A CONTINUOUS 100 THOUSAND-YEAR STALAGMITE Δ18O RECORD FROM THE YUCATAN PENINSULA: IMPLICATIONS FOR CARIBBEAN HYDROCLIMATE ON ORBITAL AND MILLENNIAL TIMESCALES

....................................................................................................................................................... iv Acknowledgments ................................................................................................................................. v List of Tables ....................................................................................................................................... vi List of Figures ..................................................................................................................................... vii List of Abbreviations ........................................................................................................................... ix

[1]  S. Burns,et al.  Long-term monitoring of drip water and groundwater stable isotopic variability in the Yucatán Peninsula: Implications for recharge and speleothem rainfall reconstruction , 2019, Geochimica et Cosmochimica Acta.

[2]  R. Bradley,et al.  Synchronous precipitation reduction in the American Tropics associated with Heinrich 2 , 2017, Scientific Reports.

[3]  R. Edwards,et al.  The Asian monsoon over the past 640,000 years and ice age terminations , 2016, Nature.

[4]  M. Prange,et al.  Palaeoclimatic insights into forcing and response of monsoon rainfall , 2016, Nature.

[5]  J. Moerman,et al.  Northern Borneo stalagmite records reveal West Pacific hydroclimate across MIS 5 and 6 , 2016 .

[6]  C. E. Shaw Late Pleistocene Bays and Reefs: Ancestors to the Modern Caribbean Coast, Yucatán Península, México , 2016, Journal of Coastal Research.

[7]  J. Overpeck,et al.  Coherent changes of southeastern equatorial and northern African rainfall during the last deglaciation , 2014, Science.

[8]  M. Alexander,et al.  Climate variability during warm and cold phases of the Atlantic Multidecadal Oscillation (AMO) 1871–2008 , 2014 .

[9]  P. deMenocal,et al.  Meridional shifts of the Atlantic intertropical convergence zone since the Last Glacial Maximum , 2013 .

[10]  R. Edwards,et al.  Improvements in 230Th dating, 230Th and 234U half-life values, and U–Th isotopic measurements by multi-collector inductively coupled plasma mass spectrometry , 2013 .

[11]  L. Araguás‐Araguás,et al.  Isotopic Patterns in Modern Global Precipitation , 2013 .

[12]  H. Oeschger,et al.  North Atlantic climatic oscillations revealed by deep Greenland ice cores , 2013 .

[13]  A. Timmermann,et al.  Links between tropical rainfall and North Atlantic climate during the last glacial period , 2013 .

[14]  R. Edwards,et al.  Climate change patterns in Amazonia and biodiversity , 2013, Nature Communications.

[15]  R. Edwards,et al.  High-precision and high-resolution carbonate 230Th dating by MC-ICP-MS with SEM protocols , 2012 .

[16]  Eelco J. Rohling,et al.  Making sense of palaeoclimate sensitivity , 2012, Nature.

[17]  Norbert Marwan,et al.  COnstructing Proxy Records from Age models (COPRA) , 2012 .

[18]  R. Edwards,et al.  The Global Paleomonsoon as seen through speleothem records from Asia and the Americas , 2012, Climate Dynamics.

[19]  Mark Brenner,et al.  Rapid climate change and no-analog vegetation in lowland Central America during the last 86,000 years , 2012 .

[20]  T. Guilderson,et al.  A ∼43-ka record of paleoenvironmental change in the Central American lowlands inferred from stable isotopes of lacustrine ostracods , 2012 .

[21]  Eelco J. Rohling,et al.  Collapse of Classic Maya Civilization Related to Modest Reduction in Precipitation , 2012, Science.

[22]  S. Burns,et al.  High-Latitude Forcing of the South American Summer Monsoon During the Last Glacial , 2012, Science.

[23]  Ambarish V. Karmalkar,et al.  Climate change in Central America and Mexico: regional climate model validation and climate change projections , 2011 .

[24]  A. Karmalkar,et al.  High resolution stalagmite climate record from the Yucatán Peninsula spanning the Maya terminal classic period , 2010 .

