Dataset - B2FIND

(Table 4) Distribution of planktonic foraminifers in ODP Hole 108-658A

Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent.

(Table 3) Distribution of planktonic foraminifers in ODP Hole 108-657A

Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent.

(Table 1) Distribution of selected planktonic foraminifer species in dissolut...

As dissolution-affected faunas are always small and contain at most a few specimens of each species, only presence (X) or absence (-) of species are indicated.

(Figure 3) Stratigraphic distribution of planktonic foraminifera in the Neoge...

X = present, r = reworked, - = absent

(Figure 2) Stratigraphic distribution of planktonic foraminifera in the Neoge...

X = present, r = reworked, - = absent

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...

(Table 1) Planktonic foraminiferal communities at DSDP Holes 94-609B and 94-609

The planktonic foraminifers in 124 samples from Holes 609 and 609B have been analyzed quantitatively to see whether oceanographic events in the late Miocene and early Pliocene...

(Table 2) Relative abundance of planktonic foraminifera species in Pliocene -...

Planktonic foraminifera from Pliocene - Early Quaternary sediments of ODP Hole 111-677A were studied in detail. It was shown that the majority of detected zonal taxa are...

Distribution of planktonic foraminifera in DSDP Hole 31-296 (Table III)

Late Neogene planktonic foraminiferal biostratigraphy of DSDP Site 296, Leg 31, reveals this site as an ideal reference section for correlation of Blow's low-latitude zonation...

Occurrence of planktic foraminifera in Pliocene to Holocene sediments of DSDP...

A new planktic foraminifer transfer function (GSF18) related 5 North Atlantic assemblages to winter and summer sea surface temperature. GSF18, based on recombined and simplified...

Relative abundance of planktonic foraminifera in Pliocene and Pleistocene sed...

Late Neogene planktonic foraminifera have been examined at Site 310 in the Central North Pacific and their stratigraphic ranges and frequencies are presented here. Blow's (1969)...