| Literature DB >> 32409476 |
Florian Zellweger1,2, Pieter De Frenne3, Jonathan Lenoir4, Pieter Vangansbeke3, Kris Verheyen3, Markus Bernhardt-Römermann5, Lander Baeten3, Radim Hédl6,7, Imre Berki8, Jörg Brunet9, Hans Van Calster10, Markéta Chudomelová6, Guillaume Decocq4, Thomas Dirnböck11, Tomasz Durak12, Thilo Heinken13, Bogdan Jaroszewicz14, Martin Kopecký15,16, František Máliš17,18, Martin Macek15, Marek Malicki19, Tobias Naaf20, Thomas A Nagel21, Adrienne Ortmann-Ajkai22, Petr Petřík15, Remigiusz Pielech23, Kamila Reczyńska19, Wolfgang Schmidt24, Tibor Standovár25, Krzysztof Świerkosz26, Balázs Teleki27, Ondřej Vild6, Monika Wulf20, David Coomes1.
Abstract
Climate warming is causing a shift in biological communities in favor of warm-affinity species (i.e., thermophilization). Species responses often lag behind climate warming, but the reasons for such lags remain largely unknown. Here, we analyzed multidecadal understory microclimate dynamics in European forests and show that thermophilization and the climatic lag in forest plant communities are primarily controlled by microclimate. Increasing tree canopy cover reduces warming rates inside forests, but loss of canopy cover leads to increased local heat that exacerbates the disequilibrium between community responses and climate change. Reciprocal effects between plants and microclimates are key to understanding the response of forest biodiversity and functioning to climate and land-use changes.Mesh:
Year: 2020 PMID: 32409476 DOI: 10.1126/science.aba6880
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728