Paleomonsoon precipitation deduced from a sediment core from the equatorial Indian Ocean

[1]  R. Ramesh,et al.  Early deglacial (∼19–17 ka) strengthening of the northeast monsoon , 2005 .

[2]  R. Ganeshram,et al.  Variations in tropical convection as an amplifier of global climate change at the millennial scale [rapid communication] , 2005 .

[3]  K. Hughen,et al.  Synchroneity of Tropical and High-Latitude Atlantic Temperatures over the Last Glacial Termination , 2003, Science.

[4]  F. Sirocko,et al.  Orbital insolation forcing of the Indian Monsoon – a motor for global climate changes? , 2003 .

[5]  R. Alley,et al.  Ice Core Records of Atmospheric N2O Covering the Last 106,000 Years , 2003, Science.

[6]  Y. Rosenthal,et al.  The amplitude and phasing of climate change during the last deglaciation in the Sulu Sea, western equatorial Pacific , 2003 .

[7]  G. Reichart,et al.  Synchroneity of oxygen minimum zone intensity on the Oman and Pakistan margins at sub-Milankovitch time scales , 2002 .

[8]  M. Altabet,et al.  The effect of millennial-scale changes in Arabian Sea denitrification on atmospheric CO2 , 2002, Nature.

[9]  J. Southon,et al.  Marine Reservoir Corrections for the Indian Ocean and Southeast Asia , 2002, Radiocarbon.

[10]  K. Stattegger,et al.  Synchronous Tropical South China Sea SST Change and Greenland Warming During Deglaciation , 2001, Science.

[11]  J. Jouzel,et al.  Oxygen isotope/salinity relationship in the northern Indian Ocean , 2001 .

[12]  R. Bhushan,et al.  ΔR Correction Values for the Northern Indian Ocean , 2001, Radiocarbon.

[13]  F. Schott,et al.  The monsoon circulation of the Indian Ocean , 2001 .

[14]  J. Severinghaus,et al.  On the origin and timing of rapid changes in atmospheric methane during the Last Glacial Period , 2000 .

[15]  R. Ramesh,et al.  High resolution Holocene monsoon record from the eastern Arabian Sea , 2000 .

[16]  Richard B. Alley,et al.  The Younger Dryas cold interval as viewed from central Greenland , 2000 .

[17]  Rainer Zahn,et al.  Warming of the tropical Atlantic Ocean and slowdown of thermohaline circulation during the last deglaciation , 1999, Nature.

[18]  Sandy P. Harrison,et al.  Monsoon changes for 6000 years ago: Results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP) , 1999 .

[19]  G. Reichart,et al.  Temporal variability in the northern Arabian Sea oxygen minimum zone (OMZ) during the last 225,000 years , 1998 .

[20]  H. Schulz,et al.  Correlation between Arabian Sea and Greenland climate oscillations of the past 110,000 years , 1998 .

[21]  J. W. Beck,et al.  INTCAL98 Radiocarbon Age Calibration, 24,000–0 cal BP , 1998, Radiocarbon.

[22]  M. Stuiver,et al.  Oxygen 18/16 variability in Greenland snow and ice with 10 -3- to 105-year time resolution , 1997 .

[23]  E. Bard,et al.  Interhemispheric synchrony of the last deglaciation inferred from alkenone palaeothermometry , 1997, Nature.

[24]  E. Brook,et al.  Rapid Variations in Atmospheric Methane Concentration During the Past 110,000 Years , 1996, Science.

[25]  M. Stuiver,et al.  The GISP2 δ18O Climate Record of the Past 16,500 Years and the Role of the Sun, Ocean, and Volcanoes , 1995, Quaternary Research.

[26]  P. Mayewski,et al.  The Accumulation Record from the GISP2 Core as an Indicator of Climate Change Throughout the Holocene , 1994, Science.

[27]  Wallace S. Broecker,et al.  Massive iceberg discharges as triggers for global climate change , 1994, Nature.

[28]  P. Bloomfield,et al.  Changes in Atmospheric Circulation and Ocean Ice Cover over the North Atlantic During the Last 41,000 Years , 1994, Science.

[29]  J. Jouzel,et al.  Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores , 1993, Nature.

[30]  J. Jouzel,et al.  Evidence for general instability of past climate from a 250-kyr ice-core record , 1993, Nature.

[31]  E. Bard,et al.  Reconstructing sea surface temperature and salinity using δ18O and alkenone records , 1993, Nature.

[32]  Syukuro Manabe,et al.  Transient responses of a coupled ocean-atmosphere model to gradual changes of atmospheric CO2 , 1991 .

[33]  R. Fairbanks A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation , 1989, Nature.

[34]  D. Donahue,et al.  Carbon-14 activities in recently fallen meteorites and Antarctic meteorites , 1989 .

[35]  J. Duplessy,et al.  Variations in mode of formation and temperature of oceanic deep waters over the past 125,000 years , 1987, Nature.

[36]  J. D. Hays,et al.  Age Dating and the Orbital Theory of the Ice Ages: Development of a High-Resolution 0 to 300,000-Year Chronostratigraphy , 1987, Quaternary Research.

[37]  W. Prell,et al.  Coherent response of Arabian Sea upwelling and pollen transport to late Quaternary monsoonal winds , 1986, Nature.

[38]  D. Donahue,et al.  Operation of the NSF-Arizona Accelerator Facility for Radioisotope Analysis and Results from Selected Collaborative Research Projects , 1986, Radiocarbon.

[39]  J. Erez,et al.  Experimental paleotemperature equation for planktonic foraminifera , 1983 .

[40]  P. Wiebe,et al.  Vertical distribution and isotopic fractionation of living planktonic foraminifera from the Panama Basin , 1982, Nature.

[41]  J. Duplessy,et al.  Climatic conditions deduced from a 150-kyr oxygen isotope–pollen record from the Arabian Sea , 1982, Nature.

[42]  J. Duplessy Glacial to interglacial contrasts in the northern Indian Ocean , 1982, Nature.

[43]  G. Reverdin,et al.  Water vapour transport over the Indian Ocean during summer 1975 , 1981 .

[44]  J. Duplessy,et al.  Oxygen and carbon isotopic composition and biogeographic distribution of planktonic foraminifera in the Indian Ocean , 1981 .

[45]  B. Molfino,et al.  Surface Circulation of the Indian Ocean during the Last Glacial Maximum, Approximately 18,000 yr B.P. , 1980, Quaternary Research.

[46]  A. Bé An ecological, zoogeographic and taxonomic review of recent planktonic foraminifera , 1977 .