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Correlation possibilities around the Jurassic/Cretaceous boundary / Ph. J. Hoedemaeker

Hoedemacker, Ph. J. (författare)
Leiden : Rijksmuseum van geologie en mineralogie, 1987
Engelska 55 s.
Serie: Scripta geologica, 0375-7587 ; 84
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  • The present-day detailed knowledge of the zonation and the chronostratigraphic ranges of the fossils of the Mediterranean Berriasian makes it possible to re-evaluate critically the factual evidence on which the correlation of the Boreal sequence with the Tethyan standard is based. It turns out that the evidence is still very meagre and that correlation by means of marine fossils is only possible for time-intervals in which the sea level was high. Some important results of this investigation are: 1) The Valanginian age of the upper Ryazanian: the base of the Tirnovella alpillensis Subzone is stratigraphically closest to, or even coinciding with, the boundary between the lower and the upper Ryazanian and to the base of the German 'Wealden' unit 4. 2) The correlation of the English Cinder Beds with the upper Tithonian Berriasella jacobi Subzone. 3) The time-equivalence of the jacobi Subzone with the lower part of the Canadian Buchia terebratuloides Zone and with at least a part, or even the whole of the underlying Buchia fischeriana Zone, and therefore also with the upper Volgian Taimyroceras taimyrense Zone and with at least the major part, or even the whole, of the Craspedites okensis Zone. 4) The lack of any evidence for the East-European Riasanites rjasanensis Zone being older than the Mediterranean Berriasella paramimouna Subzone or younger than the Berriasella picteti Subzone. 5) The correlation of the Buchia okensis Zone with the lower part of the Berriasella paramimouna Subzone, and possibly with a small part of the Dalmasiceras dalmasi Subzone, but also with an interval in the lower part of the upper Hectoroceras kochi Zone. 6) The entire Riasanites rjasanensis Zone falling within the upper part of the Héctoroceras kochi Zone. 7) The top of the Siberian Chetaites chetae Zone being stratigraphically closest to the top of the Mediterranean Pseudosubplanites grandis Subzone and to the top of the German 'Wealden' unit 1. 

Ämnesord

Stratigraphic correlation  -- Europe (LCSH)
Geology, Stratigraphic  -- Jurassic (LCSH)
Geology, Stratigraphic  -- Cretaceous (LCSH)
Geology  -- Europe (LCSH)
Paleontology  -- Jurassic (LCSH)
Paleontology  -- Cretaceous (LCSH)
Paleontology  -- Europe (LCSH)

Klassifikation

551.766094 (DDC)
Udagfb (kssb/8 (machine generated))
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