Carbon accumulation and sequestration of lakes in China during the Holocene

Mei Wang; Huai Chen; Zicheng Yu; Jianghua Wu; Qiu'an Zhu; Changhui Peng; Yanfen Wang; Boqiang Qin

doi:10.1111/gcb.13055

Carbon accumulation and sequestration of lakes in China during the Holocene

Glob Chang Biol. 2015 Dec;21(12):4436-48. doi: 10.1111/gcb.13055.

Authors

Mei Wang^{1

2}, Huai Chen^{1

3}, Zicheng Yu⁴, Jianghua Wu², Qiu'an Zhu⁵, Changhui Peng^{5

6}, Yanfen Wang⁷, Boqiang Qin⁸

Affiliations

¹ Key Laboratory of Mountain Ecological Restoration and Bioresource Utilization & Ecological Restoration Biodiversity Conservation, Key Laboratory of Sichuan Province, Chengdu Institute of Biology, Chinese Academy of Sciences, Chengdu, 610041, China.
² Sustainable Resource Management, Memorial University of Newfoundland, Corner Brook, NL, A2H 6P9, Canada.
³ Zoige Peatland and Global Change Research Station, Chinese Academy of Sciences, Hongyuan, 624400, China.
⁴ Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, PA, 18015, USA.
⁵ Laboratory for Ecological Forecasting and Global Change, College of Forestry, Northwest Agriculture and Forest University, Yangling, 712100, China.
⁶ Institute of Environment Sciences, Department of Biology Science, University of Quebec at Montreal, Montreal, C3H 3P8, Canada.
⁷ College of Life Science, University of Chinese Academy of Sciences, Beijing, 100049, China.
⁸ Nanjin Institute of Geography & Limnology, Chinese Academy of Sciences, Nanjing, 210008, China.

PMID: 26220607
DOI: 10.1111/gcb.13055

Abstract

Understanding the responses of lake systems to past climate change and human activity is critical for assessing and predicting the fate of lake carbon (C) in the future. In this study, we synthesized records of the sediment accumulation from 82 lakes and of C sequestration from 58 lakes with direct organic C measurements throughout China. We also identified the controlling factors of the long-term sediment and C accumulation dynamics in these lakes during the past 12 ka (1 ka = 1000 cal yr BP). Our results indicated an overall increasing trend of sediment and C accumulation since 12 ka, with an accumulation peak in the last couple of millennia for lakes in China, corresponding to terrestrial organic matter input due to land-use change. The Holocene lake sediment accumulation rate (SAR) and C accumulation rate (CAR) averaged (mean ± SE) 0.47 ± 0.05 mm yr(-1) and 7.7 ± 1.4 g C m(-2) yr(-1) in China, respectively, comparable to the previous estimates for boreal and temperate regions. The SAR for lakes in the East Plain of subtropical China (1.05 ± 0.28 mm yr(-1) ) was higher than those in other regions (P < 0.05). However, CAR did not vary significantly among regions. Overall, the variability and history of climate and anthropogenic interference regulated the temporal and spatial dynamics of sediment and C sequestration for lakes in China. We estimated the total amount of C burial in lakes of China as 8.0 ± 1.0 Pg C. This first estimation of total C storage and dynamics in lakes of China confirms the importance of lakes in land C budget in monsoon-influenced regions.

Keywords: aquatic ecosystems; carbon stock; climate change; global carbon cycle; human activities.

Publication types

Research Support, Non-U.S. Gov't

MeSH terms

Carbon / analysis*
Carbon Sequestration*
China
Climate
Climate Change*
Geologic Sediments / analysis*
Lakes / analysis*
Time Factors

Substances

Carbon