Stable oxygen isotope of benthic foraminifera in MIS 16 of IODP Hole 306-U1313D
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 |
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Data(s) |
10/07/2011
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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 |