(Table S1) Stable oxygen isotopes, Mg/Ca ratios and UK'37 measurement of sediment core NIOP-C2_929


Autoria(s): Saher, MH; Rostek, Frauke; Jung, S J A; Bard, Edouard; Schneider, Ralph R; Greaves, Mervyn; Ganssen, Gerald M; Elderfield, Henry; Kroon, Dick
Cobertura

LATITUDE: 13.703500 * LONGITUDE: 53.246000 * MINIMUM DEPTH, sediment/rock: 8.705 m * MAXIMUM DEPTH, sediment/rock: 11.915 m

Data(s)

15/04/2009

Formato

text/tab-separated-values, 1251 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.831773

doi:10.1594/PANGAEA.831773

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.831774

Saher, MH; Rostek, Frauke; Jung, S J A; Bard, Edouard; Schneider, Ralph R; Greaves, Mervyn; Ganssen, Gerald M; Elderfield, Henry; Kroon, Dick (2009): Western Arabian Sea SST during the penultimate interglacial: A comparison of UK'37 and Mg/Ca paleothermometry. Paleoceanography, 24(2), PA2212, doi:10.1029/2007PA001557

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #AGE; Alkenone, unsaturation index UK'37; Arabian Sea; Calculated from Mg/Ca ratios (Anand et al., 2003); Calculated from UK'37 (Sonzogni et al., 1997); Core; CORE; Corrected for dissolution (Rosenthal and Lohmann, 2002); delta 18O; DEPTH, sediment/rock; Globigerinoides ruber, d18O; Globigerinoides ruber, Magnesium/Calcium ratio; Globigerinoides ruber, shell, weight; Mass spectrometer Finnigan MAT 252; n-Alkane C37; NIOP929; NIOP-C2; NIOP-C2_929; Sea surface temperature, annual mean; Tyro; Varian Vista Pro Inductively Coupled Plasma Atomic Emission Spectrometer
Tipo

Dataset