Documentation of sediment core PS2540-3


Autoria(s): Hillenbrand, Claus-Dieter; Ehrmann, Werner; Larter, Robert D; Benetti, Sara; Dowdeswell, Julian A; Cofaigh, Colm Ó; Graham, Alastair GC; Grobe, Hannes
Cobertura

LATITUDE: -70.065000 * LONGITUDE: -87.923330 * DATE/TIME START: 1994-02-17T13:15:00 * DATE/TIME END: 1994-02-17T13:15:00 * MINIMUM ELEVATION: -1820.0 m * MAXIMUM ELEVATION: -1820.0 m

Data(s)

27/08/2009

Formato

, unknown

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.115359

doi:10.1594/PANGAEA.115359

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.711173

Hillenbrand, Claus-Dieter; Ehrmann, Werner; Larter, Robert D; Benetti, Sara; Dowdeswell, Julian A; Cofaigh, Colm Ó; Graham, Alastair GC; Grobe, Hannes (2009): Clay mineral provenance of sediments in the southern Bellingshausen Sea reveals drainage changes of the West Antarctic Ice Sheet during the Late Quaternary. Marine Geology, 265(1-2), 1-18, doi:10.1016/j.margeo.2009.06.009

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Fonte

Alfred Wegener Institute - Polarstern core repository

Palavras-Chave #ANT-XI/3; AWI_Paleo; Bellingshausen Sea; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2540-3; PS29; PS29/048; SL
Tipo

Dataset