Global acceleration in rates of vegetation change over the past 18,000 years

Author:

Mottl Ondřej1ORCID,Flantua Suzette G. A.12ORCID,Bhatta Kuber P.1ORCID,Felde Vivian A.12ORCID,Giesecke Thomas3ORCID,Goring Simon45ORCID,Grimm Eric C.6,Haberle Simon78ORCID,Hooghiemstra Henry9,Ivory Sarah10ORCID,Kuneš Petr11ORCID,Wolters Steffen12ORCID,Seddon Alistair W. R.12ORCID,Williams John W.45ORCID

Affiliation:

1. Department of Biological Sciences, University of Bergen, N-5020 Bergen, Norway.

2. Bjerknes Centre for Climate Research, University of Bergen, N-5020 Bergen, Norway.

3. Department of Physical Geography, Utrecht University, 3508 TC, Utrecht, Netherlands.

4. Department of Geography, University of Wisconsin-Madison, Madison, WI, USA.

5. Center for Climatic Research, University of Wisconsin-Madison, Madison, WI, USA.

6. Department of Earth and Environmental Sciences, University of Minnesota, Minneapolis, MN, USA.

7. Department of Archaeology and Natural History, Australian National University, Canberra, ACT 2601, Australia.

8. Australian Research Council Centre of Excellence in Australian Biodiversity and Heritage, Australian National University, Canberra, ACT 2601, Australia.

9. Department of Ecosystem and Landscape Dynamics, University of Amsterdam, 1098 XH, Amsterdam, Netherlands.

10. Department of Geosciences and the Earth and Environmental Systems Institute (EESI), Penn State University, University Park, PA, USA.

11. Department of Botany, Faculty of Science, Charles University, Prague, Czech Republic.

12. Lower Saxony Institute for Historical Coastal Research, Wilhelmshaven, Germany.

Abstract

The pace of Holocene vegetation change Although much is known about the rapid environmental changes that have occurred since the Industrial Revolution, the patterns of change over the preceding millennia have been only patchily understood. Using a global set of >1100 fossil pollen records, Mottl et al. explored the rates of vegetation change over the past 18,000 years (see the Perspective by Overpeck and Breshears). The authors show that the rates of change accelerated markedly during the Late Holocene (∼4.6 to 2.9 thousand years ago), even more rapidly than the climate-driven vegetation changes associated with the end of the last glacial period. In addition, the Late Holocene acceleration began for terrestrial communities as a whole, suggesting that the acceleration in turnover over the past two centuries is the tip of a deeper trend. Science , abg1685, this issue p. 860 ; see also abi9902, p. 786

Funder

National Science Foundation

H2020 European Research Council

Belmont Forum

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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