2007
DOI: 10.1111/j.1755-6724.2007.tb01029.x
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Abstract: Cretaceous oceanic red beds (CORBs) represented by red shales and mark, were deposited during the Cretaceous and early Paleocene, predominantly in the Tethyan realm, in lower slope and abyssal basin environments. Detailed studies of CORBs are rare; therefore, we compiled CORBs data from deep sea ocean drilling cores and outcrops of Cretaceous rocks subaerially exposed in southern Europe, northwestern Germany, Asia and New Zealand. In the Tethyan realm, CORBs mainly consist of reddish or pink shales, limestones… Show more

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Cited by 14 publications
(1 citation statement)
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“…In the studied sections, and, in general, in the Umbria‐Marche and Belluno Basins, periods of low intensity of bottom currents correspond to a color shift from light grey/whitish calcilutites/marlstones to reddish hematite‐rich micritic limestones/marlstones above both the Bonarelli Level and the post‐OAE 1d Pialli Level (Figures , , and ). This confirms a change in clay input and a general increase in oxygenation of bottom waters, during periods of mild bottom circulation [ Xi et al, ; Hu et al, ; Neuhuber and Wagreich , ; Wang et al, ], originated at temperate source areas with downwelling of cooler waters.…”
Section: Discussionmentioning
confidence: 99%
“…In the studied sections, and, in general, in the Umbria‐Marche and Belluno Basins, periods of low intensity of bottom currents correspond to a color shift from light grey/whitish calcilutites/marlstones to reddish hematite‐rich micritic limestones/marlstones above both the Bonarelli Level and the post‐OAE 1d Pialli Level (Figures , , and ). This confirms a change in clay input and a general increase in oxygenation of bottom waters, during periods of mild bottom circulation [ Xi et al, ; Hu et al, ; Neuhuber and Wagreich , ; Wang et al, ], originated at temperate source areas with downwelling of cooler waters.…”
Section: Discussionmentioning
confidence: 99%