His main research concerns Paleontology, Thermoluminescence dating, Chronology, Holocene and Sedimentary rock. His study ties his expertise on Sea level together with the subject of Paleontology. His Thermoluminescence dating research includes elements of Younger Dryas and Isotopes of oxygen.
His studies deal with areas such as Radiocarbon dating and Geomorphology as well as Chronology. His work deals with themes such as Cave and Fluvial, which intersect with Quaternary. His work carried out in the field of Glacial period brings together such families of science as Aeolian processes and Ice sheet.
His scientific interests lie mostly in Paleontology, Holocene, Quaternary, Oceanography and Aeolian processes. Much of his study explores Paleontology relationship to Ice sheet. His study looks at the relationship between Holocene and fields such as Period, as well as how they intersect with chemical problems.
Mark D. Bateman works mostly in the field of Quaternary, limiting it down to topics relating to Fluvial and, in certain cases, Colluvium. His Aeolian processes research is multidisciplinary, incorporating elements of Sedimentary rock, Deposition, Sediment and Younger Dryas. His study in Chronology is interdisciplinary in nature, drawing from both Radiocarbon dating, Ridge and Thermoluminescence dating.
Mark D. Bateman mainly focuses on Ice sheet, Glacial period, Physical geography, Holocene and Oceanography. His Ice sheet study integrates concerns from other disciplines, such as Bedrock, Paleontology, Deglaciation and Moraine. All of his Paleontology and Fluvial and Pleistocene investigations are sub-components of the entire Paleontology study.
The various areas that he examines in his Physical geography study include Period and Aeolian processes. Mark D. Bateman has included themes like Sand dune stabilization, Quaternary, Sea level and Later Stone Age in his Holocene study. His Quaternary research is multidisciplinary, relying on both Coastal plain, Optically stimulated luminescence and Arctic.
Mark D. Bateman mainly investigates Paleontology, Glacial period, Quaternary, Sedimentary rock and Ice sheet. His Paleontology study frequently draws connections between related disciplines such as Shetland. The Glacial period study combines topics in areas such as Continental shelf, Oceanography, Sea level and Headland.
His biological study spans a wide range of topics, including Physical geography, Aeolian processes and Optically stimulated luminescence. His Sedimentary rock study combines topics from a wide range of disciplines, such as Feature, Outcrop, Seafloor spreading, Archaeological evidence and Archaeological research. His Ice sheet research integrates issues from Glacial lake, Ice divide, Bedrock, Glacial landform and Last Glacial Maximum.
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Map and GIS database of glacial landforms and features related to the last British Ice Sheet
Chris D. Clark;David J. A. Evans;Anjana Khatwa;Tom Bradwell.
Identification of Younger Dryas outburst flood path from Lake Agassiz to the Arctic Ocean
Julian B. Murton;Mark D. Bateman;Scott R. Dallimore;James T. Teller.
Investigations into the potential effects of pedoturbation on luminescence dating
Mark D Bateman;Charles D Frederick;Manoj K Jaiswal;Ashok K Singhvi.
Quaternary Science Reviews (2003)
Detecting post-depositional sediment disturbance in sandy deposits using optical luminescence
Mark D. Bateman;Claire H. Boulter;Andrew S. Carr;Charles D. Frederick.
Quaternary Geochronology (2007)
Tsunami sedimentation associated with the Lisbon earthquake of 1 November AD 1755: Boca do Rio, Algarve, Portugal
A.G. Dawson;R. Hindson;C. Andrade;C. Freitas.
The Holocene (1995)
Luminescence dating of loess–palaeosol sequences and coversands: methodological aspects and palaeoclimatic implications
A.K. Singhvi;A.K. Singhvi;A. Bluszcz;M.D. Bateman;M.Someshwar Rao.
Earth-Science Reviews (2001)
An absolute chronology for the raised beach and associated deposits at Sewerby, East Yorkshire, England
M. D. Bateman;J. A. Catt.
Journal of Quaternary Science (1996)
Aeolianite and barrier dune construction spanning the last two glacial–interglacial cycles from the southern Cape coast, South Africa
Mark D. Bateman;Peter J. Holmes;Andrew S. Carr;Benjamin P. Horton.
Quaternary Science Reviews (2004)
Preserving the palaeoenvironmental record in Drylands: Bioturbation and its significance for luminescence-derived chronologies
M.D. Bateman;C.H. Boulter;A.S. Carr;C.D. Frederick.
Sedimentary Geology (2007)
Late Pleistocene wetting and drying in the NW Kalahari: an integrated study from the Tsodilo Hills, Botswana
David S.G Thomas;George Brook;Paul Shaw;Mark Bateman.
Quaternary International (2003)
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