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Differentiating moss from higher plants is critical in studying the carbon cycle of the boreal biome.
Yuan, Wenping; Liu, Shuguang; Dong, Wenjie; Liang, Shunlin; Zhao, Shuqing; Chen, Jingming; Xu, Wenfang; Li, Xianglan; Barr, Alan; Andrew Black, T; Yan, Wende; Goulden, Mike L; Kulmala, Liisa; Lindroth, Anders; Margolis, Hank A; Matsuura, Yojiro; Moors, Eddy; van der Molen, Michiel; Ohta, Takeshi; Pilegaard, Kim; Varlagin, Andrej; Vesala, Timo.
Afiliação
  • Yuan W; 1] State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875/Zhuhai 519087, China [2] State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, Gans
  • Liu S; 1] U.S. Geological Survey, Earth Resources Observation and Science Center, Sioux Falls, South Dakota 57198, USA [2].
  • Dong W; 1] State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875/Zhuhai 519087, China [2].
  • Liang S; 1] State Key Laboratory of Remote Sensing Science, Jointly Sponsored by Beijing Normal University and Institute of Remote Sensing Applications, Chinese Academy of Sciences, College of Global Change and Earth System Science, Beijing 100875, China [2] Department of Geography, University of Maryland, C
  • Zhao S; College of Urban and Environmental Sciences, Peking University, Beijing 100871, China.
  • Chen J; Department of Geography, University of Toronto, Toronto, Ontario, Canada M5S 3G3.
  • Xu W; State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875/Zhuhai 519087, China.
  • Li X; State Key Laboratory of Remote Sensing Science, Jointly Sponsored by Beijing Normal University and Institute of Remote Sensing Applications, Chinese Academy of Sciences, College of Global Change and Earth System Science, Beijing 100875, China.
  • Barr A; Climate Research Division, Environment Canada, Saskatoon, Saskatchewan, Canada S7N 3H5.
  • Andrew Black T; University of British Columbia, Vancouver, British Columbia, Canada V6T 1Z4.
  • Yan W; State Engineering Laboratory of Southern Forestry Applied Ecology and Technology, Central South University of Forestry and Technology, Changsha, Hunan 410004, China.
  • Goulden ML; Department of Earth System Science, University of California, Irvine, California 92697-3100, USA.
  • Kulmala L; Department of Forest Sciences, P.O. Box 27, FI-00014 University of Helsinki, Finland.
  • Lindroth A; Department of Earth and Ecosystem Sciences, Lund University, Sölvegatan 12 223 62, Sweden.
  • Margolis HA; Centre d'Étude de la Forêt, Faculté de foresterie, de géographie et de géomatique, Université Laval, Québec, Canada G1V 0A6.
  • Matsuura Y; International Forest Informatics Laboratory, Forestry and Forest Products Research Institute, Ibaraki 305-8687, Japan.
  • Moors E; Wageningen UR, Alterra, Earth System Science and Climate Change Group, PO Box 47, 6700 AA Wageningen, The Netherlands.
  • van der Molen M; Department of Hydrology and Geo-Environmental Sciences, Vrije Universiteit Amsterdam, 1081 HV Amsterdam, The Netherlands.
  • Ohta T; Graduate School of Bioagricultural Sciences, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8601, Japan.
  • Pilegaard K; Department of Chemical and Biochemical Engineering, Technical University of Denmark, DK-2800 Kongens Lyngby, Denmark.
  • Varlagin A; Sukachev Laboratory of Biocenology, Severtsov Institute of Ecology and Evolution RAS, Leninsky pr.33, Moscow 119071, Russia.
  • Vesala T; Department of Physics, P.O. Box 48, FI-00014, University of Helsinki, Finland.
Nat Commun ; 5: 4270, 2014 Jun 26.
Article em En | MEDLINE | ID: mdl-24967601
ABSTRACT
The satellite-derived normalized difference vegetation index (NDVI), which is used for estimating gross primary production (GPP), often includes contributions from both mosses and vascular plants in boreal ecosystems. For the same NDVI, moss can generate only about one-third of the GPP that vascular plants can because of its much lower photosynthetic capacity. Here, based on eddy covariance measurements, we show that the difference in photosynthetic capacity between these two plant functional types has never been explicitly included when estimating regional GPP in the boreal region, resulting in a substantial overestimation. The magnitude of this overestimation could have important implications regarding a change from a current carbon sink to a carbon source in the boreal region. Moss abundance, associated with ecosystem disturbances, needs to be mapped and incorporated into GPP estimates in order to adequately assess the role of the boreal region in the global carbon cycle.
Assuntos

Texto completo: 1 Base de dados: MEDLINE Assunto principal: Fotossíntese / Ecossistema / Briófitas / Ciclo do Carbono / Taiga Idioma: En Ano de publicação: 2014 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Assunto principal: Fotossíntese / Ecossistema / Briófitas / Ciclo do Carbono / Taiga Idioma: En Ano de publicação: 2014 Tipo de documento: Article