Refining soil organic carbon stock estimates for China's palustrine wetlands
Palustrine wetlands (PWs) include all bogs, fens, swamps and marshes that are non-saline and which are not lakes or rivers. They therefore form a highly important group of wetlands which hold large carbon stocks. If these wetlands are not protected properly they could become a net carbon source in t...
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Published in | Environmental research letters Vol. 10; no. 12; pp. 124016 - 124025 |
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Main Authors | , , , , , |
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Language | English |
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Abstract | Palustrine wetlands (PWs) include all bogs, fens, swamps and marshes that are non-saline and which are not lakes or rivers. They therefore form a highly important group of wetlands which hold large carbon stocks. If these wetlands are not protected properly they could become a net carbon source in the future. Compilation of spatially explicit wetland databases, national inventory data and in situ measurement of soil organic carbon (SOC) could be useful to better quantify SOC and formulate long-term strategies for mitigating global climate change. In this study, a synergistic mapping approach was used to create a hybrid map for PWs for China and to estimate their SOC content. Total SOC storage in PWs was estimated to be 4.3 1.4 Pg C, with a SOC density of 31.17 ( 10.55) kg C m−2 in the upper 1 m of the soil layer. This carbon stock is concentrated in Northeast China (49%) and the Qinghai-Tibet Plateau (41%). Given the large pool of carbon stored in PWs compared to other soil types, we suggest that urgent monitoring programmes on SOC should be established in regions with very few datasets, but where PWs appear to be common such as the Tibet region and Northwest China. |
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AbstractList | Palustrine wetlands (PWs) include all bogs, fens, swamps and marshes that are non-saline and which are not lakes or rivers. They therefore form a highly important group of wetlands which hold large carbon stocks. If these wetlands are not protected properly they could become a net carbon source in the future. Compilation of spatially explicit wetland databases, national inventory data and in situ measurement of soil organic carbon (SOC) could be useful to better quantify SOC and formulate long-term strategies for mitigating global climate change. In this study, a synergistic mapping approach was used to create a hybrid map for PWs for China and to estimate their SOC content. Total SOC storage in PWs was estimated to be 4.3 ± 1.4 Pg C, with a SOC density of 31.17 (±10.55) kg C m ^−2 in the upper 1 m of the soil layer. This carbon stock is concentrated in Northeast China (49%) and the Qinghai–Tibet Plateau (41%). Given the large pool of carbon stored in PWs compared to other soil types, we suggest that urgent monitoring programmes on SOC should be established in regions with very few datasets, but where PWs appear to be common such as the Tibet region and Northwest China. Palustrine wetlands (PWs) include all bogs, fens, swamps and marshes that are non-saline and which are not lakes or rivers. They therefore form a highly important group of wetlands which hold large carbon stocks. If these wetlands are not protected properly they could become a net carbon source in the future. Compilation of spatially explicit wetland databases, national inventory data and in situ measurement of soil organic carbon (SOC) could be useful to better quantify SOC and formulate long-term strategies for mitigating global climate change. In this study, a synergistic mapping approach was used to create a hybrid map for PWs for China and to estimate their SOC content. Total SOC storage in PWs was estimated to be 4.3 + or - 1.4 Pg C, with a SOC density of 31.17 (+ or -10.55) kg C m super(-2) in the upper 1 m of the soil layer. This carbon stock is concentrated in Northeast China (49%) and the Qinghai-Tibet Plateau (41%). Given the large pool of carbon stored in PWs compared to other soil types, we suggest that urgent monitoring programmes on SOC should be established in regions with very few datasets, but where PWs appear to be common such as the Tibet region and Northwest China. Palustrine wetlands (PWs) include all bogs, fens, swamps and marshes that are non-saline and which are not lakes or rivers. They therefore form a highly important group of wetlands which hold large carbon stocks. If these wetlands are not protected properly they could become a net carbon source in the future. Compilation of spatially explicit wetland databases, national inventory data and in situ measurement of soil organic carbon (SOC) could be useful to better quantify SOC and formulate long-term strategies for mitigating