scholarly journals Reconstructing Pleistocene Climatic Change from the Oxygen Isotope Composition of Sediments: A Review

1984 ◽  
Vol 5 ◽  
pp. 43-46 ◽  
Author(s):  
Curt Covey

The isotope composition of ocean sediments is the chief data source for Pleistocene climatic changes. It is generally believed that the18O/16O ratio of a sample indicates the global total of glacial ice at the time the sample was deposited. This is roughly correct, but numerous complicating factors limit the accuracy of the isotope proxies.

1984 ◽  
Vol 5 ◽  
pp. 43-46
Author(s):  
Curt Covey

The isotope composition of ocean sediments is the chief data source for Pleistocene climatic changes. It is generally believed that the 18O/16O ratio of a sample indicates the global total of glacial ice at the time the sample was deposited. This is roughly correct, but numerous complicating factors limit the accuracy of the isotope proxies.


Geology ◽  
1993 ◽  
Vol 21 (3) ◽  
pp. 281 ◽  
Author(s):  
Gerald M. Friedman ◽  
R. P. Major ◽  
R. Michael Lloyd ◽  
F. Jerry Lucia

2007 ◽  
Vol 41 (6) ◽  
pp. 1870-1876 ◽  
Author(s):  
Jorge E. Spangenberg ◽  
Bernhard Dold ◽  
Marie-Louise Vogt ◽  
Hans-Rudolf Pfeifer

2011 ◽  
Vol 438 (1) ◽  
pp. 697-700
Author(s):  
N. S. Bortnikov ◽  
V. M. Novikov ◽  
E. O. Dubinina ◽  
A. D. Savko ◽  
A. G. Berketa ◽  
...  

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