Two-phase change in CO2, Antarctic temperature and global climate during Termination II

[1]  F. Joos,et al.  A reconstruction of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the glacial inception , 2013 .

[2]  J. Jouzel,et al.  Synchronous Change of Atmospheric CO2 and Antarctic Temperature During the Last Deglacial Warming , 2013, Science.

[3]  M. Loutre,et al.  An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120--800 ka , 2012 .

[4]  J. Jouzel,et al.  On the gas-ice depth difference (Δdepth) along the EPICA Dome C ice core , 2012 .

[5]  Thomas F. Stocker,et al.  Carbon Isotope Constraints on the Deglacial CO2 Rise from Ice Cores , 2012, Science.

[6]  S. Rasmussen,et al.  Climate of the Past Tightened constraints on the time-lag between Antarctic temperature and CO 2 during the last deglaciation , 2012 .

[7]  D. Roche,et al.  Impact of brine-induced stratification on the glacial carbon cycle , 2010 .

[8]  G. Cabioch,et al.  Abrupt sea surface pH change at the end of the Younger Dryas in the central sub-equatorial Pacific inferred from boron isotope abundance in corals ( Porites ) , 2010 .

[9]  V. Masson‐Delmotte,et al.  Changes in atmospheric CO2 and its carbon isotopic ratio during the penultimate deglaciation , 2010 .

[10]  R. L. Edwards,et al.  The Last Glacial Termination , 2010, Science.

[11]  R. Röthlisberger,et al.  Abrupt change of Antarctic moisture origin at the end of Termination II , 2010, Proceedings of the National Academy of Sciences.

[12]  E. Michel,et al.  Constraint of the CO2 rise by new atmospheric carbon isotopic measurements during the last deglaciation , 2010 .

[13]  E. Michel,et al.  Ventilation of the Deep Southern Ocean and Deglacial CO2 Rise , 2010, Science.

[14]  J. Schmitt,et al.  Atmospheric δ13CO2 and its relation to pCO2 and deep ocean δ13C during the late Pleistocene , 2010 .

[15]  V. Masson‐Delmotte,et al.  Synchronising EDML and NorthGRIP ice cores using δ18O of atmospheric oxygen (δ18Oatm) and CH4 measurements over MIS5 (80–123 kyr) , 2010 .

[16]  J. Jouzel,et al.  What drives the millennial and orbital variations of δ18Oatm , 2010 .

[17]  R. Röthlisberger,et al.  The deuterium excess records of EPICA Dome C and Dronning Maud Land ice cores (East Antarctica) , 2010 .

[18]  J. Schmitt,et al.  Atmospheric δ 13 CO 2 and its relation to p CO 2 and deep ocean δ 13 C during the late Pleistocene , 2010 .

[19]  W. Broecker,et al.  Ice Age Terminations , 2009, Science.

[20]  R. Beaudette,et al.  Oxygen-18 of O2 Records the Impact of Abrupt Climate Change on the Terrestrial Biosphere , 2009, Science.

[21]  R. Röthlisberger,et al.  Glacial terminations as southern warmings without northern control , 2009 .

[22]  W. Broecker,et al.  Interhemispheric Atlantic seesaw response during the last deglaciation , 2009, Nature.

[23]  J. Jouzel,et al.  Firn processes and N-15 of N2: potential for a gas-phase climate proxy , 2008 .

[24]  T. Stocker,et al.  Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years , 2008, Nature.

[25]  Xiaohua Shao,et al.  Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years , 2008, Nature.

[26]  Kenji Kawamura,et al.  The EDC3 chronology for the EPICA Dome C ice core , 2007 .

[27]  A. Schilt,et al.  Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years , 2007, Science.

[28]  K. Lambeck,et al.  Constraints on the Late Saalian to early Middle Weichselian ice sheet of Eurasia from field data and rebound modelling , 2006 .

[29]  R. Edwards,et al.  A penultimate glacial monsoon record from Hulu Cave and two-phase glacial terminations , 2006 .

[30]  C. Pujol,et al.  Climatic “pause” during Termination II identified in shallow and intermediate waters off the Iberian margin , 2004 .

[31]  Jiancheng Kang,et al.  Timing of Atmospheric CO2 and Antarctic Temperature Changes Across Termination III , 2003, Science.

[32]  F. Taylor,et al.  Direct Determination of the Timing of Sea Level Change During Termination II , 2002, Science.

[33]  J. Jouzel,et al.  Atmospheric oxygen 18 and sea-level changes , 2002 .

[34]  R. Alley,et al.  Stochastic resonance in the North Atlantic , 2001 .

[35]  T. Stocker,et al.  Atmospheric CO2 concentrations over the last glacial termination. , 2001, Science.

[36]  Smith,et al.  Ice core records of atmospheric CO2 around the last three glacial terminations , 1999, Science.

[37]  Wallace S. Broecker,et al.  PALEOCEAN CIRCULATION DURING THE LAST DEGLACIATION : A BIPOLAR SEESAW ? , 1998 .

[38]  T. Sowers,et al.  The Dole Effect and its variations during the last 130,000 years as measured in the Vostok Ice Core , 1994 .

[39]  André Berger,et al.  Long-term variations of daily insolation and Quaternary climatic changes , 1978 .