文献类型：期刊文献

英文题名：Quantitative Holocene climate reconstruction and anthropogenic impact analysis based on the pollen records in peat sediment in Southern China

作者：Zhao, Lin[1,2];Zeng, Yaoyao[1];Rao, Zhiguo[1,2];Huang, Chao[3];Li, Yunxia[1,2];Liu, Lidan[1,2];Ma, Chunmei[4]

机构：[1]Hunan Normal Univ, Coll Geog Sci, Hunan Prov Key Lab Ecoenvironm Changes & Carbon Se, Changsha 410081, Peoples R China;[2]Hunan Normal Univ, Inst Interdisciplinary Studies, Changsha 410081, Peoples R China;[3]Guangdong Ocean Univ, Coll Ocean & Meteorol, Lab Coastal Ocean Variat & Disaster Predict, Zhanjiang 524088, Peoples R China;[4]Nanjing Univ, Sch Geog & Ocean Sci, Nanjing 210023, Peoples R China

年份：2024

卷号：234

外文期刊名：GLOBAL AND PLANETARY CHANGE

收录：SCI-EXPANDED(收录号：WOS:001195413800001)、、EI(收录号：20241015672945)、Scopus(收录号：2-s2.0-85186412022)、WOS

基金：We are grateful to Shikai Wei, Yiping Tian, and Haichun Guo for their help in field sampling. This study was supported by the National Natural Science Foundation of China (grants 42271168, 42171156, 42001080) , the Scientific Research Project of Education Department of Hunan Province, China (grant 23A0052) , the Ministry of Science and Tech- nology of China (the Global Change Program, grant number 2016YFA0600503) and the Aid Program for Science and Technology Innovative Research Team in Higher Educational Institutions of Hunan Province.

语种：英文

外文关键词：Pollen analysis; Quantitative reconstruction; Climate change; Anthropogenic impacts; HII; Dongting Lake Watershed

外文摘要：The quantitative reconstruction of Holocene paleoclimate is pivotal for unraveling the evolution of East Asian Monsoon (EAM). Some recent studies have highlighted the escalating human activities in the late Holocene, which could potentially pose significant challenges to the precise quantitative reconstruction of paleoclimate. In this study, we undertake a quantitative reconstruction of Holocene climate and human influence index (HII) based on pollen data from the Shiwangutian (SWGT) in Southern China. This is achieved by developing and applying a pollen-based calibration model utilizing Locally Weighted Average-Partial Least Squares Regression (LWWA-PLS) and the Modern Analogue Technique (MAT). Our findings reveal that evergreen forests experienced expansion between 11.6 and 9.0 cal ka BP, coinciding with elevated Mean Annual Precipitation (Map) and Mean Annual Temperature (Mat) levels. These patterns signify a progressively warm and wet climate during this period. Subsequently, evergreen forests achieved their maximum abundance between 9.0 and 4.0 cal ka BP, aligning with a notable increase in vegetation richness, indicating a warmer and wetter climate during the midHolocene. Notably, during the interval of 6.0-4.0 cal ka BP, the Map, Mat, and Precipitation of Warmest Month (Mpwa) reached the Holocene optimum, approximately 14% higher than modern. Consequently, we deduce that in the early and middle Holocene, when the monsoon was particularly strong, synchronous changes in precipitation fostered the regional expansion of evergreen broad-leaved forests. Furthermore, the record demonstrates a substantial reduction in forest cover and a noteworthy increase in the HII value since 4.0 cal ka BP, likely attributable to anthropogenic impacts. Our analysis suggests that the influence of anthropogenic activities surpassed that of natural climate factors in shaping regional vegetation cover. These findings offer insights into potential drivers of climate change. As a preliminary conclusion, we propose that the summer insolation, ice sheets, and meltwater fluxes were the primary controlling factors for climate variations during the early to midHolocene in Southern China.