The organic carbon storage in Chinese lake sediments during the Holocene Megathermal
Zhang Fengju1, Xue Bin2, Yao Shuchun2
1. School of Geography, Geomatics, and Planning, Jiangsu Normal University, Xuzhou 221116, Jiangsu;
2. State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, Jiangsu
As an important component of the terrestrial ecosystem, lakes play an important role in the global and regional carbon cycle. Understanding and reconstructing the carbon storage in lake sediments during the Holocene Megathermal(6±0.5 ka B.P.) can contribute to the assessment of the lake carbon sequestration potential in the near future. In this study, 65 lakes with total organic carbon content(TOC) and reliable chronology of the Holocene Megathermal were chosen to determine the total carbon storage in Chinese lakes at that time period. The results showed that the carbon storage in Chinese lakes was estimated to be 4.56 Pg C(varying from 0.90 Pg C to 19.08 Pg C) (1 Pg=1015 g) during the Holocene Megathermal. The carbon stock was mainly concentrated in Eastern Plain Lake Region, Inner Mongolian-Xinjiang Lake Region and Tibet Plateau Lake Region. The average organic carbon accumulation rate(OCAR) in Chinese lakes ranged between 4.4 g/(m2·a) and 92.6 g/(m2·a), with a mean of 22.3 g/(m2·a) during the Holocene Megathermal. The Inner Mongolian-Xinjiang Lake Region had the highest OCAR, while the Tibet Plateau Lake Region had the lowest value. Furthermore, the carbon storage in Chinese lakes during the Holocene Megathermal was about 3%of that buried by terrestrial ecosystem, but in only 2%of the area. In particular, lake sediments can be preserved for quite longer times than forest biomass and soil, thus it is reasonable to conclude that lakes play a significant role in maintaining the global carbon balance and their carbon sink functions should be taken into consideration in the future.
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Zhang Fengju, Xue Bin, Yao Shuchun. The organic carbon storage in Chinese lake sediments during the Holocene Megathermal. Quaternary Sciences, 2018, 38(4): 887-899.
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2018, Vol. 38 
