Fossil-pollen

Quantifying the response of vegetation to climate change across timescales
Climate and ecosystems exhibit dynamic behavior across various timescales. Existing studies often focus on individual timescales when …
David Fastovich, Stephen R. Meyers, Erin E. Saupe, John W. Williams, Maria Dornelas, Elizabeth M. Dowding, Seth Finnegan, Huai-Hsuan M. Huang, Lukas Jonkers, Wolfgang Kiessling, Ádám T. Kocsis, Qijian Li, Lee Hsiang Liow, Lin Na, Amelia M. Penny, Kate Pippenger, Johan Renaudie, Marina C. Rillo, Jansen Smith, Manuel J. Steinbauer, Mauro Sugawara, Adam Tomašovỳch, Moriaki Yasuhara, Pincelli M. Hull
Quantifying the response of vegetation to climate change across timescales
Roles of climatic and anthropogenic factors in shaping Holocene vegetation and fire regimes in Great Dismal Swamp, eastern USA
The Great Dismal Swamp wetland, spanning >400 km2 along the Virginia and North Carolina border, was shaped by a complex combination …
Debra A. Willard, Miriam C. Jones, Jay Alder, David Fastovich, Kristen E. Hoefke, Robert K. Poirier, Fred C. Wurster
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Roles of climatic and anthropogenic factors in shaping Holocene vegetation and fire regimes in Great Dismal Swamp, eastern USA
Spatial fingerprints and mechanisms of precipitation and temperature changes during the Younger Dryas in eastern North America
Here we seek to establish the spatial fingerprints of precipitation and temperature changes in eastern North America during the Younger …
David Fastovich, James M. Russell, Shaun A. Marcott, John W. Williams
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Spatial fingerprints and mechanisms of precipitation and temperature changes during the Younger Dryas in eastern North America
Patterns, mechanisms, and legacies of abrupt climate change: examining the Younger Dryas in eastern North America
Increasing global temperatures from anthropogenic greenhouse gas emissions are driving widespread climatological and ecological changes …
David Fastovich
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More than One Way to Kill a Spruce Forest: The Role of Fire and Climate in the Late-Glacial Termination of Spruce Woodlands across the Southern Great Lakes
In the southern Great Lakes Region, North America, between 19,000 and 8,000 years ago, temperatures rose by 2.5-6.5 degrees C and …
Allison M. Jensen, David Fastovich, Benjamin I. Watson, Jacqueline L. Gill, Stephen T. Jackson, James M. Russell, Joseph Bevington, Kate Hayes, Katherine B. Lininger, Claire Rubbelke, Grace C. Schellinger, John W. Williams
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More than One Way to Kill a Spruce Forest: The Role of Fire and Climate in the Late-Glacial Termination of Spruce Woodlands across the Southern Great Lakes
Spatial Fingerprint of Younger Dryas Cooling and Warming in Eastern North America
Abstract The Younger Dryas (YD, 12.9-11.7 ka) is the most recent, near-global interval of abrupt climate change with rates similar to …
David Fastovich, James M. Russell, Stephen T. Jackson, Teresa R. Krause, Shaun A. Marcott, John W. Williams
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Spatial Fingerprint of Younger Dryas Cooling and Warming in Eastern North America
Deglacial Temperature Controls on No-Analog Community Establishment in the Great Lakes Region
Understanding the drivers of vegetation dynamics and no-analog communities in eastern North America is hampered by a scarcity of …
David Fastovich, James M. Russell, Stephen T. Jackson, John W. Williams
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Deglacial Temperature Controls on No-Analog Community Establishment in the Great Lakes Region
Temperature Controls on No-Analog Community Establishment in the Great Lakes Region
Temperature reconstructions in eastern North America from pollen are rife in the literature, but these reconstructions cannot be used …
David Fastovich
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