Motoyama, Isao (2001): (Table T1) Census counts of radiolarian taxa in ODP Hole 175-1082A. PANGAEA, https://doi.org/10.1594/PANGAEA.231306, In supplement to: Motoyama, I (2001): Late Cenozoic radiolarians from South Atlantic Hole 1082A, Leg 175. In: Wefer, G; Berger, WH; Richter, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 175, 1-26, https://doi.org/10.2973/odp.proc.sr.175.232.2001
Always quote citation above when using data! You can download the citation in several formats below.
Latitude: -21.093940 * Longitude: 11.820580
Date/Time Start: 1997-09-13T04:45:00 * Date/Time End: 1997-09-16T00:05:00
Minimum Elevation: -1279.3 m * Maximum Elevation: -1279.3 m
175-1082A * Latitude: -21.093940 * Longitude: 11.820580 * Date/Time Start: 1997-09-13T04:45:00 * Date/Time End: 1997-09-16T00:05:00 * Elevation: -1279.3 m * Penetration: 600.6 m * Recovery: 502.01 m * Location: Benguela Current, South Atlantic Ocean * Campaign: Leg175 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 64 cores; 600.6 m cored; 0 m drilled; 83.6 % recovery
Abundance: A = abundant; >10,000 specimens on a slide. C = common; 1001-10,000 specimens on a slide. F = few; 501-1000 specimens on a slide. R = rare; 11-500 specimens on a slide. T = trace; 1-10 specimens on a slide. B = barren; 0 specimens. Preservation of the radiolarian assemblage was based on the following categories: G = good; radiolarians show no signs of dissolution with only minor fragmentation. M = moderate; radiolarians show evidence of moderate dissolution with obvious fragmentation. P = poor; radiolarians show signs of a high degree of dissolution with very few intact specimens.
9299 data points