The mid-Cenomanian eustatic low

Hancock, J.

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The mid-Cenomanian eustatic low

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Hancock J.

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Abstrakty

Through much of the earlier part of the Middle Cenomanian the sea-levels in western Asia, northern Europe and the Western Interior of the U.S.A. were lower than during the later Early Cenomanian and most of the later Middle Cenomanian. In north-west Europe the first sign of this Mid-Cenomanian Eustatic Low was just before the end of the Zone of Cunningtoniceras inerme. There was then an abrupt and strong fall of sea-level at the base of Milankovitch couplet C 1, early in the Subzone of Turrilites costatus. Sea-level continued to be low through couplets C 1 to C 3 for some 60,000 years: this is the Mid-Cenomanian Regressive Trough. In western Germany it has been distinguished as the Primus Event. In north Texas and the Western Interior of the U.S.A. the Trough occurred in the Zone of Conlinoceras tarrantense which can be dated as 95.78 [plus-minus] 0.61 Ma.A later regressive trough occurred at the start of the Subzone of Turrilites acutus, which is marked by the Mid-Cenomanian Event in Germany. The overall lower sea-level from late in the Zone of C. inerme to early in the Subzone of T. acutus is the Mid-Cenomanian Eustatic Low. It lasted some 300,000 years.

Słowa kluczowe

Anglo-Paris Basin Cenomanian Colorado Mid-Cenomanian Event Munster Basin north Texas Primus Event South Dakota T. costatus Subzone

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2004

Tom

Vol. 54, no. 4

Strony

611--627

Opis fizyczny

Bibliogr. 94 poz.

Twórcy

autor

Hancock J.

Department of Earth Science and Engineering, Royal School of Mines, Imperial College, London SW7 2BP, U.K.

Bibliografia

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