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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Atlantic Ocean
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North Atlantic
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Gulf of Maine (1)
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Australasia
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New Zealand
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Otago New Zealand (1)
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Canada
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Eastern Canada
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Maritime Provinces
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New Brunswick (1)
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Europe
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Western Europe
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United Kingdom
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Great Britain
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England
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Devon England (1)
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Outer Banks (1)
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South Island (1)
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United States
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Atlantic Coastal Plain (1)
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Delaware
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Kent County Delaware (1)
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Maine
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Hancock County Maine (1)
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Sagadahoc County Maine (1)
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Washington County Maine (2)
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York County Maine (2)
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North Carolina
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Carteret County North Carolina (1)
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Dare County North Carolina (1)
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Pamlico Sound (1)
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elements, isotopes
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carbon
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C-14 (4)
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isotopes
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radioactive isotopes
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C-14 (4)
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fossils
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Invertebrata
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Protista
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Foraminifera (3)
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Thecamoeba (1)
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microfossils (3)
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geologic age
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Cenozoic
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Quaternary
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Holocene
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upper Holocene (2)
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Pleistocene
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upper Pleistocene (1)
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upper Quaternary (1)
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Laurentide ice sheet (1)
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Primary terms
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absolute age (4)
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Atlantic Ocean
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North Atlantic
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Gulf of Maine (1)
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Australasia
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New Zealand
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Otago New Zealand (1)
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Canada
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Eastern Canada
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Maritime Provinces
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New Brunswick (1)
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carbon
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C-14 (4)
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Cenozoic
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Quaternary
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Holocene
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upper Holocene (2)
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Pleistocene
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upper Quaternary (1)
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continental shelf (1)
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earthquakes (1)
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Europe
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Western Europe
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United Kingdom
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England
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Devon England (1)
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faults (1)
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geodesy (1)
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geomorphology (1)
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glacial geology (1)
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Invertebrata
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Protista
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Foraminifera (3)
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Thecamoeba (1)
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isostasy (1)
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isotopes
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radioactive isotopes
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C-14 (4)
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sea-level changes (6)
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sediments
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marine sediments (1)
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peat (2)
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shorelines (1)
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tectonics
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neotectonics (1)
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United States
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Atlantic Coastal Plain (1)
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Delaware
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Kent County Delaware (1)
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Maine
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Hancock County Maine (1)
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Sagadahoc County Maine (1)
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Washington County Maine (2)
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York County Maine (2)
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North Carolina
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Carteret County North Carolina (1)
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Dare County North Carolina (1)
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Pamlico Sound (1)
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sediments
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sediments
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marine sediments (1)
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peat (2)
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Contemporary Salt-Marsh Foraminifera from Southern California and Implications for Reconstructing Late Holocene Sea-Level Changes
Resolving Uncertainties in Foraminifera-Based Relative Sea-Level Reconstruction: a Case Study from Southern New Zealand
Abstract The academic study of foraminifera began as the pursuit of the ‘gentleman naturalist’ in the nineteenth century, only becoming a professional occupation with the employment of micropalaeontologists by the (British) Geological Survey. The formal training of micropalaeontologists in British universities (and polytechnics) really began in the 1940s (post-World War ll) and much of this history can be traced back to Alan Wood and the employment predictions of F. R. S. Henson. Wood, either directly or indirectly, began the teaching of micropalaeontology at Imperial College (London), Aberystwyth and University College (London), and these three centres went on to develop and nurture the expertise we see in a wide range of schools and departments today. The rise, and fall, of MSc and MRes courses in UK geoscience departments is described, as well as the wide range of locations at which PhD training and research is undertaken. Much of this history can be related to the development of oil exploration, in the North Sea Basin and worldwide, and the need for suitably qualified personnel.