Key figures from the history of research on the Foraminifera of the Chalk Group in the UK
Published:January 01, 2013
Malcolm B. Hart, Haydon W. Bailey, 2013. "Key figures from the history of research on the Foraminifera of the Chalk Group in the UK", Landmarks in Foraminiferal Micropalaeontology: History and Development, A. J. Bowden, F. J. Gregory, A. S. Henderson
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The chalk facies dominates Upper Cretaceous strata in the Anglo-Paris Basin, northern Germany, Poland, southern Sweden, Denmark and the North Sea Basin. The very name of the Cretaceous is derived from ‘creta’, the Latin word for chalk. It is unsurprising, therefore, that some of the earliest uses of micropalaeontology in France and the United Kingdom was to determine the biostratigraphy of the chalk: by Alcide d’Orbigny in France and by staff of the (British) Geological Survey in the UK. This approach was extended, in the 1940s, to the analysis of on-shore, and then offshore, hydrocarbon exploration wells. The continuing interest in the foraminifera of the chalk can be linked to the site investigation for the Channel Tunnel, construction of the Thames Barrier and the development of chalk oilfields in the North Sea Basin. Supporting these interests is a body of research aimed at the understanding of both the overall biostratigraphy of the chalk and some of the key bio-events of the Late Cretaceous: most notably the Cenomanian/Turonian boundary event (OAE ll) and the end-Cretaceous mass extinction.
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Landmarks in Foraminiferal Micropalaeontology: History and Development
This TMS Special Publication comprises a collection of 23 papers with an international authorship reflecting on landmarks in the history and development of Foraminiferal micropalaeontology. The volume is prefaced by an introductory overview that provides a brief and selected historical setting, as well as the intended aims of the book. Selected developments in Foraminiferal studies from a global perspective are presented from the time of Alcide d’Orbignyand the founding of the Paris MNHN collections in the mid-nineteenth century to the use of foraminifera in industry, other museum collections, palaeoceanography and environmental studies, regional studies from the Southern Hemisphere and the riseand fall of significant research schools. The book concludes with a chapter on the modelling of foraminifera. Landmarks in Foraminiferal Micropalaeontology: History and Development will be of particular interest to micropalaeontologists, other Earth scientists, historians of science, museum curators and the general reader with an interest in science.