His primary scientific interests are in Holocene, Oceanography, Climate change, Paleoclimatology and Maya. His research integrates issues of δ18O, Deforestation and Chronology in his study of Holocene. His Oceanography study incorporates themes from Marine isotope stage and Glacial period.
The study incorporates disciplines such as Physical geography and Ostracod in addition to Climate change. His Physical geography study combines topics from a wide range of disciplines, such as Mesoamerica and Arid. His work in Maya addresses subjects such as Period, which are connected to disciplines such as Precipitation.
His primary areas of study are Oceanography, Holocene, Physical geography, Sediment and Climate change. His studies in Oceanography integrate themes in fields like Glacial period and Isotopes of carbon. His Holocene research is multidisciplinary, relying on both Deforestation, δ18O and Precipitation.
As a member of one scientific family, he mostly works in the field of Physical geography, focusing on Pleistocene and, on occasion, Chronology. In his study, which falls under the umbrella issue of Sediment, Total organic carbon is strongly linked to Organic matter. Jason H. Curtis has researched Climate change in several fields, including Period, Isotope geochemistry and Maya.
His primary areas of study are Holocene, Physical geography, Oceanography, Sediment and Total organic carbon. His study in the fields of Last Glacial Maximum under the domain of Holocene overlaps with other disciplines such as Volcanism. His Physical geography research includes themes of Glacial period, Radiocarbon dating, Pleistocene, Evaporite and Arid.
His Arid research focuses on subjects like Global climate, which are linked to Paleoclimatology. His Oceanography research is multidisciplinary, incorporating perspectives in Organic matter and Vegetation. His Sediment research is multidisciplinary, incorporating elements of Diatom, Lake ecosystem and Shallow lake.
His primary scientific interests are in Holocene, Physical geography, Oceanography, Precipitation and Arid. His work in Holocene tackles topics such as Monsoon which are related to areas like Isotopes of oxygen, Ice sheet, Temperature record and Younger Dryas. His Physical geography research incorporates elements of Radiocarbon dating, Reforestation, Pleistocene, Macrofossil and Deforestation.
His studies deal with areas such as Organic matter and Mangrove as well as Oceanography. His work deals with themes such as Spatial heterogeneity, Quaternary and Paleolimnology, which intersect with Precipitation. His study in Arid is interdisciplinary in nature, drawing from both Stadial and Climate change, Paleoclimatology, Global climate.
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Possible role of climate in the collapse of Classic Maya civilization
David A. Hodell;Jason H. Curtis;Mark Brenner.
Solar Forcing of Drought Frequency in the Maya Lowlands
David A. Hodell;Mark Brenner;Jason H. Curtis;Thomas Guilderson.
Climate Variability on the Yucatan Peninsula (Mexico) during the Past 3500 Years, and Implications for Maya Cultural Evolution
Jason H. Curtis;David A. Hodell;Mark Brenner.
Quaternary Research (1996)
Reconstruction of Caribbean climate change over the past 10,500 years
David A. Hodell;Jason H. Curtis;Glenn A. Jones;Antonia Higuera-Gundy.
Climate Variation and the Rise and Fall of an Andean Civilization
Michael W. Binford;Alan L. Kolata;Mark Brenner;John W. Janusek.
Quaternary Research (1997)
Abrupt Temperature Changes in the Western Mediterranean over the Past 250,000 Years
Belen Martrat;Joan O. Grimalt;Constancia López-Martínez;Isabel Cacho;Isabel Cacho.
Stable isotope (δ13C and δ15N) signatures of sedimented organic matter as indicators of historic lake trophic state
Mark Brenner;Thomas J. Whitmore;Jason H. Curtis;David A. Hodell.
Journal of Paleolimnology (1999)
Terminal Classic drought in the northern Maya lowlands inferred from multiple sediment cores in Lake Chichancanab (Mexico)
David A. Hodell;Mark Brenner;Jason H. Curtis.
Quaternary Science Reviews (2005)
Onset of “Hudson Strait” Heinrich events in the eastern North Atlantic at the end of the middle Pleistocene transition (∼640 ka)?
David A. Hodell;David A. Hodell;James E. T. Channell;Jason H. Curtis;Oscar E. Romero.
A multi-proxy study of Holocene environmental change in the Maya Lowlands of Peten, Guatemala
Jason H. Curtis;Mark Brenner;David A. Hodell;Richard A. Balser.
Journal of Paleolimnology (1998)
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