-
(Figure 6) Occurrence of planktonic foraminifers and other selected constitue...
Species abundance: A = abundant, C = common, F = few, R = rare, ? = questionable occurrence, - = absent. -
(Figure 4) Occurrence of planktonic foraminifers and other selected constitue...
Species abundance: A = abundant, C = common, F = few, R = rare, ? = questionable occurrence, - = absent. -
(Figure 3) Occurrence of planktonic foraminifers and other selected constitue...
Species abundance: A = abundant, C = common, F = few, R = rare, ? = questionable occurrence, - = absent. -
(Table 6) Occurrence and estimated abundance of planktonic foraminifers at DS...
A = abundant (>10% of assemblage); C = common (3-10%); F = few (0.5-3%); R = rare (<0.5%); T = trace; - = not found; (L) = left coiling; (R) = right coiling. -
(Table 5) Occurrence and estimated abundance of planktonic foraminifers at DS...
A = abundant (>10% of assemblage); C = common (3-10%); F = few (0.5-3%); R = rare (<0.5%); T = trace; - = not found; (L) = left coiling; (R) = right coiling. -
(Table 4) Occurrence and estimated abundance of planktonic foraminifers at DS...
A = abundant (>10% of assemblage); C = common (3-10%); F = few (0.5-3%); R = rare (<0.5%); T = trace; - = not found. Species looked for and not found: Globigerina... -
(Table 3B) Occurrence and estimated abundance of planktonic foraminifers at D...
A = abundant (>10% of assemblage); C = common (3-10%); F = few (0.5-3%); R = rare (<0.5%); T = trace; - = not found; (L) = left coiling; (R) = right coiling. -
(Table T5) Planktonic foraminifera abundance of ODP Hole 170-1043A sediments
Sediment depth is given in mbsf. <0.1 = trace (counts <50 specimens in sample). -
(Table T2) Abundance of stratigraphically important planktonic foraminifera i...
Sediment depth is given in mbsf. Abundance estimates as follows: VA = very abundant (>20%), A = abundant (10%-19%), C = common (5%-9%), R = rare (<5%), + = present, - =... -
(Table 10) Distribution of planktonic foraminifera in the middle to late Mioc...
Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present. -
(Table 4) Distribution and abundance of selected planktonic foraminifera of t...
Species abundaces: C = common, R = rare, - = absent. ? = questionable occurrence. -
(Figure 7) 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... -
(Figure 6) 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... -
(Figure 5) 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... -
(Figure 10) Stratigraphic ranges of selected planktonic foraminifers at ODP H...
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... -
(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 1) Range table of planktonic foraminifers from ODP Hole 166-1006A sedi...
This dataset has no description
-
(Table 3) Distribution and abundance of selected planktonic foraminifera of t...
Species abundaces: C = common, R = rare, + = present, - = absent. ? = questionable occurrence. -
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... -
Abundances of shells of planktic foraminifera species in Upper Miocene sedime...
Locations of climatic zones at four time intervals during Miocene are reconstructed from ranges of planktic foraminifera shells in Miocene deposits of the Indian Ocean. Gradual...
