Discussion on estimates of the amount and rate of sea-level change across the rhaetian-hettangian and pliensbachian-toarcian boundaries (latest triassic to early jurassic)

Journal of the Geological Society

Volumn 155, Issue 2, 1998, Pages 421-422

  Cope, John C W ^a   Hallam, A ^b  

^a CARDIFF UNIVERSITY   (United Kingdom)

^b UNIVERSITY OF BIRMINGHAM   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0000853345     PISSN: 00167649     EISSN: None     Source Type: Journal    
DOI: 10.1144/gsjgs.155.2.0421     Document Type: Note

References (8)

1. BRINKMANN, R. 1929. Statistisch-biostratigraphische Untersuchungen an mitteljurassischen Ammoniten über Artebegriff und Stammesentwicklung. Abhandlungen der Gesellschaft der Wissenschaft, Göttingen, mathematische und physische Klasse. N. F. 13.
2. COPE, J. C. W. 1993. High resolution biostratigraphy. In: HAILWOOD, E. A. & KIDD, R. B. (eds) High Resolution Stratigraphy. Geological Society, London, Special Publications, 70, 257-265.
3. GRADSTEIN, F. M., AGTERBERG, F. P., OGG, J. G., HARDENBOL, J., VAN VEEN, P., THIERRY, J. & HUANG, Z. 1994. A Mesozoic time scale. Journal of Geophysical Research, 99, B12, 24 051-24 074.
4. HALLAM, A. 1967. An environmental study of the Upper Domerian and Lower Toarcian in Great Britain. Philosophical Transactions of the Royal Society, London, B252, 393-445.
5. HALLAM, A. 1997. Estimates of the amount and rate of sea-level change across the Rhaetian-Hettangian and Pliensbachian-Toarcian boundaries (latest Triassic to early Jurassic). Journal of the Geological Society, London, 154, 773-779.
6. HARLAND, W. B., ARMSTRONG, R. L., COX, A. V., CRAIG, L. E., SMITH, A. G. & SMITH, D. G. 1990. A geologic time scale 1989. Cambridge University Press.
7. HOWARTH, M. K. 1992. The ammonite family Hildoceratidae in the Lower Jurassic of Great Britain. Monograph of the Palaeontographical Society, London.
8. SNELLING, N. J. (ed.) 1985. The chronology of the geological record. Geological Society of London, Memoir,10