[25]  P. Beddows,et al.  Linkages between Holocene paleoclimate and paleohydrogeology preserved in a Yucatan underwater cave , 2010 .

[26]  Sara Maria Lerer,et al.  Hydrogeology of the south-eastern Yucatan Peninsula: New insights from water level measurements, geochemistry, geophysics and remote sensing , 2010 .

[27]  Timothy D. Herbert,et al.  Tropical Ocean Temperatures Over the Past 3.5 Million Years , 2010, Science.

[28]  G. Schmidt,et al.  Water vapour source impacts on oxygen isotope variability in tropical precipitation during Heinrich events , 2010 .

[29]  W. Lambert,et al.  Oxygen and hydrogen isotopes of rainfall and dripwater at DeSoto Caverns (Alabama, USA): Key to understanding past variability of moisture transport from the Gulf of Mexico , 2010 .

[30]  M. Lachniet,et al.  Oxygen isotope values of precipitation and surface waters in northern Central America (Belize and Guatemala) are dominated by temperature and amount effects , 2009 .

[31]  D. Hodell,et al.  Onset of “Hudson Strait” Heinrich events in the eastern North Atlantic at the end of the middle Pleistocene transition (∼640 ka)? , 2008 .

[32]  F. Anselmetti,et al.  An 85-ka record of climate change in lowland Central America , 2008 .

[33]  T. Stocker,et al.  High-resolution carbon dioxide concentration record 650,000–800,000 years before present , 2008, Nature.

[34]  W. Cheng,et al.  Fast teleconnections to the tropical Atlantic sector from Atlantic thermohaline adjustment , 2008 .

[35]  E. Muñoz,et al.  Winter and Summer Structure of the Caribbean Low-Level Jet , 2008 .

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

[37]  X. Liang,et al.  Rectification of the Bias in the Wavelet Power Spectrum , 2007 .

[38]  A. Timmermann,et al.  Tropical Air-Sea Interactions Accelerate the Recovery of the Atlantic Meridional Overturning Circulation after a Major Shutdown , 2007 .

[39]  Yan Zhao,et al.  Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum - Part 1: experiments and large-scale features , 2007 .

[40]  Alberto M. Mestas-Nuñez,et al.  Water Vapor Fluxes over the Intra-Americas Sea: Seasonal and Interannual Variability and Associations with Rainfall , 2007 .

[41]  Christina M. Patricola,et al.  Dynamics of the West African Monsoon under Mid-Holocene Precessional Forcing: Regional Climate Model Simulations , 2007 .

[42]  B. Soden,et al.  Robust Responses of the Hydrological Cycle to Global Warming , 2006 .

[43]  Adam A. Scaife,et al.  Climate impacts of the Atlantic Multidecadal Oscillation , 2006 .

[44]  E. Jáuregui,et al.  A Study of Historical Droughts in Southeastern Mexico , 2006 .

[45]  G. Haug,et al.  Variability in the mean latitude of the Atlantic Intertropical Convergence Zone as recorded by riverine input of sediments to the Cariaco Basin (Venezuela) , 2006 .

[46]  Andrei P. Sokolov,et al.  Investigating the Causes of the Response of the Thermohaline Circulation to Past and Future Climate Changes , 2006 .

[47]  S. Klein,et al.  GFDL's CM2 Global Coupled Climate Models. Part I: Formulation and Simulation Characteristics , 2006 .

[48]  R. Higgins,et al.  Characteristics of Landfalling Tropical Cyclones in the United States and Mexico: Climatology and Interannual Variability , 2005 .

[49]  Mathias Vuille,et al.  Insolation-driven changes in atmospheric circulation over the past 116,000 years in subtropical Brazil , 2005, Nature.

[50]  J. Betancourt,et al.  A tree‐ring based reconstruction of the Atlantic Multidecadal Oscillation since 1567 A.D. , 2004 .

[51]  A. Wittmann,et al.  The Fluidized Chicxulub Ejecta Blanket, Mexico: Implications for Mars , 2004 .

