| Literature DB >> 30166491 |
Connor Nolan1, Jonathan T Overpeck2,1, Judy R M Allen3, Patricia M Anderson4, Julio L Betancourt5, Heather A Binney6, Simon Brewer7, Mark B Bush8, Brian M Chase9, Rachid Cheddadi9, Morteza Djamali10, John Dodson11,12, Mary E Edwards6,13, William D Gosling14,15, Simon Haberle16, Sara C Hotchkiss17, Brian Huntley3, Sarah J Ivory18, A Peter Kershaw19, Soo-Hyun Kim17, Claudio Latorre20, Michelle Leydet10, Anne-Marie Lézine21, Kam-Biu Liu22, Yao Liu23, A V Lozhkin24, Matt S McGlone25, Robert A Marchant26, Arata Momohara27, Patricio I Moreno28, Stefanie Müller29, Bette L Otto-Bliesner30, Caiming Shen31, Janelle Stevenson32, Hikaru Takahara33, Pavel E Tarasov29, John Tipton34, Annie Vincens35, Chengyu Weng36, Qinghai Xu37, Zhuo Zheng38, Stephen T Jackson39,1.
Abstract
Impacts of global climate change on terrestrial ecosystems are imperfectly constrained by ecosystem models and direct observations. Pervasive ecosystem transformations occurred in response to warming and associated climatic changes during the last glacial-to-interglacial transition, which was comparable in magnitude to warming projected for the next century under high-emission scenarios. We reviewed 594 published paleoecological records to examine compositional and structural changes in terrestrial vegetation since the last glacial period and to project the magnitudes of ecosystem transformations under alternative future emission scenarios. Our results indicate that terrestrial ecosystems are highly sensitive to temperature change and suggest that, without major reductions in greenhouse gas emissions to the atmosphere, terrestrial ecosystems worldwide are at risk of major transformation, with accompanying disruption of ecosystem services and impacts on biodiversity.Mesh:
Year: 2018 PMID: 30166491 DOI: 10.1126/science.aan5360
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728