Post-drainage vegetation, microtopography and organic matter in Arctic drained lake basins

被引:4
作者
Wolter, Juliane [1 ,2 ]
Jones, Benjamin M. [3 ]
Fuchs, Matthias [4 ]
Breen, Amy [5 ]
Bussmann, Ingeborg [6 ,7 ]
Koch, Boris [8 ]
Lenz, Josefine [2 ]
Myers-Smith, Isla H. [9 ]
Sachs, Torsten [10 ]
Strauss, Jens [2 ]
Nitze, Ingmar [2 ]
Grosse, Guido [2 ,11 ]
机构
[1] Univ Potsdam, Inst Biochem & Biol, Potsdam, Germany
[2] Alfred Wegener Inst Helmholtz Ctr Polar & Marine R, Sect Permafrost Res, Potsdam, Germany
[3] Univ Alaska Fairbanks, Inst Northern Engn, Fairbanks, AK USA
[4] Univ Colorado, Renewable & Sustainable Energy Inst, Boulder, CO USA
[5] Univ Alaska Fairbanks, Int Arctic Res Ctr, Fairbanks, AK 99701 USA
[6] Alfred Wegener Inst Helmholtz Ctr Polar & Marine R, Sect Shelf Sea Syst Ecol, Helgoland, Germany
[7] Alfred Wegener Inst Helmholtz Ctr Polar & Marine R, Sect Marine Geochem, Bremerhaven, Germany
[8] Alfred Wegener Inst Helmholtz Ctr Polar & Marine R, Sect Ecol Chem, Bremerhaven, Germany
[9] Univ Edinburgh, Sch Geosci, Edinburgh, Scotland
[10] GFZ German Res Ctr Geosci, Sect Remote Sensing & Geoinformat, Potsdam, Germany
[11] Univ Potsdam, Inst Geosci, Potsdam, Germany
基金
美国国家科学基金会;
关键词
tundra vegetation; methane; carbon; nitrogen; remote sensing; machine learning; Teshekpuk lake observatory; METHANE EMISSIONS; CARBON-DIOXIDE; COASTAL-PLAIN; PERMAFROST; TUNDRA; THERMOKARST; THAW; ICE; PENINSULA; BARROW;
D O I
10.1088/1748-9326/ad2eeb
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Wetlands in Arctic drained lake basins (DLBs) have a high potential for carbon storage in vegetation and peat as well as for elevated greenhouse gas emissions. However, the evolution of vegetation and organic matter is rarely studied in DLBs, making these abundant wetlands especially uncertain elements of the permafrost carbon budget. We surveyed multiple DLB generations in northern Alaska with the goal to assess vegetation, microtopography, and organic matter in surface sediment and pond water in DLBs and to provide the first high-resolution land cover classification for a DLB system focussing on moisture-related vegetation classes for the Teshekpuk Lake region. We associated sediment properties and methane concentrations along a post-drainage succession gradient with remote sensing-derived land cover classes. Our study distinguished five eco-hydrological classes using statistical clustering of vegetation data, which corresponded to the land cover classes. We identified surface wetness and time since drainage as predictors of vegetation composition. Microtopographic complexity increased after drainage. Organic carbon and nitrogen contents in sediment, and dissolved organic carbon (DOC) and dissolved nitrogen (DN) in ponds were high throughout, indicating high organic matter availability and decomposition. We confirmed wetness as a predictor of sediment methane concentrations. Our findings suggest moderate to high methane concentrations independent of drainage age, with particularly high concentrations beneath submerged patches (up to 200 mu mol l-1) and in pond water (up to 22 mu mol l-1). In our DLB system, wet and shallow submerged patches with high methane concentrations occupied 54% of the area, and ponds with high DOC, DN and methane occupied another 11%. In conclusion, we demonstrate that DLB wetlands are highly productive regarding organic matter decomposition and methane production. Machine learning-aided land cover classification using high-resolution multispectral satellite imagery provides a useful tool for future upscaling of sediment properties and methane emission potentials from Arctic DLBs.
引用
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页数:12
相关论文
共 74 条
[1]   Rising plant-mediated methane emissions from arctic wetlands [J].
Andresen, Christian G. ;
Lara, Mark J. ;
Tweedie, Craig E. ;
Lougheed, Vanessa L. .
GLOBAL CHANGE BIOLOGY, 2017, 23 (03) :1128-1139
[2]   VEGETATIONAL CHANGE AND ICE-WEDGE POLYGONS THROUGH THE THAW-LAKE CYCLE IN ARCTIC ALASKA [J].
BILLINGS, WD ;
PETERSON, KM .
ARCTIC AND ALPINE RESEARCH, 1980, 12 (04) :413-432
[3]   Soil organic carbon storage and distribution in Arctic Tundra, Barrow, Alaska [J].
Bockheim, JG ;
Everett, LR ;
Hinkel, KM ;
Nelson, FE ;
Brown, J .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1999, 63 (04) :934-940
[4]   Methane dynamics in three different Siberian water bodies under winter and summer conditions [J].
Bussmann, Ingeborg ;
Fedorova, Irina ;
Juhls, Bennet ;
Overduin, Pier Paul ;
Winkel, Matthias .
BIOGEOSCIENCES, 2021, 18 (06) :2047-2061
[5]   Vegetation Type Dominates the Spatial Variability in CH4 Emissions Across Multiple Arctic Tundra Landscapes [J].
Davidson, Scott J. ;
Sloan, Victoria L. ;
Phoenix, Gareth K. ;
Wagner, Robert ;
Fisher, James P. ;
Oechel, Walter C. ;
Zona, Donatella .
ECOSYSTEMS, 2016, 19 (06) :1116-1132
[6]   How does spatial heterogeneity affect inter- and intraspecific growth patterns in tundra shrubs? [J].
Dobbert, Svenja ;
Pape, Roland ;
Loeffler, Jorg .
JOURNAL OF ECOLOGY, 2021, 109 (12) :4115-4131
[7]   The evolution of a thermokarst-lake landscape: Late Quaternary permafrost degradation and stabilization in interior Alaska [J].
Edwards, Mary ;
Grosse, Guido ;
Jones, Benjamin M. ;
McDowell, Patricia .
SEDIMENTARY GEOLOGY, 2016, 340 :3-14
[8]   Remote sensing northern lake methane ebullition [J].
Engram, M. ;
Anthony, K. M. Walter ;
Sachs, T. ;
Kohnert, K. ;
Serafimovich, A. ;
Grosse, G. ;
Meyer, F. J. .
NATURE CLIMATE CHANGE, 2020, 10 (06) :511-+
[9]  
French H.M., 2017, PERIGLACIAL ENV, V4th
[10]   Holocene ice-wedge polygon development in northern Yukon permafrost peatlands (Canada) [J].
Fritz, Michael ;
Wolter, Juliane ;
Rudaya, Natalia ;
Palagushkina, Olga ;
Nazarova, Larisa ;
Obu, Jaroslav ;
Rethemeyer, Janet ;
Lantuit, Hugues ;
Wetterich, Sebastian .
QUATERNARY SCIENCE REVIEWS, 2016, 147 :279-297