-
(Table 4) Radiolarians at DSDP Hole 58-445
Abundance abbreviations: A = abundant (>20); C = common (11-20); F = few (7-10); R = rare (4-6); + = present (1-3). -
(Table T3) Radiolarian biostratigraphy of ODP Site 199-1220
Sediment depth is given in mbsf. Species abundance estimates (specimens > 63 µm): P = present but no abundance estimated, A = abundant (>10%), C = common (>1%-10%), F =... -
(Table T2) Radiolarian biostratigraphy of ODP Site 199-1219
Sediment depth is given in mbsf. Species abundance estimates (specimens > 63 µm): P = present but no abundance estimated, A = abundant (>10%), C = common (>1%-10%), F =... -
(Table T1) Radiolarian biostratigraphy of ODP Site 199-1218
Sediment depth is given in mbsf. Species abundance estimates (specimens > 63 µm): P = present but no abundance estimated, A = abundant (>10%), C = common (>1%-10%), F =... -
(Table T2) Relative abundance of selected radiolarian species from ODP Hole 1...
Sediment depth is given in mbsf. All radiolarians were counted under a light microscope with a magnification of 250x until the total exceeded 500. Note that relative abundances... -
(Table T1) Relative abundance of selected radiolarian species from ODP Hole 1...
Sediment depth is given in mbsf. All radiolarians were counted under a light microscope with a magnification of 250x until the total exceeded 500. Note that relative abundances... -
(Table 14) Distribution of radiolaria in Oligocene to Pleistocene sediments o...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 12) Distribution of radiolaria in Oligocene to Miocene sediments of DS...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 11) Distribution of radiolaria in Oligocene to Pliocene sediments of D...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 9) Distribution of radiolaria in Oligocene to Miocene sediments of DSD...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 8) Distribution of radiolaria in Oligocene to Pliocene sediments of DS...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 7) Distribution of radiolaria in Oligocene to Miocene sediments of DSD...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 6) Distribution of radiolaria in Miocene to Pleistocene sediments of D...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 3) Distribution of radiolaria in Oligocene to Miocene sediments of DSD...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 1) Occurrence of radiolarians and interpreted radiolarian zonal assign...
species abundances:A = abundant (at least one specimen in each field of view 1000 X), C = common (one specimen in 5 fields), F = few (one specimen per transect), R = rare (fewer... -
(Table 2) Occurrence of radiolarians and interpreted radiolarian zonal assign...
species abundances:A = abundant (at least one specimen in each field of view 1000 X), C = common (one specimen in 5 fields), F = few (one specimen per transect), R = rare (fewer... -
(Table 3) Range chart for stratigraphically important radiolarian species in ...
Sediment depth is given in mbsf. Barren intervals below 850 m not shown. Species abundance estimates as follows: C = common, F = few, VF = very few, MR = moderately rare, R =... -
(Table 1) Range chart for stratigraphically important radiolarian species in ...
Sediment depth is given in mbsf. Species abundance estimates as follows: A = abundant, F = few, R = rare, + = single specimen, - = searched for but not found, and ? = dubious... -
(Table 1) Radiolarians in the Oligocene-Miocene at DSDP Hole 72-515B
The Neogene of the southwestern Atlantic is virtually barren of biogenic silica. Of the four sites drilled on Leg 72, only two contained identifiable radiolarian specimens. In... -
Microfossils detected in a block of ancient dense clay coated with a ferroman...
The area in study is characterized by a regional stratigraphic hiatus from Early Miocene to Quaternary. Deposits from Late Eocene to Early Miocene occur on the bottom surface or...
