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

• Published in: Global and planetary change Vol. 234; p. 104390
• Main Authors: Zhao, Lin, Zeng, Yaoyao, Rao, Zhiguo, Huang, Chao, Li, Yunxia, Liu, Lidan, Ma, Chunmei
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.03.2024
• Subjects: Anthropogenic impacts; Climate change; Dongting Lake Watershed; HII; Pollen analysis; Quantitative reconstruction; Anthropogenic impacts; Climate change; HII; Quantitative reconstruction; Dongting Lake Watershed; Pollen analysis
• DOI: 10.1016/j.gloplacha.2024.104390
• ISSN: 0921-8181

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 mid-Holocene. 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 mid-Holocene in Southern China. •Map, Mat, and Mpwa reached a Holocene peak between 6.0 and 4.0 cal ka BP.•An increased HII values since 4.0 cal ka BP, indicating anthropogenic influence.•Summer insolation, ice sheets, and meltwater fluxes were the primary drivers of climate change.