Aspects of mid-Cretaceous stratigraphical micropalaeontology
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Aspects of mid-Cretaceous stratigraphical micropalaeontology

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Published by British Museum (Natural History) in London .
Written in English

Subjects:

Places:

  • England.,
  • France.

Subjects:

  • Foraminifera, Fossil.,
  • Paleontology -- Cretaceous.,
  • Geology, Stratigraphic -- Cretaceous.,
  • Micropaleontology -- England.,
  • Micropaleontology -- France.

Book details:

Edition Notes

StatementD. J. Carter & M. B. Hart.
SeriesBulletin of the British Museum (Natural History)., v. 29, no. 1
ContributionsHart, M. B., joint author.
Classifications
LC ClassificationsQE1 .B65 vol. 29, no. 1, QE772 .B65 vol. 29, no. 1
The Physical Object
Pagination135 p. :
Number of Pages135
ID Numbers
Open LibraryOL4287926M
LC Control Number78314876

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Abstract. The subgeneric arenobuliminid classification of Voloshina (, ) is followed, whereby the genus Vialovella is recognised (with a new species, V. praefrankei, ancestral to Crenaverneuilina frankei), and Arenobulimina (Arenobulimina), Arenobulimina (Harena) and Arenobulimina (Pasternakia) are agreed ulimina (Hagenowella) is employed Cited by: 6. Micropalaeontology and stratigraphical setting of the Cambridge Greensand. For a hothouse Earth such as the mid-Cretaceous, humid-arid climate cycles controlling groundwater-related sea . Members of the Globigerinida constitute up to 10 per cent of the Zooplankton in the oceans and may exceed 60 per cent in certain areas in summer (King and Desmond, ). Although they accumulate very slowly their microscopic, dead shells have laid down a blanket of ‘Globigerina Ooze’ on the deep ocean floor. PDF | On Dec 1, , Hart M.D. and others published A history of academic research on Foraminifera in the UK | Find, read and cite all the research you need on ResearchGate.

Full text of "Mesozoic and Cenozoic stratigraphical micropalaeontology of the Dorset coast and Isle of Wight, southern England: field guide for the an Micropalaeontological Colloquium" See other formats >S M MICROPALAEONTOLOGICAL SOCIETY = MICROPALAEONTOLOGY OF THE DORSET COAST AND = ISLE OF WIGHT SOUTHERN . The mid-Cretaceous geological history of the central North Sea is described and related to that of the surrounding onshore and offshore areas of North West Europe. An overall transgression during the Albian to latest Cenomanian/early Turonian was followed by a brief regression and associated erosion later in the early Turonian. An additional use for this book may arise as many micropalaeontology courses do not cover radiolarians due to a lack of specialists to teach and so this volume could be used by any competent micropalaeontologist to put together a very complete course. divided into 13 chapters) is devoted to early and mid Cretaceous taxa. Chapter 3 forms a.   The “Albian transgression” is a regional event in NW Europe which is important for understanding the pattern of basin evolution during Early and “Mid” Cretaceous times. It is also important because the diachronous coarse clastics associated with the transgression may prove to be of important reservoir potential in the southern North Sea.

Stratigraphy of Mid-Cretaceous Formations at Drilling Sites in Weston and Johnson Counties, Northeastern Wyoming By E. A. MEREWETHER PALEONTOLOGY AND STRATIGRAPHY OF MID-CRETACEOUS ROCKS- NORTHEASTERN WYOMING GEOLOGICAL SURVEY PROFESSIONAL PAPER A A description and comparison of theCited by: 5. International Symposium on the Cretaceous System Page | 4 • Cretaceous volcanic and tectonic processes • Cretaceous Geochemistry, stable isotopes, etc. • Chalk of the North Sea Basin and adjacent areas (stratigraphy, micropalaeontology, diagenesis, exploration, biosteer ing, etc.) • . Cambridge Core - Palaeontology and Life History - Foraminifera and their Applications - by Robert Wynn JonesCited by: *** Limited stocks available. The papers in this volume cover surface and subsurface rocks from a wide range of stratigraphic ages and sedimentary environment, but in addressing the application of sequence stratigraphy to British geology, this book focuses on diverse aspects of sequence stratigraphy that tend to cut across divisions based on depositional environments or age alone. .