A novel approach for quantitatively distinguishing between anthropogenic and natural effects on paleovegetation

Author:

Fan Baoshuo12ORCID,Lu Houyuan23ORCID,Li Yuecong1,Shen Caiming4ORCID,Xu Qinghai1,Zhang Jianping2ORCID,Huan Xiujia25,Wang Yonglei6,Wang Ningyuan6,Xu Deke2ORCID,Dong Yajie2ORCID,Cui Anning2,Wu Naiqin2

Affiliation:

1. Hebei Key Laboratory of Environmental Change and Ecological Construction, College of Geographical Sciences, Hebei Normal University , Shijiazhuang 050024 , PR China

2. Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences , Beijing 100029 , PR China

3. University of Chinese Academy of Sciences , Beijing 100049 , PR China

4. Yunnan Key Laboratory of Plateau Geographical Processes and Environmental Changes, Faculty of Geography, Yunnan Normal University , Kunming 650500 , PR China

5. Shandong Provincial Key Laboratory of Soil Conservation and Environmental Protection, School of Resources and Environment, Linyi University , Linyi 276000 , PR China

6. Zhejiang Provincial Institute of Relics and Archaeology , Hangzhou 310014 , PR China

Abstract

Abstract How to distinguish and quantify past human impacts on vegetation is a significant challenge in paleoecology. Here, we propose a novel method, the error inflection point-discriminant technique. It finds out the inflection points (IPs) of the regression errors of pollen–climate transfer functions using modern pollen spectra from vegetation with different values of the Human Influence Index (HII), which represent the HII threshold values of native/secondary and secondary/artificial vegetation systems. Our results show that the HII value at the native/secondary vegetation IPs is approximately 22 and globally uniform, whereas it varies regionally for the secondary/artificial vegetation IPs. In a case study of the Liangzhu archaeological site in the lower Yangtze River, discriminant functions for pollen spectra from three vegetation types and pollen–climate transfer functions of the native vegetation were established to reconstruct paleovegetation and paleoclimate over the past 6,600 years. Our study demonstrates this method's feasibility for quantitatively distinguishing human impacts on paleovegetation and assessing quantitative paleoclimate reconstructions using pollen data.

Funder

National Natural Science Foundation of China

Special Project for Basic Research of Yunnan Province-Key Project

Graduate Innovation Grant Program of the Education Department of Hebei Province

Publisher

Oxford University Press (OUP)

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