(Appendix Table 6) Isotope activity of sediment core PS1526-12


Autoria(s): Bohrmann, Horst
Cobertura

LATITUDE: 85.905000 * LONGITUDE: 22.725000 * DATE/TIME START: 1987-07-31T00:00:00 * DATE/TIME END: 1987-07-31T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.010 m * MAXIMUM DEPTH, sediment/rock: 3.250 m

Data(s)

19/03/2013

Formato

text/tab-separated-values, 1275 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.809012

doi:10.1594/PANGAEA.809012

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.809032

Bohrmann, Horst (1991): Radioisotopenstratigraphie, Sedimentologie und Geochemie jungquartärer Sedimente des östlichen Arktischen Ozeans (Radioisotope Stratigraphy, Sedimentology and Geochemistry of Late Quaternary Sediments from the Eastern Arctic Ocean). Berichte zur Polarforschung = Reports on Polar Research, 95, 133 pp, doi:10.2312/BzP_0095_1991

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #Accumulation rate, sediment, mean; AGE; Age model; Alpha-spectrometry; Arctic Ocean; ARK-IV/3; AWI_Paleo; Calculated; Calculated from weight/volume; Cumulative Thorium 230 standing crop; Cumulative Thorium 230 standing crop/Thorium 230 standing crop, expected; Density, dry bulk; DEPTH, sediment/rock; GIK21526-12 PS11/370-12; Gravity corer (Kiel type); Interval Cored; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; Protactinium 231; Protactinium 231, standard deviation; PS11; PS1526-12; Sedimentation rate; SL; Thorium 230; Thorium 230, standard deviation; Thorium 230 excess; Thorium 230 excess, standard deviation; Thorium 230 excess/Thorium 232 activity ratio; Thorium 230 excess/Thorium 232 activity ratio, standard deviation; Thorium 232; Thorium 232, standard deviation; Uranium 234; Uranium 234/Uranium 238 activity ratio; Uranium 234/Uranium 238 activity ratio, standard deviation; Uranium 238; Uranium 238, authigenic; Uranium 238, standard deviation; Uranium 238/Thorium 232 activity ratio
Tipo

Dataset