-
(Table T3) Calcareous nannofossil stratigraphy of ODP Hole 198-1208A
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant (>10 specimens per field of view [FOV]); C = common (1 -10 specimens per FOV); F = few (1... -
(Table T2) Calcareous nannofossil stratigraphy of ODP Hole 198-1207B
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant (>10 specimens per field of view [FOV]); C = common (1 -10 specimens per FOV); F = few (1... -
(Table T1) Calcareous nannofossil stratigraphy of ODP Hole 198-1207A
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant (>10 specimens per field of view [FOV]); C = common (1 -10 specimens per FOV); F = few (1... -
(Table 3) Relative abundance of nannofossils of ODP Hole 103-640A
Species abundance: V = very abundant (>20 specimens per field of view), A = abundant (1-10 specimens per field of view), C = common (1 specimen per 11-100 fields of view), F... -
(Table T5) Cretaceous calcareous nannofossil abundance of ODP Hole 173-1069A
Sediment depth is given in mbsf. Abundance estimates as follows: Abundance: A = abundant, C = common, F = few, R = rare, 1 = single, B = barren, - = not found. -
(Table 5) Relative abundance of nannofossils of ODP Hole 103-641A
Species abundance: V = very abundant (>20 specimens per field of view), A = abundant (1-10 specimens per field of view), C = common (1 specimen per 11-100 fields of view), F... -
(Table 4) Relative abundance of nannofossils of ODP Hole 103-641C
Species abundance: V = very abundant (>20 specimens per field of view), A = abundant (1-10 specimens per field of view), C = common (1 specimen per 11-100 fields of view), F... -
(Table 2) Relative abundance of nannofossils of ODP Site 103-638
Species abundance: V = very abundant (>20 specimens per field of view), A = abundant (1-10 specimens per field of view), C = common (1 specimen per 11-100 fields of view), F... -
(Table 1) Relative abundance of nannofossils of ODP Hole 103-639A
Species abundance: V = very abundant (>20 specimens per field of view), A = abundant (1-10 specimens per field of view), C = common (1 specimen per 11-100 fields of view), F... -
(Table 6) 40K-40Ar radiometric analyses of DSDP Hole 84-567A
This dataset has no description
-
(Table T12) Calcareous nannofossil stratigraphy of ODP Hole 198-1213A
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant (>10 specimens per field of view [FOV]); C = common (1 -10 specimens per FOV); F = few (1... -
(Table T10) Calcareous nannofossil stratigraphy of ODP Hole 198-1212A
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant (>10 specimens per field of view [FOV]); C = common (1 -10 specimens per FOV); F = few (1... -
(Table T9) Calcareous nannofossil stratigraphy of ODP Hole 198-1211C
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant (>10 specimens per field of view [FOV]); C = common (1 -10 specimens per FOV); F = few (1... -
(Table T3) Cretaceous calcareous nannofossil abundance of ODP Hole 173-1068A
Sediment depth is given in mbsf. Abundance estimates as follows: Abundance: A = abundant, C = common, F = few, R = rare, 1 = single, B = barren, - = not found. -
Radiocarbon dating of siliceous sinter deposits from El Tatio Geyser field, C...
Radiocarbon 14C Dating of hydrothermal siliceous sinter deposits from El Tatio Geyser field in the Chilean Altiplano. All samples were analyzed at the Keck-Carbon Cycle... -
Biogenic and lithogenic silica, silicic acid, production of biogenic silica, ...
This dataset has no description
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MORI Party Conference Poll, 1977
Abstract copyright UK Data Service and data collection copyright owner. To investigate public opinion about politics before the British political party conferences in 1977.... -
(Tab.2) K-Ar age determination of dredged basalt samples at station PS2693-1
This dataset has no description
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Age determination of beachrocks and hybrid carbonates deposited during the Ho...
The data refer to the geochemical and isotopic characterization of sandstones, with carbonate cementation (beach rocks), and hybrid carbonates, formed by algal mats, in the... -
Age determination of sediment core HZM, lake Holzmar (Tables 1, 2)
AMS radiocarbon ages have been determined on terrestrial macrofossils selected from the annually laminated sediments of lake Holzmaar (Germany). The radiocarbon chronology of...
