Stable isotope record, Mg/Ca ratios and age model of St. Stephens Quarry, Alabama, supplement to: Katz, Miriam E; Miller, Kenneth G; Wright, James D; Wade, Bridget S; Browning, James V; Cramer, Benjamin S; Rosenthal, Yair (2008): Stepwise transition from the Eocene greenhouse to the Oligocene icehouse. Nature Geoscience, 1, 329-334

In the largest global cooling event of the Cenozoic Era, between 33.8 and 33.5 Myr ago, warm, high-CO2 conditions gave way to the variable 'icehouse' climates that prevail today. Despite intense study, the history of cooling versus ice-sheet growth and sea-level fall reconstructed from oxy...

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Bibliographic Details
Main Authors: Katz, Miriam E, Miller, Kenneth G, Wright, James D, Wade, Bridget S, Browning, James V, Cramer, Benjamin S, Rosenthal, Yair
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2008
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.769587
https://doi.pangaea.de/10.1594/PANGAEA.769587