碳循环
环境科学
生物圈
永久冻土
气候变化
全球变暖
碳纤维
二氧化碳
地球大气中的二氧化碳
温室气体
总有机碳
自行车
固碳
甲烷
全球变化
丰度(生态学)
大气(单位)
水循环
大气碳循环
溶解有机碳
生态学
生态系统
地理
生物
考古
气象学
材料科学
复合数
复合材料
作者
Lars J. Tranvik,John Downing,James B. Cotner,Steven Loiselle,Robert G. Striegl,Thomas J. Ballatore,Peter J. Dillon,Kerri Finlay,Kenneth Fortino,Lesley B. Knoll,Pirkko Kortelainen,Tiit Kutser,Søren E. Larsen,Isabelle Laurion,Dina M. Leech,S. Leigh McCallister,Diane M. McKnight,John M. Mélack,Erin P. Overholt,Jason A. Porter
标识
DOI:10.4319/lo.2009.54.6_part_2.2298
摘要
We explore the role of lakes in carbon cycling and global climate, examine the mechanisms influencing carbon pools and transformations in lakes, and discuss how the metabolism of carbon in the inland waters is likely to change in response to climate. Furthermore, we project changes as global climate change in the abundance and spatial distribution of lakes in the biosphere, and we revise the estimate for the global extent of carbon transformation in inland waters. This synthesis demonstrates that the global annual emissions of carbon dioxide from inland waters to the atmosphere are similar in magnitude to the carbon dioxide uptake by the oceans and that the global burial of organic carbon in inland water sediments exceeds organic carbon sequestration on the ocean floor. The role of inland waters in global carbon cycling and climate forcing may be changed by human activities, including construction of impoundments, which accumulate large amounts of carbon in sediments and emit large amounts of methane to the atmosphere. Methane emissions are also expected from lakes on melting permafrost. The synthesis presented here indicates that (1) inland waters constitute a significant component of the global carbon cycle, (2) their contribution to this cycle has significantly changed as a result of human activities, and (3) they will continue to change in response to future climate change causing decreased as well as increased abundance of lakes as well as increases in the number of aquatic impoundments.
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