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(Table 1) Distribution of calcareous nannofossils in ODP Hole 117-723A
Species abundance: A = abundant (1-10 specimens per field of view at 1500 X=, C = common (1 specimen per 2- 10 fields), F = few (1 specimen per 11-100 fields), R = rare (1... -
(Figure 8) Range chart of calcareous nannofossils in ODP Hole 116-719A
X = very rare (1-2 specimens), R = rare 3-5 specimens), F = few 6-20 specimens), C = common (20-100 specimens), A = abundant (>100 specimens), W = very abundant >80%), ? =... -
(Figure 4) Range chart of calcareous nannofossils in ODP Hole 116-717A
X = very rare (1-2 specimens), R = rare 3-5 specimens), F = few 6-20 specimens), C = common (20-100 specimens), A = abundant (>100 specimens), W = very abundant >80%), ? =... -
(Table 5A) Neogene distribution of calcareous nannofossils at DSDP Hole 43-386
Species distribution: A = abundant (>10 % of total Cenozoic forms), C = common (1-10 %), F = few (0.1-1 %), R = rare (<0.1 %), - = absent -
(Table 2A) Neogene distribution of calcareous nannofossils at DSDP Hole 43-382
Species distribution: A = abundant (>10 % of total Cenozoic forms), C = common (1-10 %), F = few (0.1-1 %), R = rare (<0.1 %), - = absent -
Coccolithophores abundance at IODP Hole 385-U1549A in Guaymas Basin, Gulf of ...
The sedimentary samples studied came from cores of Hole 385-U1549A (27° 28.33167' N, 111° 28.7844' W) obtained during the International Ocean Discovery Program (IODP) Expedition... -
Coccolithophore relative abundances at the Ideale Section - Montalbano Jonico...
In the present dataset we provide relative abundance (%) of the main taxa of the coccolithophore. Slides for coccolithophore analysis were prepared following Flores and Sierro... -
Coccolithophore absolute abundances at the Ideale Section - Montalbano Jonico...
In the present dataset we provide absolute abundance of total coccolithophore assemblage (Total N) and of the main taxa as # coccoliths/g *107. Slides for coccolithophore... -
Range chart of calcareous nannofossils from ODP Hole 188-1165B (Table 1)
Bio- and magnetostratigraphic age data and nannofossil assemblage analysis from ODP Site 1165 evidence an anomalous warming event of the surface waters in and around Prydz Bay...
