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....
Main Authors: | , , , , |
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Format: | Text |
Language: | English |
Published: |
2001
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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 |