar to 6000 cal yr BP), a striking increase in the relative abundance of Discostella pseudostelligera and Asterionella formosa, at the expense of previously dominant eutrophic indicators, signified another lake ecosystem change from well-mixed, turbid and phosphorus-rich conditions to a lower nutrient state with longer open-water periods and increased thermal stability. The turnover to oligotrophic diatom taxa was likely in response to variations in seasonal temperature, precipitation and dust deposition. The diatom shifts of Lake Moon during the past similar to 17,500 years were directly or indirectly mediated by climate change that affected thermal stratification, productivity, lake level and trophic state. Our results indicate that climate change had an overarching control on aquatic ecosystem changes in the mountain regions of NE China since the last deglaciation. (C) 2021 Elsevier Ltd. All rights reserved.
关键词	ASIAN SUMMER MONSOON NORTHEAST CHINA INNER-MONGOLIA TIBETAN PLATEAU POLLEN RECORD HULUN LAKE MAAR LAKE HOLOCENE TEMPERATURE SEDIMENTS
英文关键词	Climate events; Lake paleoecology; Alpine lake; Dust deposition; Paleolimnology
语种	英语
WOS研究方向	Physical Geography ; Geology
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号	WOS:000708698300009
来源期刊	QUATERNARY SCIENCE REVIEWS
来源机构	中国科学院青藏高原研究所
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/260316
推荐引用方式 GB/T 7714	Chen, Jie,Liu, Jianbao,Ruhland, Kathleen M.,et al. Aquatic ecosystem responses to environmental and climatic changes in NE China since the last deglaciation (similar to 17, 500 cal yr BP) tracked by diatom assemblages from Lake Moon[J]. 中国科学院青藏高原研究所,2021,272.
APA	Chen, Jie.,Liu, Jianbao.,Ruhland, Kathleen M..,Smol, John P..,Zhang, Xiaosen.,...&Chen, Fahu.(2021).Aquatic ecosystem responses to environmental and climatic changes in NE China since the last deglaciation (similar to 17, 500 cal yr BP) tracked by diatom assemblages from Lake Moon.QUATERNARY SCIENCE REVIEWS,272.
MLA	Chen, Jie,et al."Aquatic ecosystem responses to environmental and climatic changes in NE China since the last deglaciation (similar to 17, 500 cal yr BP) tracked by diatom assemblages from Lake Moon".QUATERNARY SCIENCE REVIEWS 272(2021).