Age model and d13C (C. wuellerstorfi) of sediment core GeoB1112-4


Autoria(s): Mackensen, Andreas; Bickert, Torsten
Cobertura

LATITUDE: -5.778333 * LONGITUDE: -10.750000 * DATE/TIME START: 1989-01-03T00:00:00 * DATE/TIME END: 1989-01-03T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.03 m * MAXIMUM DEPTH, sediment/rock: 6.88 m

Data(s)

03/03/2009

Formato

text/tab-separated-values, 276 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.713741

doi:10.1594/PANGAEA.713741

Idioma(s)

en

Publicador

PANGAEA

Relação

Bickert, Torsten; Wefer, Gerold (1996): Late Quaternary deep water circulation in the South Atlantic: Reconstruction from carbonate dissolution and benthic stable isotopes. In: Wefer, G; Berger, W H; Siedler, G & Webb, D (eds.), The South Atlantic: Present and Past Circulation. Springer-Verlag, Berlin, 103, 599-620

Mackensen, Andreas; Bickert, Torsten (1999): Stable carbon isotopes in benthic foraminifera: proxies for deep and bottom water circulation and new production. In: Fischer, G & Wefer, G (eds.), Use of Proxies in Paleoceanography - Examples from the South Atlantic, Springer, Berlin, Heidelberg, 229-254

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #Age model; Age model, SPECMAP chronology, Imbrie et al. (1984); Cibicidoides wuellerstorfi, d13C; DEPTH, sediment/rock; Equatorial Atlantic; GeoB; GeoB1112-4; Geosciences, University of Bremen; Gravity corer (Kiel type); M9/4; Mass spectrometer Finnigan MAT 251; Meteor (1986); SFB261; SL; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents
Tipo

Dataset