SpringerBriefs in Earth System Sciences: Comparisons, Linkages and Uncertainties

Rutter, Nat; Coronato, Andrea; Helmens, Karin; Rabassa, Jorge; Zárate, Marcelo

Improved dating methods have increased our ability to more precisely determine the timing and durations of glaciations. Utilizing glacial and loess deposits, we have compared glaciations that occurred in North and South America in order to determine if events are synchronous or not, to explore forcing mechanisms, and to compare glaciations with cold periods of the Marine Oxygen Isotope stages and the loess/paleosol records of China. Stratigraphic sections containing a variety of glacial deposits, some with interbedded volcanics, as well as loess deposits, were used in reconstructing the glacial history. The Late Pleistocene (Brunhes Chron) Last Glacial Maximum is recognized in  mountain and continental areas of North America but only in the mountains of South America. Commonly our comparisons indicate roughly synchronous glaciations on the two continents, whereas other glaciations are more elusive and difficult to compare. Although our comparisons are at low resolutions, the results suggest that Milankovitch forcing is most likely the dominant trigger for hemispheric glaciation modified by local factors.

Details

Published by: Springer

Publication Date: 2012-07-01

Format: Paperback

ISBN-13: 9789400743984

DOI: 10.1007/978-94-007-4399-1

Dimensions: 235cm x155cm

Pages: 67