global climate change. In this study, a synergistic mapping approach was used to create a hybrid map for PWs for China and to estimate their SOC content. Total SOC storage in PWs was estimated to be 4.3 1.4 Pg C, with a SOC density of 31.17 ( 10.55) kg C m−2 in the upper 1 m of the soil layer. This carbon stock is concentrated in Northeast China (49%) and the Qinghai-Tibet Plateau (41%). Given the large pool of carbon stored in PWs compared to other soil types, we suggest that urgent monitoring programmes on SOC should be established in regions with very few datasets, but where PWs appear to be common such as the Tibet region and Northwest China. Palustrine wetlands (PWs) include all bogs, fens, swamps and marshes that are non-saline and which are not lakes or rivers. They therefore form a highly important group of wetlands which hold large carbon stocks. If these wetlands are not protected properly they could become a net carbon source in the future. Compilation of spatially explicit wetland databases, national inventory data and in situ measurement of soil organic carbon (SOC) could be useful to better quantify SOC and formulate long-term strategies for mitigating global climate change. In this study, a synergistic mapping approach was used to create a hybrid map for PWs for China and to estimate their SOC content. Total SOC storage in PWs was estimated to be 4.3 ± 1.4 Pg C, with a SOC density of 31.17 (±10.55) kg C m−2 in the upper 1 m of the soil layer. This carbon stock is concentrated in Northeast China (49%) and the Qinghai–Tibet Plateau (41%). Given the large pool of carbon stored in PWs compared to other soil types, we suggest that urgent monitoring programmes on SOC should be established in regions with very few datasets, but where PWs appear to be common such as the Tibet region and Northwest China. |
Author | Zhang, Ying Liu, Junguo Parry, Lauren E Ma, Kun Holden, Joseph Ciais, Philippe |
Author_xml | – sequence: 1 givenname: Kun surname: Ma fullname: Ma, Kun organization: Beijing Forestry University School of Nature Conservation, Qinghua East Road 35, Haidian District, 100083, Beijing, People's Republic of China – sequence: 2 givenname: Junguo surname: Liu fullname: Liu, Junguo email: junguo.liu@gmail.com organization: Beijing Forestry University School of Nature Conservation, Qinghua East Road 35, Haidian District, 100083, Beijing, People's Republic of China – sequence: 3 givenname: Ying surname: Zhang fullname: Zhang, Ying organization: Beijing Forestry University School of Nature Conservation, Qinghua East Road 35, Haidian District, 100083, Beijing, People's Republic of China – sequence: 4 givenname: Lauren E surname: Parry fullname: Parry, Lauren E organization: University of Leeds water@leeds, School of Geography, Leeds, LS2 9JT, UK – sequence: 5 givenname: Joseph surname: Holden fullname: Holden, Joseph organization: University of Leeds water@leeds, School of Geography, Leeds, LS2 9JT, UK – sequence: 6 givenname: Philippe surname: Ciais fullname: Ciais, Philippe organization: Laboratoire des Sciences du Climat et de 1'Environment, CEA-CNRS-UVSQ, F-91191, Gif sur Yvette, France |
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Cites_doi | 10.1038/298156a0 10.1038/nature11461 10.1023/A:1020289403835 10.1007/BF02837371 10.1111/j.1365-2486.2007.01458.x 10.1071/SR09171 10.1007/s10641-013-0152-4 10.1007/s11430-009-0075-2 10.1360/02yd0029 10.2307/1941811 10.1111/j.1747-6593.2010.00233.x 10.1007/s11434-012-5529-9 10.1029/2008gb003327 10.5194/bg-9-235-2012 10.1111/j.1365-2486.2010.02279.x 10.17521/cjpe.2003.0071 10.1007/BF02205586 10.1098/rsta.2005.1671 10.1371/journal.pone.0047814 10.1155/2014/487961 10.1016/j.jhydrol.2004.03.028 10.1029/2001GB001844 10.5194/bg-10-929-2013 10.1038/nature04514 10.1038/nature07944 10.1016/j.jenvman.2006.09.020 10.1007/978-94-011-6003-2 10.1007/BF03161761 10.1016/j.quascirev.2014.06.004 10.1007/13280.1654-7209 10.1073/pnas.1200452109 10.1038/nature04038 10.1016/j.ecoleng.2009.05.004 10.1007/s13157-012-0366-9 10.1016/j.geoderma.2008.06.006 10.1111/j.1365-2486.2009.01976.x |
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Snippet | Palustrine wetlands (PWs) include all bogs, fens, swamps and marshes that are non-saline and which are not lakes or rivers. They therefore form a highly... |
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StartPage | 124016 |
SubjectTerms | Bogs Carbon Carbon sources China Climate change Continental interfaces, environment Ecology, environment ecosystem services Ecosystems Fens In situ measurement Lakes Life Sciences marsh Marshes Organic carbon Organic soils peatland Sciences of the Universe Soil layers Soil types Soils swamp Swamps Wetlands |
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Title | Refining soil organic carbon stock estimates for China's palustrine wetlands |
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