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Relative abundance of radiolarian from different cores in the Pacific Ocean
Radiolarian census counts (in relative abundance) and environmental data from 801 core-tops distributed across the Pacific Ocean (mmn8). -
(Table 6) Abundance of radiolarian species present at ODP Hole 119-745B
Species abundance: X = 1 specimen, R = rare (<5 specimens), F = few (5-10), C = common (10-20), A = abundant (>20), - = absent, ? = questionable -
(Table 1) Abundance of radiolarian species present at ODP Site 119-736
Species abundance: X = 1 specimen, R = rare (<5 specimens), F = few (5-10), C = common (10-20), A = abundant (>20), - = absent, ? = questionable -
Radiolarian abundance of sediment core Y8
A high-resolution record of radiolarian faunal changes from Site Y8 south of the Subtropical Front (STF), offshore eastern New Zealand, provides insight into the... -
Radiolaria abundance of Hole 28-269
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 28-268
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 28-267A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 28-267
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 28-266
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 28-265
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Southern Ocean RADiolarian dataset (SO-RAD)
Radiolarians (holoplanktonic Protozoa) found in marine sediments are commonly used in Southern Ocean as palaeoclimate proxies. Generating such reconstructions of past climate...
