As the last ice age came to an end and the planet warmed, the Earth's vegetation changed dramatically, reports a University of Arizona-led international research team.
The current warming from climate change may drive an equally dramatic change in vegetation within the next 100 to 150 years unless greenhouse-gas emissions are reduced, the team wrote.
"We found that ecosystems all over the globe experienced big changes," said Connor Nolan, a doctoral candidate in the UA Department of Geosciences. "About 70 percent of those sites experienced large changes in the species that were there and what the vegetation looked like."
The researchers used their analysis of how vegetation changed after the last ice age to project how much current ecosystems could change in the 21st century and beyond as global warming progresses.
The analysis required synthesizing information from published reports for 594 sites covering every continent except Antarctica. Nolan said the study is the most comprehensive compilation of vegetation and other ecological data covering the period from the height of the last ice age 21,000 years ago to the pre-industrial era.
The regions of the world that had the biggest temperature increases since the ice age also had the greatest changes in vegetation, the team found.
Knowing the relationship between temperature change and the degree of vegetation change allowed the researchers to determine how ecosystems might change under various greenhouse-gas emissions models.
"We used the results from the past to look at the risk of future ecosystem change," Nolan said. "We find that as temperatures rise there are bigger and bigger risks for more ecosystem change."
The Earth warmed 7-13 degrees F (4-7 degrees C) since the last ice age. Climate change projections indicate the world will warm about that much "in the next 100-150 years if greenhouse-gas emissions are not reduced substantially," the authors write.
Corresponding author Stephen Jackson, director of the U.S. Geological Survey's Southwest Climate Adaptation Science Center, said, "Under the business-as-usual scenario of greenhouse-gas emissions there's a very high likelihood of large changes across all the vegetated continents."
The changes would threaten global biodiversity and derail vital services that nature provides to humanity, such as water security, carbon storage and recreation, according to study co-author Jonathan Overpeck, dean of the School for Environment and Sustainability at the University of Michigan.
"If we allow climate change to go unchecked, the vegetation of this planet is going to look completely different than it does today, and that means a huge risk to the diversity of the planet," Overpeck said.
The team's paper, "Past and future global transformation of terrestrial ecosystems under climate change," is scheduled for publication in the August 31 issue of the journal Science. A list of the 42 authors is at the end of this release.
The National Science Foundation, the U.S. Department of the Interior Southwest Climate Adaptation Science Center, the Russian Academy of Sciences and the Russian Foundation for Fundamental Research funded the research.
The idea for the study originated with Jackson, who is also an adjunct professor in the UA Department of Geosciences. He thought the warming since the end of the last ice age 14,000 years ago had caused significant changes in vegetation all over the globe, and realized his idea was testable using evidence from ancient pollen and plant fossils -- paleoecological data -- that could show how vegetation had changed.
He and Overpeck, then a UA professor of geosciences, developed the study and enlisted researchers from all over the globe for help and data. UA's Nolan did the bulk of the analysis.
The team used previously published research that calculated how the temperature changed from the ice ages to the pre-industrial era for sites throughout the globe.
For each of the sites, the authors enlisted experts to determine whether the degree of vegetation change since the ice age was low, moderate or large. That common framework made it possible to compare the 594 records.
The experts classified more than 67 percent of the vegetation changes as high and at least another 26 percent as moderate. The changes were especially pronounced in the mid-to-high latitudes in North America, Europe and South America -- regions that were most heavily glaciated and therefore had warmed the most since the ice ages.
"When we compared the spatial patterns of the size of the ecological change with the size of the temperature change, they matched up," Jackson said.
However, the warming projected for the 21st century and beyond will occur much, much faster, he said.
"We're talking about the same amount of change in 10 to 20 thousand years that's going to be crammed into a century or two," he said. "Ecosystems are going to be scrambling to catch up."
As one example, he said forests in the Western U.S. devastated by wildfires might not grow back with the same species that had been there.
"You take the ponderosa pine forests in the Sky Islands and turn it into oak scrub -- we're starting to see that," Jackson said. "Then you can't go up to those pine forests anymore for shade or coolness or the experience of walking through a beautiful grove of trees."
UA Department of Geosciences
U.S. Geological Survey
University of Arizona
University of Michigan
Mari N. Jensen
University of Arizona
University of Michigan
Author list for "Past and future global transformation of terrestrial ecosystems under climate change." Connor Nolan, University of Arizona, Tucson; Jonathan T. Overpeck, University of Michigan and the University of Arizona; Judy R. M. Allen, University of Durham, UK; Patricia M. Anderson, University of Washington, Seattle; Julio L. Betancourt, U.S. Geological Survey, Reston, VA; Heather A. Binney, University of Southampton, UK; Simon Brewer, University of Utah, Salt Lake City; Mark B. Bush, Florida Institute of Technology, Melbourne; Brian M. Chase and Rachid Cheddadi of Centre National de la Recherche Scientifique, Université Montpellier, France; Morteza Djamali, Aix Marseille Université, Aix-en Provence, France; John Dodson, University of New South Wales, Sydney and Chinese Academy of Sciences, Xi'an 71002, Shaanxi; Mary E. Edwards, University of Southampton, UK; William D. Gosling, University of Amsterdam, Netherlands and The Open University, Milton Keynes, UK; Simon Haberle, Australian National University, Canberra, Australia; Sara C. Hotchkiss, University of Wisconsin, Madison; Brian Huntley, University of Durham, UK; Sarah J. Ivory, Pennsylvania State University, State College; A. Peter Kershaw, Monash University, Melbourne, Australia; Soo-Hyun Kim, The Open University, Milton Keynes, UK; Claudio Latorre, Pontificia Universidad Católica de Chile, Santiago; Michelle Leydet, Aix Marseille Université, Aix-en Provence, France; Anne-Marie Lézine, Sorbonne Université, Paris, France; Kam-Biu Liu, Louisiana State University, Baton Rouge; Yao Liu, Northern Arizona University, Flagstaff; A. V. Lozhkin, Far East Branch Russian Academy of Sciences, Magadan, Russia; Matt S. McGlone, Landcare Research, Lincoln, New Zealand; Robert A. Marchant, University of York, UK; Arata Momohara, Chiba University, Japan; Patricio I. Moreno, Universidad de Chile, Santiago; Stefanie Müller, Institute of Geological Sciences, Berlin, Germany; Bette L. Otto-Bliesner, National Center for Atmospheric Research, Boulder, CO; Caiming Shen, Yunnan Normal University, China; Janelle Stevenson, Australian National University, Canberra; Hikaru Takahara, Kyoto Prefectural University, Japan; Pavel E. Tarasov, Institute of Geological Sciences, Berlin, Germany; John Tipton, University of Arkansas, Fayetteville; Annie Vincens, Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement, Aix-en-Provence, France; Chengyu Weng, Tongji University, Shanghai, China; Qinghai Xu, Hebei Normal University, Shijiazhuang, China; Zhuo Zheng, Sun Yat-Sen University, Guangzhou, China; Stephen T. Jackson*, U.S. Geological Survey and the University of Arizona.
*Corresponding author. Email: email@example.com