-
(Figure 8) Stratigraphic ranges of selected planktonic foraminifers at ODP Ho...
Species abundance: T = trace (one specimen), R = rare (<3%), F = few (3-15%), C = common (16-30%), A = abundant (>30%), P = present, samples with too few planktonic... -
(Table 6) Planktonic foraminifer abundance of ODP Hole 162-982B
DEPTH, sediment is given in mbsf. Abundance estimates as follows: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, - = not found. -
(Table 5) Planktonic foraminifer abundance of ODP Hole 162-982A
DEPTH, sediment is given in mbsf. Abundance estimates as follows: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, - = not found. -
(Table 4) Planktonic foraminifer abundance of ODP Hole 162-981A
DEPTH, sediment is given in mbsf. Abundance estimates as follows: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, - = not found. -
(Table 16A) Occurrences of planktonic foraminifers in DSDP Hole 90-594, sampl...
X = present, - = absent, cf. = confer, R = reworked. -
(Table 14A) Occurrences of planktonic foraminifers in DSDP Hole 90-592, sampl...
X = present, - = absent, cf. = confer. -
Abundance of planktonic foraminifera from IODP Hole 339-U1386C
The base of the Faro contouritic drift (IODP Site U1386) on the northern margin of the Gulf of Cádiz (Algarve margin) is characterized by two sequences of frequent gravity...
