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Cenomanian-Turonian foraminifera, radiolarians and calcispheres abundance fro...
This dataset has no description
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Late Cretaceous planktonic foraminifera distributionof IODP Site 369-U1513
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Late Cretaceous planktonic and benthic foraminifera stable isotopes data from...
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(Figure 3) Distribution of latest Aptian and Cenomanian-Turonian planktonic f...
X = present, ? quetionable occurrence, r = reworked, - = absent. -
(Table 2) Distribution of planktonic foraminifera in the upper Turonian-lower...
Abundances: AA = very abundant (dominant); A = abundant (>50 %); C = common (15-30 spedimens); F = few (5-15 specimens); R = rare (2-5 specimens); VR = very rare (1... -
(Table 1) Distribution of planktonic foraminifera in the upper Turonian-lower...
Abundances: AA = very abundant (dominant); A = abundant (>50 %); C = common (15-30 spedimens); F = few (5-15 specimens); R = rare (2-5 specimens); VR = very rare (1... -
(Table 3) Distribution of planktonic foraminifera in ODP Hole 183-1138A, Part...
cf. = uncertain identification, transitional forms, ? = questionable identification. -
(Table 1) Distribution of planktonic foraminifera in ODP Hole 183-1135A, Part II
Abundances: AA = very abundant (>40%), A = abundant (26-39%), C = common (16-25%), F = few (6-15%), R = rare (2-5%), VR = very rare (<2%), cf. = uncertain identification,... -
Distribution of late Turronian planktonic foraminifers in ODP Hole 114-700B
The oldest Cretaceous sediments in the subantarctic region were recovered from ODP Hole 700B in the East Georgia Basin. Planktonic foraminifers from the deepest indurated... -
Range table from planktonic foraminifers in ODP Hole 143-869B
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