Author
Adam, David PeterIssue Date
1965Keywords
CaliforniaCenozoic
microfossils
paleontology
palynomorphs
Quaternary
Sierra Nevada
United States
Pollen, Fossil -- Sierra Nevada (Calif. and Nev.)
Palynology -- Sierra Nevada (Calif. and Nev.)
Paleoclimatology -- Sierra Nevada (Calif. and Nev.)
Committee Chair
Martin, Paul S.
Metadata
Show full item recordPublisher
The University of Arizona.Rights
Copyright © is held by the author. Digital access to this material is made possible by the Antevs Library, Department of Geosciences, and the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author or the department.Abstract
Pollen analysis of two surface transects of modern soil samples and four stratigraphic sections from the central Sierra Nevada of California have provided a climatic record covering the time interval since the recession of the last glaciers of the Wisconsin glaciation. Two separate warm intervals are recognized between the recession of the Wisconsin glaciers and the reappearance of glaciers in the Sierra during the Little Ice Age.Type
textThesis-Reproduction (electronic)
Degree Name
M.S.Degree Level
mastersDegree Program
Graduate CollegeGeochronology