Lyell Collection

Journal of the Geological Society

Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help


Keywords:
Author:
Advanced search>>
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by CRAME, J. A.
Right arrow Articles by RIDING, J. B.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Journal of the Geological Society; 1999; v. 156; issue.5; p. 957-964;
DOI: 10.1144/gsjgs.156.5.0957
© 1999 Geological Society of London

Article

Strontium isotope correlation of the basal Maastrichtian Stage in Antarctica to the European and US biostratigraphic schemes

J. A. CRAME1, J. M. McARTHUR2, D. PIRRIE3 & J. B. RIDING4

1 British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK (e mail: A.Crame{at}bas.ac.uk)
2 Department of Geological Sciences, University College, London, Gower Street, London WC1E 6BT, UK (e mail: j.mcarthur{at}ucl.ac.uk)
3 Camborne School of Mines, University of Exeter, Redruth, Cornwall TR15 3SE, UK (e mail: d.pirrie{at}csm.ex.ac.uk)
4 British Geological Survey, Keyworth, Nottingham NG12 5GG, UK (e mail: jbr{at}bgs.ac.uk)

New 87Sr/86Sr dating allows the correlation of a marker horizon within the prolific Late Cretaceous Gunnarites antarcticus faunal assemblage of the Cape Lamb Member, Snow Hill Island Formation, Vega Island, Antarctica with reference sections in Europe and the USA. This horizon is between 81.5 and 96.5 m above the base of the G antarcticus assemblage. Replicate analysis of six macrofossils from within it yielded a mean value for 87Sr/86Sr of 0.707 735 9 ± 0.000 004 3 (± 2 s.e., n=17). This ratio in turn yields a numerical age of 71.0 ± 0.2 Ma when compared to the standard 87Sr/s6Sr reference curve for the latest Cretaceous, for which the Campanian-Maastrichtian boundary is placed at 71.3 ± 0.5 Ma. The value of 0.707 735 9 ± 0.000 004 3 correlates to a level in the Belemnella lanceolata belemnite Zone of the Chalk of northwestern Germany that is 2.5 ± 5 m beneath the base of the overlying B. pseudobtusa Zone (and 7.5 m above the Campanian-Maastrichtian belemnite boundary), and to an interval within the ammonite zonation of the US Western Interior that spans the early Maastrichtian Baculites baculus and B. eliasi zones, but with a most likely level within the B. eliasi Zone. An earliest Maastrichtian age is thereby determined for the Antarctic horizon, and indeed for the entire G. antarcticus assemblage. Gunnarites, sensu lato, is an important ammonite marker for the base of the Maastrichtian throughout the southern high-latitude regions, and the associated large heteromorph ammonite Diplomoceras may comprise a macrofossil link back to the Maastrichtian type sections.

Key Words: 87Sr/86Sr • Maastrichtian • Antarctica • USA • Europe • correlation




This article has been cited by other articles:


Home page
Geological Society, London, Special PublicationsHome page
J. A. Crame, D. Pirrie, and J. B. Riding
Mid-Cretaceous stratigraphy of the James Ross Basin, Antarctica
Geological Society, London, Special Publications, 2006; 258: 7 - 19.
[Abstract] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
J. Kriwet, J. M. Lirio, H. J. Nunez, E. Puceat, and C. Lecuyer
Late Cretaceous Antarctic fish diversity
Geological Society, London, Special Publications, 2006; 258: 83 - 100.
[Abstract] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
J. E. Martin and J. A. Crame
Palaeobiological significance of high-latitude Late Cretaceous vertebrate fossils from the James Ross Basin, Antarctica
Geological Society, London, Special Publications, 2006; 258: 109 - 124.
[Abstract] [PDF]