The Jurassic transgression and the mid-late Jurassic succession in Milne Land, central East Greenland

Summary New ammonite finds indicate that the sea transgressed over the crystalline basement of Milne Land, East Greenland, in Boreal Bathonian time and not in Middle Oxfordian as previously thought. A coral ( Enallocoenia callomoni Beauvais) occurring in the transgressive Upper Bathonian deposits is...

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Published in:Geological Magazine
Main Authors: Callomon, J. H., Birkelund, T.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1980
Subjects:
Online Access:http://dx.doi.org/10.1017/s0016756800030442
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800030442
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spelling crcambridgeupr:10.1017/s0016756800030442 2024-09-15T18:04:13+00:00 The Jurassic transgression and the mid-late Jurassic succession in Milne Land, central East Greenland Callomon, J. H. Birkelund, T. 1980 http://dx.doi.org/10.1017/s0016756800030442 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800030442 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 117, issue 3, page 211-226 ISSN 0016-7568 1469-5081 journal-article 1980 crcambridgeupr https://doi.org/10.1017/s0016756800030442 2024-07-24T04:03:32Z Summary New ammonite finds indicate that the sea transgressed over the crystalline basement of Milne Land, East Greenland, in Boreal Bathonian time and not in Middle Oxfordian as previously thought. A coral ( Enallocoenia callomoni Beauvais) occurring in the transgressive Upper Bathonian deposits is the first hermatypic coral known from the Boreal Middle Jurassic. The unusually complete Boreal Upper Callovian–Oxfordian–Kimmeridgian ammonite succession is described; the faunas include remarkable occurrences of submediterranean genera ( Hibolithes, Pachypictonia, Streblites ). Finally, the sedimentary and tectonic evolution of Milne Land and adjacent areas in Jurassic time is outlined. It is shown that the area was characterized by gentle block-faulting. Article in Journal/Newspaper East Greenland Greenland Milne Land Cambridge University Press Geological Magazine 117 3 211 226
institution Open Polar
collection Cambridge University Press
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language English
description Summary New ammonite finds indicate that the sea transgressed over the crystalline basement of Milne Land, East Greenland, in Boreal Bathonian time and not in Middle Oxfordian as previously thought. A coral ( Enallocoenia callomoni Beauvais) occurring in the transgressive Upper Bathonian deposits is the first hermatypic coral known from the Boreal Middle Jurassic. The unusually complete Boreal Upper Callovian–Oxfordian–Kimmeridgian ammonite succession is described; the faunas include remarkable occurrences of submediterranean genera ( Hibolithes, Pachypictonia, Streblites ). Finally, the sedimentary and tectonic evolution of Milne Land and adjacent areas in Jurassic time is outlined. It is shown that the area was characterized by gentle block-faulting.
format Article in Journal/Newspaper
author Callomon, J. H.
Birkelund, T.
spellingShingle Callomon, J. H.
Birkelund, T.
The Jurassic transgression and the mid-late Jurassic succession in Milne Land, central East Greenland
author_facet Callomon, J. H.
Birkelund, T.
author_sort Callomon, J. H.
title The Jurassic transgression and the mid-late Jurassic succession in Milne Land, central East Greenland
title_short The Jurassic transgression and the mid-late Jurassic succession in Milne Land, central East Greenland
title_full The Jurassic transgression and the mid-late Jurassic succession in Milne Land, central East Greenland
title_fullStr The Jurassic transgression and the mid-late Jurassic succession in Milne Land, central East Greenland
title_full_unstemmed The Jurassic transgression and the mid-late Jurassic succession in Milne Land, central East Greenland
title_sort jurassic transgression and the mid-late jurassic succession in milne land, central east greenland
publisher Cambridge University Press (CUP)
publishDate 1980
url http://dx.doi.org/10.1017/s0016756800030442
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800030442
genre East Greenland
Greenland
Milne Land
genre_facet East Greenland
Greenland
Milne Land
op_source Geological Magazine
volume 117, issue 3, page 211-226
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0016756800030442
container_title Geological Magazine
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