His primary areas of investigation include Radiocarbon dating, Oceanography, Calibration curve, Physical geography and Ecology. Radiocarbon dating is the subject of his research, which falls under Paleontology. As a part of the same scientific study, Thomas P. Guilderson usually deals with the Paleontology, concentrating on Foraminifera and frequently concerns with Reservoir effect, Mixed layer and Varve.
His Calibration curve study integrates concerns from other disciplines, such as Calibration and Northern Hemisphere. His work in Calibration addresses subjects such as Younger Dryas, which are connected to disciplines such as Data set, Epigravettian and Multi proxy. His Physical geography research incorporates themes from Palynology, Estuary, Salt marsh and Tsuga.
His main research concerns Oceanography, Radiocarbon dating, Coral, Deep sea and Holocene. While the research belongs to areas of Oceanography, he spends his time largely on the problem of Glacial period, intersecting his research to questions surrounding North Atlantic Deep Water, Ice sheet and Climate change. Thomas P. Guilderson has researched Radiocarbon dating in several fields, including Dissolved organic carbon, Calibration curve and Before Present.
His research in Calibration curve intersects with topics in Calibration and Physical geography. His Coral research integrates issues from Reef and Surface water. His Deep sea research includes elements of δ13C and Biogeochemical cycle.
Thomas P. Guilderson focuses on Radiocarbon dating, Oceanography, Deep sea, Environmental chemistry and Dissolved organic carbon. With his scientific publications, his incorporates both Radiocarbon dating and Extinction. The concepts of his Oceanography study are interwoven with issues in Range, Glacial period, Indus, Sediment and Ocean gyre.
The Deep sea study combines topics in areas such as Ecology, Biogeochemical cycle, Coral, δ13C and Holocene. He combines subjects such as Total inorganic carbon, Environmental change, δ18O and Sclerochronology with his study of Dissolved organic carbon. His study in Atmosphere is interdisciplinary in nature, drawing from both Northern Hemisphere, Physical geography, Ocean circulation model, Calibration curve and Earth system science.
Radiocarbon dating, Oceanography, Glacial period, Pacific ocean and Composition are his primary areas of study. His work carried out in the field of Radiocarbon dating brings together such families of science as Atmosphere, Ocean circulation model, Calibration curve and Earth system science. He interconnects Deep sea, Water mass and Thermohaline circulation in the investigation of issues within Glacial period.
The various areas that he examines in his Deep sea study include Abyssal zone, Antarctic Cold Reversal and Holocene. His Thermohaline circulation study incorporates themes from Climate change, Ocean current and Physical oceanography. His Pacific ocean research is multidisciplinary, relying on both Organic matter and Carbon cycle, Biological pump.
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IntCal13 and Marine13 radiocarbon age calibration curves 0-50,000 years cal BP
Paula J Reimer;Edouard Bard;Alex Bayliss;J Warren Beck.
IntCal04 terrestrial radiocarbon age calibration, 0-26 cal kyr BP
Paula J. Reimer;Mike G.L. Baillie;Edouard Bard;Alex Bayliss.
SHCal13 Southern Hemisphere Calibration, 0–50,000 Years cal BP
Alan G Hogg;Quan Hua;Paul G Blackwell;Mu Niu.
The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0-55 cal kBP)
Paula J Reimer;William E N Austin;Edouard Bard;Alex Bayliss.
Abrupt onset and termination of the African Humid Period:rapid climate responses to gradual insolation forcing
Peter deMenocal;Joseph D Ortiz;Tom Guilderson;Jess Adkins.
Quaternary Science Reviews (2000)
Marine04 marine radiocarbon age calibration, 0-26 cal kyr BP
Konrad A Hughen;Mike G L Baillie;Edouard Bard;J Warren Beck.
Radiocarbon calibration curve spanning 0 to 50,000 years BP based on paired 230 Th/ 234 U/ 238 U and 14 C dates on pristine corals
Richard G. Fairbanks;Richard G. Fairbanks;Richard A. Mortlock;Tzu-Chien Chiu;Tzu-Chien Chiu;Li Cao;Li Cao.
Quaternary Science Reviews (2005)
Coherent high- and low-latitude climate variability during the holocene warm period
Peter deMenocal;Joseph D Ortiz;Tom Guilderson;Michael Sarnthein.
Climate change and the collapse of the Akkadian empire: Evidence from the deep sea
H. M. Cullen;P. B. deMenocal;S. Hemming;G. Hemming.
Tropical Temperature Variations Since 20,000 Years Ago: Modulating Interhemispheric Climate Change
Thomas P. Guilderson;Richard G. Fairbanks;James L. Rubenstone.
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