Stalagmite evidence from Belize indicating significant droughts at the time of Preclassic Abandonment, the Maya Hiatus, and the Classic Maya collapse

[1]  M. Lachniet,et al.  Use of correlation and stepwise regression to evaluate physical controls on the stable isotope values of Panamanian rain and surface waters , 2006 .

[2]  C. Bronk RADIOCARBON CALIBRATION AND ANALYSIS OF STRATIGRAPHY: THE OxCal PROGRAM , 2006 .

[3]  Martin Werner,et al.  Stable isotopes in precipitation recording South American summer monsoon and ENSO variability: observations and model results , 2005 .

[4]  C. Hillaire‐Marcel,et al.  Tropical response to the 8200 yr B.P. cold event? Speleothem isotopes indicate a weakened early Holocene monsoon in Costa Rica: Comment and Reply COMMENT , 2005 .

[5]  S. Burns,et al.  Tropical response to the 8200 yr B.P. cold event? Speleothem isotopes indicate a weakened early Holocene monsoon in Costa Rica , 2004 .

[6]  D. Piperno,et al.  A 1500‐year El Niño/Southern Oscillation and rainfall history for the Isthmus of Panama from speleothem calcite , 2004 .

[7]  Konrad A Hughen,et al.  Climate and the Collapse of Maya Civilization , 2003, Science.

[8]  D. Sahagian,et al.  El Niño Events Recorded by Stalagmite Carbon Isotopes , 2002, Science.

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

[10]  Mark Brenner,et al.  A 4000-Year Lacustrine Record of Environmental Change in the Southern Maya Lowlands, Petén, Guatemala , 2002, Quaternary Research.

[11]  J. Fontes,et al.  The altitude effect on the isotopic composition of tropical rains , 2001 .

[12]  P. deMenocal Cultural Responses to Climate Change During the Late Holocene , 2001, Science.

[13]  R. Gill The great Maya droughts : water, life, and death , 2001 .

[14]  H. Schwarcz,et al.  Paleoclimate and vegetation of the Last Glacial Cycles in Jerusalem from a Speleothem Record , 2000 .

[15]  Hai Cheng,et al.  The half-lives of uranium-234 and thorium-230 , 2000 .

[16]  W. Karlén,et al.  Stable isotope composition of tropical high-altitude fresh-waters on Mt. Kenya, Equatorial East Africa , 2000 .

[17]  J. Webster Speleothem evidence of late Holocene climate variation in the Maya lowlands of Belize Central American and archaeological implications , 2000 .

[18]  L. Sigha-Nkamdjou,et al.  Variations of the stable isotopic compositions of rainfall events from the Cameroon rain forest, Central Africa , 1999 .

[19]  J. D. Hughes The classic Maya collapse , 1999 .

[20]  E. Derbyshire,et al.  Paleoenvironmental reconstruction in arid lands , 1999 .

[21]  L. Araguás‐Araguás,et al.  Stable isotope composition of precipitation over southeast Asia , 1998 .

[22]  P. Smart,et al.  High-resolution records of soil humification and paleoclimate change from variations in speleothem luminescence excitation and emission wavelengths , 1998 .

[23]  H. Schwarcz,et al.  A submerged stalactite from Belize: Petrography, geochemistry, and geochronology of massive marine cementation , 1998, Carbonates and Evaporites.

[24]  A. Tanahara,et al.  Application of excess 210Pb dating method to stalactites. , 1998 .

[25]  J. Brady,et al.  Geoarchaeological investigations on the northern Vaca Plateau, Belize , 1998 .

[26]  L. Keigwin,et al.  The Little Ice Age and Medieval Warm Period in the Sargasso Sea , 1996, Science.

[27]  D. Hodell,et al.  Climate Variability on the Yucatan Peninsula (Mexico) during the Past 3500 Years, and Implications for Maya Cultural Evolution , 1996, Quaternary Research.

[28]  D. Hodell,et al.  Possible role of climate in the collapse of Classic Maya civilization , 1995, Nature.

[29]  Christopher Bronk,et al.  Radiocarbon Calibration and Analysis of Stratigraphy: The OxCal Program , 1995, Radiocarbon.

[30]  Christopher Bronk Ramsey,et al.  Radiocarbon Calibration and Analysis of Stratigraphy: The OxCal Program , 1995, Radiocarbon.

[31]  H. Schwarcz,et al.  Luminescent microbanding in speleothems: High-resolution chronology and paleoclimate , 1994 .

[32]  T. Iliffe,et al.  Age determination of recent cave deposits using excess 210Pb ‐ A new technique , 1993 .

[33]  Gary G. Gallopin,et al.  A Water Storage Adaptation in the Maya Lowlands , 1991, Science.

[34]  B. Taylor,et al.  Stable isotope analysis of multiple carbonate samples using selective acid extraction , 1990 .

[35]  Gary G. Gallopin Water Storage Technology at Tikal, Guatemala , 1990 .

[36]  G. Wasserburg,et al.  238U234U230Th232Th systematics and the precise measurement of time over the past 500,000 years , 1987 .

[37]  Arlen F. Chase,et al.  The Lowland Maya Postclassic. , 1986 .

[38]  Arlen F. Chase,et al.  Postclassic Temporal and Spatial Frames for the Lowland Maya: A Background , 1985, The Lowland Maya Postclassic.

[39]  R. Santley The Dynamics of Apocalypse: A Systems Simulation of the Classic Maya Collapse. John W. G. Lowe , 1985 .

[40]  W. Folan Contributions to the archaeology and ethnohistory of Greater Mesoamerica , 1985 .

[41]  R. Adams,et al.  Spatial Patterns and Regional Growth among Classic Maya Cities , 1981, American Antiquity.

[42]  R. Sternberg,et al.  The use of Pb-210 geochronology as a sedimentological tool: Application to the Washington continental shelf , 1979 .

[43]  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 .

[44]  G. L. Vinson Upper Cretaceous and Tertiary Stratigraphy of Guatemala , 1962 .

[45]  John Eric Sidney Thompson The rise and fall of Maya civilization , 1954 .

[46]  J. McCrea On the Isotopic Chemistry of Carbonates and a Paleotemperature Scale , 1950 .

[47]  R. Edwards,et al.  U-234 U _ 230 Th-232 Th systematics and the precise measurement of time over the past 500 , 000 years , 2022 .