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DOI10.1177/09596836211019093
The link between climate change and biodiversity of lacustrine inhabitants and terrestrial plant communities of the Uvs Nuur Basin (Mongolia) during the last three millennia
Rudaya, Natalia; Nazarova, Larisa; Frolova, Larisa; Palagushkina, Olga; Soenov, Vasiliy; Cao, Xianyong; Syrykh, Lyudmila; Grekov, Ivan; Otgonbayar, Demberel; Bayarkhuu, Batbayar
通讯作者Rudaya, N (通讯作者)
发表日期2021
ISSN0959-6836
EISSN1477-0911
起始页码1443
结束页码1458
卷号31期号:9
英文摘要The paper is focused on changes in biodiversity, the environment, and human activity in the Uvs Nuur Basin during the last three millennia based on biological and geochemical proxies from the lake Bayan Nuur. Regions with high biodiversity and relatively low anthropogenic pressures are typically the most vulnerable to both climate change and human activities. One such area is the Uvs Nuur Basin located on the north of the Great Lake Depression of Mongolia. The main objective of this study is to assess changes in the past biodiversity of the lake's microflora and microfauna, and surrounding vegetation biodiversity in the Uvs Nuur Basin, and to determine the main drivers of diversity change. Based on the analysis of pollen and chironomids we conclude that the most humid and afforested phase was between 1400 and 1800 CE. We assume that the Little Ice Age in the Uvs Nuur Basin was humid with mean annual precipitation ca. 305 mm/year and mean July temperature about 13 degrees C. Conversely, the warmest and most arid period was between 650 and 1350 CE with mean annual precipitation ca. 280 mm/year and mean July temperature of about 16 degrees C, attributed to the Medieval Warm Period. The biodiversity of terrestrial plants, chironomids, and Cladocera positive react to changes in annual precipitation and July temperature, whereas diatoms do not correlate directly to the climatic factors. The diversity and the evenness of plants are strongly correlated with the change in the leading biomes. The calculated species turnover suggests no significant changes in plant and Cladocera taxa composition, but significant changes in diatom and chironomid communities. This may be explained by the instability of lake ecology due to the fluctuation of the salinity and acidity of the water. An additional aim was to assess if dung fungi in lacustrine sediments reflect changes in human population density around the lake. We found that neither historical sources of human presence nor the influx of coprophilous fungi are correlated with the inferred climate changes. Coprophilous fungi can be used as individual or additional sources of assessment for the peopling and human-related herbivore density including overgrazing of the studied area.
关键词LATE HOLOCENE CLIMATEENVIRONMENTAL-CHANGESDATA SETPOLLENLAKEALTAIDIVERSITYRECORDSSIBERIARECONSTRUCTION
英文关键词anthropogenic activity; biodiversity; chironomids; Cladocera; diatoms; dung fungi; late-Holocene; LIA; Mongolia; paleoclimate; pollen
语种英语
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000657891500001
来源期刊HOLOCENE
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/260532
推荐引用方式
GB/T 7714
Rudaya, Natalia,Nazarova, Larisa,Frolova, Larisa,et al. The link between climate change and biodiversity of lacustrine inhabitants and terrestrial plant communities of the Uvs Nuur Basin (Mongolia) during the last three millennia[J]. 中国科学院青藏高原研究所,2021,31(9).
APA Rudaya, Natalia.,Nazarova, Larisa.,Frolova, Larisa.,Palagushkina, Olga.,Soenov, Vasiliy.,...&Bayarkhuu, Batbayar.(2021).The link between climate change and biodiversity of lacustrine inhabitants and terrestrial plant communities of the Uvs Nuur Basin (Mongolia) during the last three millennia.HOLOCENE,31(9).
MLA Rudaya, Natalia,et al."The link between climate change and biodiversity of lacustrine inhabitants and terrestrial plant communities of the Uvs Nuur Basin (Mongolia) during the last three millennia".HOLOCENE 31.9(2021).
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