Age model of sediment core PS2547-3
| Cobertura |
LATITUDE: -71.150000 * LONGITUDE: -119.918333 * DATE/TIME START: 1994-03-02T16:54:00 * DATE/TIME END: 1994-03-02T16:54:00 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 8.75 m |
|---|---|
| Data(s) |
01/12/2002
|
| Formato |
text/tab-separated-values, 21 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.55951 doi:10.1594/PANGAEA.55951 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.711660 Hillenbrand, Claus-Dieter (2000): Glazialmarine Sedimentationsentwicklung am westantarktischen Kontinentalrand im Amundsen- und Bellingshausenmeer - Hinweise auf Paläoumweltveränderungen während der quartären Klimazyklen (Glaciomarine sedimentation on the continental margins of the Amundsen and Bellingshausen Seas, West Antarctica - indications for paleoenvironmental changes during the Quaternary climatic cycles). Berichte zur Polarforschung = Reports on Polar Research, 346, 182 pp, doi:10.2312/BzP_0346_2000 Hillenbrand, Claus-Dieter; Fütterer, Dieter K; Grobe, Hannes; Frederichs, Thomas (2002): No evidence for a Pleistocene collapse of the West Antarctic Ice Sheet from continental margin sediments recovered in the Amundsen Sea. Geo-Marine Letters, 22(2), 51-59, doi:10.1007/s00367-002-0097-7 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Age model; Age model, lithological correlation; Amundsen Sea; ANT-XI/3; AWI_Paleo; DEPTH, sediment/rock; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2547-3; PS29; PS29/063; SL |
| Tipo |
Dataset |
