What is he best known for?
The fields of study he is best known for:
- Paleontology
- Erosion
- Sedimentary rock
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 most cited work include:
- Map and GIS database of glacial landforms and features related to the last British Ice Sheet (196 citations)
- Identification of Younger Dryas outburst flood path from Lake Agassiz to the Arctic Ocean (175 citations)
- Investigations into the potential effects of pedoturbation on luminescence dating (154 citations)
What are the main themes of his work throughout his whole career to date?
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.
He most often published in these fields:
- Paleontology (33.15%)
- Holocene (24.46%)
- Quaternary (22.28%)
What were the highlights of his more recent work (between 2018-2021)?
- Ice sheet (17.39%)
- Glacial period (19.57%)
- Physical geography (15.76%)
In recent papers he was focusing on the following fields of study:
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.
Between 2018 and 2021, his most popular works were:
- Long-term sediment decline causes ongoing shrinkage of the Mekong megadelta, Vietnam. (11 citations)
- The Holocene humid period in the Nefud Desert: Hunters and herders in the Jebel Oraf palaeolake basin, Saudi Arabia (8 citations)
- A chronology for North Sea Lobe advance and recession on the Lincolnshire and Norfolk coasts during MIS 2 and 6 (8 citations)
In his most recent research, the most cited papers focused on:
- Paleontology
- Erosion
- Sedimentary rock
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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