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Carboniferous biostratigraphy of the Rookhope Borehole, Co. Durham

Published online by Cambridge University Press:  03 November 2011

G. A. L. Johnson  and
J. R. Nudds
G. A. L. Johnson
Affiliation:
Department of Geological Sciences, University of Durham, Science Laboratories, South Road, Durham DH1 3LE
J. R. Nudds
Affiliation:
The Manchester Museum, University of Manchester, Oxford Road, Manchester M13 9PL
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Abstract

A deep borehole drilled at Rookhope in Weardale, Co. Durham in 1960–61 proved the Weardale Granite below Carboniferous sediments at a depth of 390 m; an account of the Carboniferous rocks is presented. The boring commenced in the basal Namurian Great Limestone and entered the Dinantian at the bottom of the limestone at 25 m. Most of the ten Brigantian cyclothems sectioned in the borehole are compound and average 30 m thick. They consist of an initial cycle often more than 20 m thick and overlying minor cycles that are usuallyless than 6 m thick. Each of the cycles, both initial and minor, are coarsening upwards sequences from marine limestone or mudstohe to deltaic and fluvial mudstone, sandstone, seatearth and occasionally a thin coal seam. The underlying Asbian consists of seven cyclothems averaging 8 m thick. By contrast they are simple coarsening upwards sequences similar to the Brigantian initial cycles, but no minor cycles are developed.

Marine fossils are abundant in the majority of cyclothems and are listed against their stratigraphical horizon in the borehole. Special studies of miospores, conodonts and foraminiferans from the borehole are presented. A consensus of biostratigraphical evidence shows that the base of the Carboniferous succession in the borehole is of early Asbian age.

Keywords

basal Namurianupper Dinantiancyclothemsinitial cyclesminor cyclesfossilspalaeogeographypalaeoecologystratigraphical palaeontology.

Information

Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 86 , Issue 3 , 1995 , pp. 181 - 226
Copyright
Copyright © Royal Society of Edinburgh 1995

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