[52]  M. Biasutti,et al.  Sensitivity of the Atlantic Intertropical Convergence Zone to Last Glacial Maximum boundary conditions , 2003 .

[53]  D. R. Hardy,et al.  Modeling δ18O in precipitation over the tropical Americas: 2. Simulation of the stable isotope signal in Andean ice cores , 2003 .

[54]  S. B. Moran,et al.  Measurement of attogram quantities of 231Pa in dissolved and particulate fractions of seawater by isotope dilution thermal ionization mass spectroscopy. , 2003, Analytical chemistry.

[55]  Manfred Mudelsee,et al.  A 780-year annually resolved record of Indian Ocean monsoon precipitation from a speleothem from south Oman , 2002, Journal of Geophysical Research.

[56]  S. Rahmstorf Ocean circulation and climate during the past 120,000 years , 2002, Nature.

[57]  M. J. Salinger,et al.  Relative influences of the Interdecadal Pacific Oscillation and ENSO on the South Pacific Convergence Zone , 2002 .

[58]  S. B. Moran,et al.  Uranium and thorium isotopic and concentration measurements by magnetic sector inductively coupled plasma mass spectrometry , 2002 .

[59]  R. L. Edwards,et al.  A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China , 2001, Science.

[60]  W. M. Gray,et al.  The Recent Increase in Atlantic Hurricane Activity: Causes and Implications , 2001, Science.

[61]  Shawn J. Marshall,et al.  Freshwater Forcing of Abrupt Climate Change During the Last Glaciation , 2001, Science.

[62]  Geoffrey O. Seltzer,et al.  The history of South American tropical precipitation for the past 25,000 years. , 2001, Science.

[63]  G. Haug,et al.  Rapid changes in the hydrologic cycle of the tropical Atlantic during the last glacial. , 2000, Science.

[64]  N. Shackleton,et al.  The 100,000-year ice-Age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity , 2000, Science.

[65]  V. Magaña,et al.  The midsummer drought over Mexico and Central America , 1999 .

[66]  Lloyd J. Shapiro,et al.  Physical Mechanisms for the Association of El Niño and West African Rainfall with Atlantic Major Hurricane Activity , 1996 .

[67]  W. Broecker,et al.  The role of ocean-atmosphere reorganizations in glacial cycles , 1989 .

[68]  J. Kutzbach,et al.  The Influence of Changing Orbital Parameters and Surface Boundary Conditions on Climate Simulations for the Past 18 000 Years , 1986 .

[69]  W. M. Gray,et al.  Atlantic Seasonal Hurricane Frequency. Part I: El Niño and 30 mb Quasi-Biennial Oscillation Influences , 1984 .

[70]  J. Shukla,et al.  On the Dynamics of Droughts in Northeast Brazil: Observations, Theory and Numerical Experiments with a General Circulation Model , 1981 .

[71]  C. Hendy,et al.  The isotopic geochemistry of speleothems—I. The calculation of the effects of different modes of formation on the isotopic composition of speleothems and their applicability as palaeoclimatic indicators , 1971 .

[72]  D. Hoffmann,et al.  Millennial-scale climate variability during the last 12.5 ka recorded in a Caribbean speleothem , 2013 .

[73]  E. Villalobos,et al.  Interglacial Hydroclimate in the Tropical West Pacific Through the Late Pleistocene , 2012 .

[74]  B. Otto‐Bliesner,et al.  The sensitivity of the climate response to the magnitude and location of freshwater forcing: last glacial maximum experiments , 2010 .

[75]  J. A. Dorale,et al.  LIMITATIONS OF HENDY TEST CRITERIA IN JUDGING THE PALEOCLIMATIC SUITABILITY OF SPELEOTHEMS AND THE NEED FOR REPLICATION , 2009 .

[76]  C. Torrence,et al.  A Practical Guide to Wavelet Analysis. , 1998 .

[77]  H. Oeschger,et al.  Late Glacial Climate History from Ice Cores , 1983 .

[78]  E. L. Ramos. Geological Summary of the Yucatan Peninsula , 1975 .