Interactions between carbon dioxide, climate, weathering, and the Antarctic ice sheet in the earliest Oligocene
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[1] E. Martin,et al. Antarctic weathering and carbonate compensation at the Eocene-Oligocene transition , 2013 .
[2] David Pollard,et al. Description of a hybrid ice sheet-shelf model, and application to Antarctica , 2012 .
[3] P. Barrett,et al. Antarctic topography at the Eocene–Oligocene boundary , 2012 .
[4] G. Knorr,et al. A warm Miocene climate at low atmospheric CO2 levels , 2011 .
[5] Hugues Goosse,et al. Response of the Greenland and Antarctic Ice Sheets to Multi-Millennial Greenhouse Warming in the Earth System Model of Intermediate Complexity LOVECLIM , 2011 .
[6] P. Wilson,et al. Early Oligocene glaciation and productivity in the eastern equatorial Pacific: Insights into global carbon cycling , 2011 .
[7] J. Zachos,et al. Two-stepping into the icehouse: East Antarctic weathering during progressive ice-sheet expansion at the Eocene–Oligocene transition , 2011 .
[8] David Pollard,et al. A retrospective look at coupled ice sheet–climate modeling , 2010 .
[9] P. Pearson,et al. Atmospheric carbon dioxide through the Eocene–Oligocene climate transition , 2009, Nature.
[10] B. Luyendyk,et al. West Antarctic paleotopography estimated at the Eocene‐Oligocene climate transition , 2009 .
[11] David Pollard,et al. Modelling West Antarctic ice sheet growth and collapse through the past five million years , 2009, Nature.
[12] Caroline H. Lear,et al. Thresholds for Cenozoic bipolar glaciation , 2008, Nature.
[13] Y. Goddéris,et al. Shield effect on continental weathering: Implication for climatic evolution of the Earth at the geological timescale , 2008 .
[14] G. Ravizza,et al. Os isotope chemostratigraphy applied to organic-rich marine sediments from the Eocene-Oligocene transition on the West African margin (ODP Site 959) , 2008 .
[15] David Pollard,et al. Amplification of Cretaceous Warmth by Biological Cloud Feedbacks , 2008, Science.
[16] Heiko Pälike,et al. The Heartbeat of the Oligocene Climate System , 2006, Science.
[17] R. Pierrehumbert,et al. A GEOCLIM simulation of climatic and biogeochemical consequences of Pangea breakup , 2006 .
[18] J. Zachos,et al. Carbon cycle feedbacks and the initiation of Antarctic glaciation in the earliest Oligocene , 2005 .
[19] R. DeConto,et al. Hysteresis in Cenozoic Antarctic ice-sheet variations , 2005 .
[20] Caroline H. Lear,et al. Late Eocene to early Miocene ice sheet dynamics and the global carbon cycle , 2004 .
[21] P. Oliva,et al. Chemical weathering in granitic environments , 2003 .
[22] R. DeConto,et al. A coupled climate–ice sheet modeling approach to the Early Cenozoic history of the Antarctic ice sheet , 2003 .
[23] David Pollard,et al. Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2 , 2003, Nature.
[24] J. Oerlemans. On glacial inception and orography , 2002 .
[25] Catherine Ritz,et al. Modeling the evolution of Antarctic ice sheet over the last 420,000 years: Implications for altitude changes in the Vostok region , 2001 .
[26] B. Dupré,et al. Global silicate weathering and CO2 consumption rates deduced from the chemistry of large rivers , 1999 .
[27] Lee R. Kump,et al. Global chemical erosion over the last 250 MY: Variations due to changes in paleogeography, paleoclimate, and paleogeology , 1999 .
[28] James J. Hack,et al. Response of Climate Simulation to a New Convective Parameterization in the National Center for Atmospheric Research Community Climate Model (CCM3) , 1998 .
[29] David Pollard,et al. Greenland and Antarctic Mass Balances for Present and Doubled Atmospheric CO2 from the GENESIS Version-2 Global Climate Model , 1997 .
[30] Karen A. Salamy,et al. High‐resolution (104 years) deep‐sea foraminiferal stable isotope records of the Eocene‐Oligocene climate transition , 1996 .
[31] Huug van den Dool,et al. Analysis of model-calculated soil moisture over the United States (1931-1993) and applications to long-range temperature forecasts , 1996 .
[32] Y. Erel,et al. A silicate weathering mechanism linking increases in marine 87Sr/ 86Sr with global glaciation , 1995, Nature.
[33] Lee R. Kump,et al. Global chemical erosion during the Last Glacial Maximum and the present: Sensitivity to changes in lithology and hydrology , 1994 .
[34] R. Garrels,et al. The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years , 1983 .
[35] Paul B. Hays,et al. A negative feedback mechanism for the long‐term stabilization of Earth's surface temperature , 1981 .
[36] C. W. Thornthwaite. An Approach Toward a Rational Classification of Climate , 1948 .
[37] R. DeConto,et al. Cenozoic variations of the Antarctic Ice Sheet: A model-data mismatch? , 2007 .
[38] Caroline H. Lear,et al. Rapid stepwise onset of Antarctic glaciation and deeper calcite compensation in the Pacific Ocean , 2005, Nature.
[39] R. DeConto,et al. Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2 , 2003, Nature.
[40] Philippe Huybrechts,et al. Sea-level changes at the LGM from ice-dynamic reconstructions of the Greenland and Antarctic ice sheets during the glacial cycles , 2002 .
[41] K. Salamy,et al. Latest Eocene–Early Oligocene climate change and Southern Ocean fertility: inferences from sediment accumulation and stable isotope data , 1999 .
[42] F. Pattyn,et al. Report of the Third EISMINT Workshop on Model Intercomparison , 1998 .
[43] L. Kump,et al. Global Chemical Erosion during the Cenozoic: Weatherability Balances the Budgets , 1997 .
[44] R. DeConto. Late Cretaceous Climate, Vegetation and Ocean Interactions: AN Earth System Approach to Modeling AN Extreme Climate , 1996 .
[45] R. Berner,et al. GEOCARB III : A REVISED MODEL OF ATMOSPHERIC CO 2 OVER PHANEROZOIC TIME , 2001 .
[46] John Harte,et al. Consider a Spherical Cow: A course in environmental problem solving , 1985 .
[47] C. W. Thornthwaite. An approach toward a rational classification of climate. , 1948 .