Late Pleistocene paleoclimate in the Black Hills of South Dakota from isotope records in speleothems

Two coeval speleothems from the Black Hills are used to investigate δ18O and δ13C variations within Reed’s Cave and reconstruct climate during the Wisconsin glacial period from 82 000 to 24 000 years ago. Variation in growth rates between the two speleothems reveals a strong control of hydrology and...

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Bibliographic Details
Published in:Palaeogeography, Palaeoclimatology, Palaeoecology
Main Authors: Serefiddin, Feride, Schwarcz, Henry P., Ford, Derek C., Baldwin, Steve
Format: Text
Language:unknown
Published: Digital Commons @ University of South Florida 2004
Subjects:
Online Access:https://digitalcommons.usf.edu/kip_articles/3093
https://doi.org/10.1016/S0031-0182(03)00639-4