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(Table 18) Distribution of radiolaria in Miocene to Pleistocene sediments of ...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 17) Distribution of radiolaria in Miocene to Pleistocene sediments of ...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 10) Distribution of radiolaria in Miocene to Pleistocene sediments of ...
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 5) Distribution of radiolaria in Miocene to Pleistocene sediments of D...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 11) Distribution of radiolarians in ODP Hole 126-792E
species abundance: A = abundant, C = common, F = few, R = rare, - = absent -
(Table 8) Distribution of radiolarians in ODP Hole 126-792B
species abundance: A = abundant, C = common, F = few, R = rare, - = absent -
(Table 6) Distribution of radiolarians in ODP Hole 126-791B
species abundance: A = abundant, C = common, F = few, R = rare, - = absent -
(Appendix B4) Radiolaria abundance of ODP Hole 112-688A
P = present, - = absent -
(Appendix A) Radiolarian abundances in sediment core MD96-2086
Ages are from the age model of Bertrand et al. (2002, doi:10.1016/S0025-3227(01)00216-X) based on the benthic oxygen-isotope record measured on Cibicidoides wuellerstorfi -
(Appendix II-D) Occurrence of radiolarians in Neogene sediments of DSDP Hole ...
species abundance: P = present, + = very rare (1 specimen), - = absent -
(Appendix II-A) Occurrence of radiolarians in Neogene sediments of DSDP Hole ...
species abundance: P = present, + = very rare (1 specimen), - = absent -
Quaternary radiolarians from offshore eastern New Zealand, ODP Leg 181, Site ...
This dataset has no description
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Quaternary radiolarians from offshore eastern New Zealand, ODP Leg 181, Site ...
This dataset has no description
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Counts of radiolarians at Hole C9001C
The Northwest Pacific Ocean is characterized by a strong mixing of water masses, due to the interplay of three distinct currents, i.e., the Kuroshio, the Tsugaru, and the... -
Fossil occurrence of radiolarians from IODP Hole 316-C0008C
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Fossil occurrence of radiolarians from IODP Hole 316-C0008B
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Fossil occurrence of radiolarians from IODP Hole 316-C0008A
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Fossil occurrence of radiolarians from IODP Hole 316-C0004C
Geocode = [m CSF-A] Top Core depth (below sea floor) -
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...
