作者
Anthony P Walker, Martin G De Kauwe, Ana Bastos, Soumaya Belmecheri, Katerina Georgiou, Ralph Keeling, Sean M McMahon, Belinda E Medlyn, David JP Moore, Richard J Norby, Sönke Zaehle, Kristina J Anderson‐Teixeira, Giovanna Battipaglia, Roel JW Brienen, Kristine G Cabugao, Maxime Cailleret, Elliott Campbell, Josep Canadell, Philippe Ciais, Matthew E Craig, David Ellsworth, Graham Farquhar, Simone Fatichi, Joshua B Fisher, David Frank, Heather Graven, Lianhong Gu, Vanessa Haverd, Kelly Heilman, Martin Heimann, Bruce A Hungate, Colleen M Iversen, Fortunat Joos, Mingkai Jiang, Trevor F Keenan, Jürgen Knauer, Christian Körner, Victor O Leshyk, Sebastian Leuzinger, Yao Liu, Natasha MacBean, Yadvinder Malhi, Tim McVicar, Josep Penuelas, Julia Pongratz, A Shafer Powell, Terhi Riutta, Manon EB Sabot, Juergen Schleucher, Stephen Sitch, William K Smith, Benjamin Sulman, Benton Taylor, César Terrer, Margaret S Torn, Kathleen Treseder, Trugman
发表日期
2021
期刊
New Phytologist
卷号
229
期号
5
页码范围
2413-2445
出版商
Wiley
简介
Atmospheric carbon dioxide concentration ([CO2]) is increasing, which increases leaf‐scale photosynthesis and intrinsic water‐use efficiency. These direct responses have the potential to increase plant growth, vegetation biomass, and soil organic matter; transferring carbon from the atmosphere into terrestrial ecosystems (a carbon sink). A substantial global terrestrial carbon sink would slow the rate of [CO2] increase and thus climate change. However, ecosystem CO2 responses are complex or confounded by concurrent changes in multiple agents of global change and evidence for a [CO2]‐driven terrestrial carbon sink can appear contradictory. Here we synthesize theory and broad, multidisciplinary evidence for the effects of increasing [CO2] (iCO2) on the global terrestrial carbon sink. Evidence suggests a substantial increase in global photosynthesis since pre‐industrial times. Established theory, supported by …
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