【作者单位】Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Qinghai Provincial Key Laboratory of Restoration Ecology of Cold Area, Xining, China;University of the Chinese Academy of Sciences, Beijing, China;Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Qinghai Provincial Key Laboratory of Restoration Ecology of Cold Area, Xining, China;University of the Chinese Academy of Sciences, Beijing, China;Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;CAS Center for Excellence in Tibetan Plateau Earth Science, Chinese Academy of Sciences, Beijing, China;Naqu Integrated Observation and Research Station of Ecology and Environment, Institute of Tibetan Plateau Research, Tibet University, Chinese Academy of Sciences, Lasa, China;Shiping Wang;and;Yanfen Wang;Binhai Research Institute in Tianjin, Tianjin, China;Aarhus Institute of Advanced Studies, Aarhus University, Aarhus C, Denmark;Chicago Botanic Garden, Glencoe, Illinois;Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;CAS Center for Excellence in Tibetan Plateau Earth Science, Chinese Academy of Sciences, Beijing, China;Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Qinghai Provincial Key Laboratory of Restoration Ecology of Cold Area, Xining, China;Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;University of the Chinese Academy of Sciences, Beijing, China;Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;University of the Chinese Academy of Sciences, Beijing, China;Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;University of the Chinese Academy of Sciences, Beijing, China;Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;The University of Chicago Medicine and Biological Sciences Division, Chicago, Illinois;Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Qinghai Provincial Key Laboratory of Restoration Ecology of Cold Area, Xining, China;Institute for Agro‐Environmental Sciences, National Agriculture and Food Research Organization, Tsukuba, Japan;Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Qinghai Provincial Key Laboratory of Restoration Ecology of Cold Area, Xining, China;Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Qinghai Provincial Key Laboratory of Restoration Ecology of Cold Area, Xining, China;CAS Center for Excellence in Tibetan Plateau Earth Science, Chinese Academy of Sciences, Beijing, China;Shiping Wang;and;Yanfen Wang
【关键词】alpine meadows biodiversity climate change experiment elevation gradient reciprocal transplant species gain species loss
【摘要】 Experimental warming in situ suggests that warming could lead to a loss of biodiversity. However, species that remain in situ and experience climate change will interact with species tracking climate change, which could also affect patterns of biodiv...
