Dubinin, Alexander V (2006): (Table 54) Part of chemical elements (in % of their total contents) combined with bone detritus, micronodules, and phillipsite from >0.05 mm grain size fraction of bottom sediment from Core AKO26-35 [dataset]. P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, PANGAEA, https://doi.org/10.1594/PANGAEA.743900, In supplement to: Dubinin, AV (2006): Geochemistry of Rare-Earth Elements in the Ocean. Nauka Publ. (Moscow): in Russian, 360 pp
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: -29.600000 * Longitude: -149.966700
Minimum DEPTH, sediment/rock: 0.385 m * Maximum DEPTH, sediment/rock: 1.895 m
Event(s):
AKO26-35 * Latitude: -29.600000 * Longitude: -149.966700 * Elevation: -3880.0 m * Campaign: AKO_1970-1982_USSR * Basis: Akademik Korolev * Method/Device: Gravity corer (GC)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
288 data points
Data
1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Samp type | 5 Elements (La, Inductively coupled plasm...) | 6 Elements (Ce, Inductively coupled plasm...) | 7 Elements (Pr, Inductively coupled plasm...) | 8 Elements (Nd, Inductively coupled plasm...) | 9 Elements (Sm, Inductively coupled plasm...) | 10 Elements (Eu, Inductively coupled plasm...) | 11 Elements (Gd, Inductively coupled plasm...) | 12 Elements (Tb, Inductively coupled plasm...) | 13 Elements (Dy, Inductively coupled plasm...) | 14 Elements (Ho, Inductively coupled plasm...) | 15 Elements (Er, Inductively coupled plasm...) | 16 Elements (Tm, Inductively coupled plasm...) | 17 Elements (Yb, Inductively coupled plasm...) | 18 Elements (Lu, Inductively coupled plasm...) | 19 P [%] (Wet chemistry) | 20 Fe [%] (Atomic absorption spectrometr...) | 21 Mn [%] (Atomic absorption spectrometr...) | 22 Al [%] (Atomic absorption spectrometr...) | 23 Ni [%] (Atomic absorption spectrometr...) | 24 Co [%] (Atomic absorption spectrometr...) | 25 Cu [%] (Atomic absorption spectrometr...) |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.385 | 0.37 | 0.40 | bone detritus | 2.2 | 0.7 | 2.1 | 2 | 2 | 1.9 | 2.1 | 2.1 | 2.1 | 2.1 | 2.1 | 2.1 | 2.2 | 2.2 | 2.5 | <0.1 | <0.1 | <0.1 | 0.1 | <0.1 | <0.1 |
0.385 | 0.37 | 0.40 | micronodules | 1.5 | 9.6 | 1.4 | 1.3 | 1.4 | 1.2 | 1.2 | 1.3 | 1.2 | 1.3 | 1.3 | 1.2 | 1.3 | 1.3 | 1.5 | 6.5 | 22.9 | 2.0 | 33.1 | 23.2 | 16.5 |
0.385 | 0.37 | 0.40 | phillipsite | 1 | 2.1 | 0.9 | 0.9 | 0.9 | 0.8 | 0.8 | 0.8 | 0.8 | 0.8 | 0.7 | 0.7 | 0.7 | 0.7 | 0.9 | 2.0 | 0.5 | 5.1 | 1.1 | 0.6 | 2.7 |
1.075 | 1.05 | 1.10 | bone detritus | 3.8 | 1.7 | 4 | 3.9 | 4 | 4.1 | 3.9 | 4.1 | 4 | 4 | 3.9 | 4.1 | 4.1 | 4.3 | 5.0 | <0.1 | <0.1 | <0.1 | 0.1 | 0.2 | 0.2 |
1.075 | 1.05 | 1.10 | micronodules | 1 | 6.5 | 1 | 1 | 1 | 1 | 0.9 | 1 | 0.9 | 0.9 | 0.8 | 0.9 | 0.9 | 0.9 | 1.0 | 5.9 | 19.7 | 1.8 | 22.6 | 27.6 | 13.5 |
1.075 | 1.05 | 1.10 | phillipsite | 0.2 | 0.3 | 0.2 | 0.2 | 0.1 | 0.2 | 0.1 | 0.1 | 0.1 | 0.1 | 0.1 | 0.1 | 0.1 | 0.1 | 0.2 | 0.6 | 0.1 | 1.5 | 0.1 | 0.1 | 0.7 |
1.700 | 1.65 | 1.75 | bone detritus | 1.9 | 1 | 2.1 | 2.1 | 2.1 | 2.1 | 2.1 | 2.2 | 2.1 | 2.2 | 2.1 | 2.1 | 2.3 | 2.3 | 4.1 | <0.1 | <0.1 | <0.1 | 0.1 | <0.1 | 0.1 |
1.700 | 1.65 | 1.75 | micronodules | 0.5 | 1.3 | 0.5 | 0.5 | 0.5 | 0.5 | 0.5 | 0.5 | 0.4 | 0.5 | 0.4 | 0.4 | 0.4 | 0.4 | 0.7 | 2.1 | 5.1 | 0.6 | 8.4 | 4.8 | 4.5 |
1.700 | 1.65 | 1.75 | phillipsite | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | 0.1 | 0.1 | <0.1 | 0.3 | <0.1 | <0.1 | 0.1 |
1.895 | 1.89 | 1.90 | bone detritus | 1.4 | 0.8 | 1.5 | 1.4 | 1.5 | 1.4 | 1.4 | 1.5 | 1.5 | 1.5 | 1.5 | 1.5 | 1.6 | 1.6 | 3.9 | <0.1 | <0.1 | <0.1 | <0.1 | 0.1 | 0.1 |
1.895 | 1.89 | 1.90 | micronodules | 0.4 | 1 | 0.4 | 0.4 | 0.4 | 0.4 | 0.4 | 0.4 | 0.4 | 0.4 | 0.4 | 0.3 | 0.4 | 0.4 | 0.7 | 1.6 | 4.7 | 0.7 | 8.5 | 3.4 | 2.6 |
1.895 | 1.89 | 1.90 | phillipsite | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | <0.1 | 0.1 | <0.1 | <0.1 | <0.1 |