-
(Figure 3) Distribution of planktonic foraminifers in the Upper Cretaceous of...
Species abundance: C = common, F = few, R = rare,VR = very rare, - = not observed. -
(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,... -
(Figure 3) Distribution chart of creatceous planktonic foraminifera of ODP Ho...
species abundance: A = abundant, C = common, F = few, R = rare, P = present, - = absent, ? = questionable -
(Figure 2) Distribution chart of creatceous planktonic foraminifera of ODP Ho...
species abundance: A = abundant, C = common, F = few, R = rare, P = present, - = absent -
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...
