Keys to the global treeline formation: Thermal limit for its position and moisture for the taxon-specific variation
Abstract
Alpine treeline is a prominent biogeographic feature worldwide, determined by the physiological limit of tree life form. There are considerable variations in the various dimensions of physiological limit among tree taxa; thus, varied environmental drivers and spatial patterns are expected for different tree taxa at treelines. However, such taxonomic variability of treeline is often overlooked in large-scale studies. Here, we assembled, to our knowledge, the most comprehensive dataset of tree species at alpine treelines, drawing from research conducted over the past half-century, encompassing over 2,000 records across 38 mountain regions and 43 countries. Using this extensive global dataset, we examined the spatial patterns and environmental drivers shaping different tree taxa at treelines worldwide. The highest tree richness at treelines was found in mid-latitude mountains of the Northern Hemisphere, reflecting floristic differentiation caused by continental isolation. Moisture and climatic variability, particularly seasonal fluctuations, determine the turnover of tree taxa at treelines. Heat limitations appear to restrict the establishment of all genera, effectively defining treeline positions. Heat conditions at treeline positions tend to be about 35% below the genus- and species- level thermal optima. This thermal threshold can effectively explain the global pattern of uppermost tree elevation. Our findings highlight the synergic effects between heat and moisture in determining the taxonomic variation in treeline formation, offering insights for alpine treeline studies under climate change.
Article Details
Journal Info
Proceedings of the National Academy of Sciences
National Academy of Sciences
Authors (10)
Yuyang Xie
Institute of Ecology, College of Urban and Environmental Sciences and Key Laboratory for Earth Surface Processes of Ministry of Education, Peking University
Zehao Shen
Institute of Ecology, College of Urban and Environmental Sciences and Key Laboratory for Earth Surface Processes of Ministry of Education, Peking University
J. Julio Camarero
Instituto Pirenaico de Ecología, Consejo Superior de Investigaciones Científicas
Josep Peñuelas
Xuejing Wang
Institute of Ecology, College of Urban and Environmental Sciences and Key Laboratory for Earth Surface Processes of Ministry of Education, Peking University
Jitang Li
Institute of Ecology, College of Urban and Environmental Sciences and Key Laboratory for Earth Surface Processes of Ministry of Education, Peking University
Wenge Rao
Institute of Ecology, College of Urban and Environmental Sciences and Key Laboratory for Earth Surface Processes of Ministry of Education, Peking University
Xiangwu Chen
Institute of Ecology, College of Urban and Environmental Sciences and Key Laboratory for Earth Surface Processes of Ministry of Education, Peking University
Fu Zhao
Institute of Ecology, College of Urban and Environmental Sciences and Key Laboratory for Earth Surface Processes of Ministry of Education, Peking University
Xiao Feng
Frontiers Science Center for High Energy Material, Advanced Technology Research Institute (Jinan), Key Laboratory of Cluster Science (Ministry of Education), Beijing Key Laboratory of Intelligent Molecular Materials and High-Throughput Manufacturing, School of Interdisciplinary Science, School of Chemistry and Chemical Engineering