Parallel climate and vegetation responses to the early Holocene collapse of the Laurentide Ice Sheet

Parallel changes in lake-level and pollen data show that the rapid decline of the Laurentide Ice Sheet (LIS) between 10,000 and 8000 cal yr BP triggered a step-like change in North American climates: from an ice-sheet-and-insolation-dominated climate to a climate primarily controlled by insolation....

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Bibliographic Details
Main Authors: Bryan Shumana, Patrick Bartleinb, Nathaniel Logara, Paige Newbya, Thompson Webb Iiia
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2001
Subjects:
MAP
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.580.8423
http://www.geo.brown.edu/georesearch/esh/QE/Publications/QSR2002/BShuman/ParallelPesponses/ParallelResponses.pdf