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Combining and competing effects between precipitation and temperature on Holocene fire regime evolution inferred from a sedimentary black carbon record in southwestern China

Published online by Cambridge University Press:  24 October 2019

Dongliang Ning ,
Enlou Zhang ,
James Shulmeister ,
Jie Chang ,
Weiwei Sun  and
Zhenyu Ni
Dongliang Ning
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 73 Beijing E Rd, Xuanwu, Nanjing, Jiangsu 210008, China University of Chinese Academy of Sciences, Beijing 100049, China
Enlou Zhang*
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 73 Beijing E Rd, Xuanwu, Nanjing, Jiangsu 210008, China
James Shulmeister
Affiliation:
School of Earth and Environmental Sciences, The University of Queensland, St. Lucia, Brisbane, QLD 4072, Australia
Jie Chang
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 73 Beijing E Rd, Xuanwu, Nanjing, Jiangsu 210008, China School of Earth and Environmental Sciences, The University of Queensland, St. Lucia, Brisbane, QLD 4072, Australia
Weiwei Sun
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 73 Beijing E Rd, Xuanwu, Nanjing, Jiangsu 210008, China
Zhenyu Ni
Affiliation:
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 73 Beijing E Rd, Xuanwu, Nanjing, Jiangsu 210008, China
*
*Corresponding author e-mail address: [email protected] (E. Zhang).
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Abstract

Wildfires are sensitive to climate change, but their response to changes in temperature and precipitation on long timescales is still disputed. In this study, we present a ~9.4 ka black carbon mass sedimentation rate (BCMSR) record from Lake Ximenglongtan (XMLT), southwestern China, to elucidate the Holocene fire regime and its linkages to climatic conditions. The results indicate that the regional fire activity was low during the early Holocene (before 7.6 cal ka BP), increased notably at 7.6 cal ka BP, and continued to increase gradually during the mid- to late Holocene until 2.2 ka. The episodes of higher fire occurrence reflected by higher BCMSR over the last 2.2 ka might be more likely related to the intensified human activities. The cool and humid climate during the early Holocene limited the spread of fire, while warming and drying at ~7.6 cal ka BP triggered higher fire occurrence. Instead of temperature, changes in precipitation dominated fire regime variation during the mid- to late Holocene. On millennial timescales, we suggest that Holocene fire variability has been predominantly controlled by the combined effects of Northern Hemisphere (NH) summer and winter insolation that influenced monsoonal precipitation and fire season temperature, respectively. Indian Ocean Dipole (IOD) events may also have affected fire incidence through influencing monsoon intensity.

Keywords

HoloceneFire regimeInsolationMoisture balanceIndian Ocean MonsoonIndian Ocean Dipole (IOD)
Type
Research Article
Information
Quaternary Research , Volume 93 , January 2020 , pp. 243 - 254
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2019 

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