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- W1993708614 abstract "The Cenomanian-Turonian boundary event has been fully documented from a series of localities between Flamborough Head in Humberside and Marham in Norfolk. The carbon isotope excursion can be identified and extrapolated to all the studied sections using bed-by-bed correlation. Evidence from studies of the isotope data, trace element geochemistry, and the micropalaeontology are discussed. The famous 'Black Band' is seen to change laterally into a 'red' horizon and then a 'green' horizon when traced southwards. This appears to represent the 'feather-edge' of the anoxic event which dies out when traced towards a palaeo-high, which appears to have been located in the region of the Wash. The 'Black Band' itself is a result of high levels of preferential preservation of organic material and dinoflagellate cysts, although the flora indicates a stressed environment. The planktonic and benthonic foraminifers are variously affected by the event, with faunal changes being traced throughout the region. A correlation with the events described by Jarvis et al., (1988, Cretaceous Research) will be demonstrated." @default.
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- W1993708614 date "1993-08-01" @default.
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- W1993708614 title "The late Cenomanian Event in eastern England" @default.
- W1993708614 doi "https://doi.org/10.1006/cres.1993.1035" @default.
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