Stable oxygen isotope of benthic foraminifera in MIS 16 of IODP Hole 306-U1313D


Autoria(s): Naafs, Bernhard David A; Hefter, Jens; Ferretti, Patrizia; Stein, Ruediger; Haug, Gerald H
Cobertura

MEDIAN LATITUDE: 41.000021 * MEDIAN LONGITUDE: -32.957162 * SOUTH-BOUND LATITUDE: 41.000019 * WEST-BOUND LONGITUDE: -32.957300 * NORTH-BOUND LATITUDE: 41.000023 * EAST-BOUND LONGITUDE: -32.957023 * MINIMUM DEPTH, sediment/rock: 14.54 m * MAXIMUM DEPTH, sediment/rock: 42.50 m

Data(s)

10/07/2011

Formato

text/tab-separated-values, 633 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.762826

doi:10.1594/PANGAEA.762826

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.758056

Naafs, Bernhard David A; Hefter, Jens; Ferretti, Patrizia; Stein, Ruediger; Haug, Gerald H (2011): Sea surface temperatures did not control the first occurrence of Hudson Strait Heinrich Events during MIS 16. Paleoceanography, 26, PA4201, doi:10.1029/2011PA002135

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #306-U1313B; 306-U1313D; Calculated; Cibicidoides wuellerstorfi, d18O; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Exp306; Foraminifera, benthic d18O; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Mass spectrometer Finnigan MAT 251; North Atlantic Climate 2; ODP sample designation; Sample code/label; Sample code/label 2; Sea surface temperature, annual mean
Tipo

Dataset