• Corpus ID: 12666546

Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO 2

@inproceedings{Foley2003RapidCG,
  title={Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO 2},
  author={Stephen F. Foley and Stephan Buhre and Dorrit E. Jacob},
  year={2003}
}
1313–1317 (2001). 18. Chen, C.-L. Elements of Optoelectronics and Fiber Optics (Irwin, Chicago, 1996). 19. Wang, J., Gudiksen, M. S., Duan, X., Cui, Y. & Lieber, C. M. Highly polarized photoluminescence and polarization sensitive photodetectors from single indium phosphide nanowires. Science 293, 1455–1457 (2001). 20. Bagnall, D. M., Ullrich, B., Sakai, H. & Segawa, Y. Micro-cavity lasing of optically excited CdS thin films at room temperature. J. Cryst. Growth. 214/215, 1015–1018 (2000). 21… 

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References

SHOWING 1-10 OF 48 REFERENCES
Magnetobiostratigraphic chronology of the Eocene—Oligocene transition in the CIROS-1 core, Victoria Land margin, Antarctica: Implications for Antarctic glacial history
In 1986, cores were obtained to a depth of 702 m (with 98% recovery) from the CIROS-1 drill hole beneath the Ross Sea on the Victoria Land margin. Glaciogene sediments identified near the base of the
Cenozoic evolution of Antarctic glaciation the Circum-Antarctic Ocean and their impact on global paleoceanography
Deep-sea drilling in the Antarctic region (Deep-Sea Drilling Project legs 28, 29, 35, and 36) has provided many new data about the development of circum-Antarctic circulation and the closely related
Miocene evolution of atmospheric carbon dioxide
Changes in pCO2 or ocean circulation are generally invoked to explain warm early Miocene climates and a rapid East Antarctic ice sheet (EAIS) expansion in the middle Miocene. This study reconstructs
Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present
TLDR
This work focuses primarily on the periodic and anomalous components of variability over the early portion of this era, as constrained by the latest generation of deep-sea isotope records.
The Opening of the Tasmanian Gateway Drove Global Cenozoic Paleoclimatic and Paleoceanographic Changes: Results of Leg 189
The major ice sheets of the Cenozoic Era are unusual in geological history. Progressive cooling at high latitudes during the Cenozoic eventually formed major ice sheets, initially on Antarctica and
Glaciological modelling of the late Cenozoic East Antarctic ice sheet: Stability or dynamism?
On the basis of geological arguments, two widely different hypotheses have been proposed for the late-Tertiary glacial history of East Antarctica. Theseinvoke ice-sheet reconstructions ranging from
The opening of Drake Passage
Origin of the Middle Pleistocene Transition by ice sheet erosion of regolith
The transition in the middle Pleistocene (∼0.9 Ma) seen in δ18O deep-sea-core records from relatively low-amplitude, high-frequency (41 kyr) to high-amplitude, low-frequency (100 kyr) ice volume
Tectonic boundary conditions for climate reconstructions
Introduction 1. Significance of Tectonic Boundary Conditions for Paleoclimate Simulations I. Role of Continental Configuration 2. The Role of Geography and Atmospheric CO2 in Long-Term Climate
...
1
2
3
4
5
...