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(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) Occurrence of Lower Cretaceous planktonic foraminifera in ODP Hole...
Sediment depth is given in mbsf. Abundance estimates as follows: - = not found, R = rare, F = few, C = common, A = abundant. -
(Table T4) Occurrence of Lower Cretaceous planktonic foraminifera in ODP Hole...
Sediment depth is given in mbsf. Abundance estimates as follows: - = not found, R = rare, F = few, C = common, A = abundant. -
(Table S1) Late Albian foraminiferal carbon and oxygen isotope data from ODP ...
This dataset has no description
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Stable carbon and oxygen isotope record of Cretaceous planktonic foraminifera...
The Cretaceous Heterohelix moremani (Cushman) was the only biserial planktonic foraminiferal species from its first appearance in the late Albian up to the Cenomanian/Turonian... -
Stable oxygen and carbon isotope ratios for Early to Middle Cretaceous benthi...
Stable isotopic measurements have been made on planktonic and benthic foraminifera of Early to mid-Cretaceous (Early Albian-Cenomanian) age from DSDP site 463 located in the... -
Range table from planktonic foraminifers in ODP Hole 171-1050C
This dataset has no description
