| Literature DB >> 31427733 |
Jian Song1,2, Shiqiang Wan3,4, Shilong Piao5,6,7, Alan K Knapp8,9, Aimée T Classen10,11, Sara Vicca12, Philippe Ciais5,13, Mark J Hovenden14, Sebastian Leuzinger15, Claus Beier16, Paul Kardol17, Jianyang Xia18,19, Qiang Liu5, Jingyi Ru2, Zhenxing Zhou2, Yiqi Luo20, Dali Guo21, J Adam Langley22, Jakob Zscheischler23,24, Jeffrey S Dukes25, Jianwu Tang26, Jiquan Chen27, Kirsten S Hofmockel28,29, Lara M Kueppers30,31, Lindsey Rustad32, Lingli Liu33, Melinda D Smith8,9, Pamela H Templer34, R Quinn Thomas35, Richard J Norby36, Richard P Phillips37, Shuli Niu38, Simone Fatichi39, Yingping Wang40, Pengshuai Shao41, Hongyan Han41, Dandan Wang2, Lingjie Lei2, Jiali Wang2, Xiaona Li2, Qian Zhang2, Xiaoming Li2, Fanglong Su2, Bin Liu2, Fan Yang2, Gaigai Ma2, Guoyong Li2, Yanchun Liu2, Yinzhan Liu2, Zhongling Yang2, Kesheng Zhang2, Yuan Miao2, Mengjun Hu2, Chuang Yan2, Ang Zhang2, Mingxing Zhong2, Yan Hui2, Ying Li2, Mengmei Zheng2.
Abstract
Direct quantification of terrestrial biosphere responses to global change is crucial for projections of future climate change in Earth system models. Here, we synthesized ecosystem carbon-cycling data from 1,119 experiments performed over the past four decades concerning changes in temperature, precipitation, CO2 and nitrogen across major terrestrial vegetation types of the world. Most experiments manipulated single rather than multiple global change drivers in temperate ecosystems of the USA, Europe and China. The magnitudes of warming and elevated CO2 treatments were consistent with the ranges of future projections, whereas those of precipitation changes and nitrogen inputs often exceeded the projected ranges. Increases in global change drivers consistently accelerated, but decreased precipitation slowed down carbon-cycle processes. Nonlinear (including synergistic and antagonistic) effects among global change drivers were rare. Belowground carbon allocation responded negatively to increased precipitation and nitrogen addition and positively to decreased precipitation and elevated CO2. The sensitivities of carbon variables to multiple global change drivers depended on the background climate and ecosystem condition, suggesting that Earth system models should be evaluated using site-specific conditions for best uses of this large dataset. Together, this synthesis underscores an urgent need to explore the interactions among multiple global change drivers in underrepresented regions such as semi-arid ecosystems, forests in the tropics and subtropics, and Arctic tundra when forecasting future terrestrial carbon-climate feedback.Entities:
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Year: 2019 PMID: 31427733 DOI: 10.1038/s41559-019-0958-3
Source DB: PubMed Journal: Nat Ecol Evol ISSN: 2397-334X Impact factor: 15.460