globalchange  > 气候减缓与适应
DOI: 10.1007/s10533-016-0252-2
Scopus记录号: 2-s2.0-84991109088
论文题名:
Biogeochemistry of “pristine” freshwater stream and lake systems in the western Canadian Arctic
作者: Dean J.F.; Billett M.F.; Baxter R.; Dinsmore K.J.; Lessels J.S.; Street L.E.; Subke J.-A.; Tetzlaff D.; Washbourne I.; Wookey P.A.
刊名: Biogeochemistry
ISSN: 0168-2563
EISSN: 1573-515X
出版年: 2016
卷: 130, 期:3
起始页码: 191
结束页码: 213
语种: 英语
英文关键词: Arctic catchments ; Baseline study ; Climate change ; Freshwater biogeochemistry ; Inland waters ; Permafrost thaw ; Pristine environment
Scopus关键词: air temperature ; baseline survey ; biogeochemistry ; carbon dioxide ; catchment ; climate change ; freeze-thaw cycle ; freshwater ecosystem ; headwater ; methane ; permafrost ; pristine environment ; warming ; Canada ; Canadian Arctic
英文摘要: Climate change poses a substantial threat to the stability of the Arctic terrestrial carbon (C) pool as warmer air temperatures thaw permafrost and deepen the seasonally-thawed active layer of soils and sediments. Enhanced water flow through this layer may accelerate the transport of C and major cations and anions to streams and lakes. These act as important conduits and reactors for dissolved C within the terrestrial C cycle. It is important for studies to consider these processes in small headwater catchments, which have been identified as hotspots of rapid mineralisation of C sourced from ancient permafrost thaw. In order to better understand the role of inland waters in terrestrial C cycling we characterised the biogeochemistry of the freshwater systems in a c. 14�km2 study area in the western Canadian Arctic. Sampling took place during the snow-free seasons of 2013 and 2014 for major inorganic solutes, dissolved organic and inorganic C (DOC and DIC, respectively), carbon dioxide (CO2) and methane (CH4) concentrations from three water type groups: lakes, polygonal pools and streams. These groups displayed differing biogeochemical signatures, indicative of contrasting biogeochemical controls. However, none of the groups showed strong signals of enhanced permafrost thaw during the study seasons. The mean annual air temperature in the region has increased by more than 2.5��C since 1970, and continued warming will likely affect the aquatic biogeochemistry. This study provides important baseline data for comparison with future studies in a warming Arctic. � 2016, The Author(s).
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/83346
Appears in Collections:气候减缓与适应
气候变化事实与影响

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作者单位: Biological and Environment Sciences, Faculty of Natural Sciences, University of Stirling, Stirling, United Kingdom; Earth and Climate Cluster, Faculty of Earth and Life Sciences, Vrije Universiteit Amsterdam, De Boelelaan 1085, Amsterdam, Netherlands; School of Biological and Biomedical Sciences, University of Durham, Durham, United Kingdom; Centre for Ecology and Hydrology, Bush Estate, Penicuik, United Kingdom; Northern Rivers Institute, School of Geosciences, University of Aberdeen, Aberdeen, United Kingdom; Environmental Sciences, School of Life Sciences, Heriot-Watt University, Edinburgh, United Kingdom; School of Geosciences, University of Edinburgh, Crew Building, Alexander Crum Brown Road, Edinburgh, United Kingdom

Recommended Citation:
Dean J.F.,Billett M.F.,Baxter R.,et al. Biogeochemistry of “pristine” freshwater stream and lake systems in the western Canadian Arctic[J]. Biogeochemistry,2016-01-01,130(3)
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