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Foraminifera census counts at salt-marsch archive GeoHH-FK (Friedrichskoog, s...
Here we have evaluated and compared two benthic foraminiferal records derived from sedimentary salt-marsh archives from the south-eastern North Sea coast, covering the past ~100... -
(Table S2) Stable oxygen and carbon isotope data and reconstructed paleo sea ...
This dataset has no description
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(Tab. 7) Occurence of microfossils in Late Jurassic sediments of DSDP Hole 50...
R = rare (1-5 specimens), C = common (6-20 specimens), A = abundante (significant occurence). Samples 50-416A-7-1,120-125, 50-416A-10-2,111-113, 50-416A-11-4,16-18,... -
(Table 3) Stable isotope record of Cretaceous foraminifera from DSDP Hole 44-...
Mid-Cretaceous (Barremian-Turonian) plankton preserved in deep-sea marl, organic-rich shale, and pelagic carbonate hold an important record of how the marine biosphere responded... -
Foraminifera abundance of Hole 61-462
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 22-217
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 2-10
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table 1) Oxygen and carbon isotopic values for planktonic and benthic forami...
This dataset has no description
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(Figure 10) Distribution of Cretaceous planktonic foraminifers and associated...
Species abundance: A = abundant, AF = frequent, C = common, F = few, R = rare, small case letters = reworked, cf. = confirm, ? = presence is questionable, - = absent. -
(Figure 9) Distribution of Cretaceous planktonic foraminifers and associated ...
Species abundance: A = abundant, AF = frequent, C = common, F = few, R = rare, small case letters = reworked, cf. = confirm, ? = presence is questionable, - = absent. -
(Figure 8c) Distribution of Cretaceous planktonic foraminifers, calpellionids...
Species abundance: A = abundant, AF = frequent, C = common, F = few, R = rare, small case letters = reworked, cf. = confirm, ? = presence is questionable, - = absent. -
(Figure 8b) Distribution of Cretaceous planktonic foraminifers, calpellionids...
Species abundance: A = abundant, AF = frequent, C = common, F = few, R = rare, small case letters = reworked, cf. = confirm, ? = presence is questionable, - = absent. -
(Figure 8 a) Distribution of Cretaceous planktonic foraminifers and associate...
Species abundance: A = abundant, AF = frequent, C = common, F = few, R = rare, small case letters = reworked, cf. = confirm, ? = presence is questionable, - = absent. -
(Table 2) Distribution and relative abundance of mid-Cretaceous planktonic fo...
Abundances: Based on 300-specimen counts. A = abundant (25%), C = common (5-25%), R = rare (1-5%), V = very rare (1%), - = absent, ? = questionable occurrence, cf. = confer,... -
(Table 1) Distribution and relative abundance of mid-Cretaceous planktonic fo...
Abundances: Based on 300-specimen counts. A = abundant (25%), C = common (5-25%), R = rare (1-5%), V = very rare (1%), - = absent, ? = questionable occurrence, cf. = confer,... -
(Table T5) Planktic foraminiferal assemblages in sediments of ODP Hole 198-12...
This dataset has no description
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(Figure 3) Distribution of planktonic foraminifers in the Upper Cretaceous of...
Species abundance: C = common, F = few, R = rare,VR = very rare, - = not observed. -
(Figure 2) Distribution of planktonic foraminifers in the Albian of DSDP Hole...
Species abundance: C = common, F = few, R = rare, VR = very rare, - = not observed. The Albian section is assumed to begin between Samples 71-511-49-5,102-104 and... -
(Table 2) Relative abundances of planktic foraminifera across the K/T transit...
This dataset has no description
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(Table 1) Relative abundances of planktic foraminifera across the K/T transit...
size fraction >63 µm except for the laminated interval with 1 cm sample intervals across the K/T boundary, where the >38 µm size fraction was used
