Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Hillenbrand, Claus-Dieter; Grobe, Hannes; Diekmann, Bernhard; Kuhn, Gerhard; Fütterer, Dieter K (2003): Sedimentology on surface samples from the Amundsen and Bellingshausen Seas [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.87359, Supplement to: Hillenbrand, C-D et al. (2003): Distribution of clay minerals and proxies for productivity in surface sediments of the Bellingshausen and Amundsen seas (West Antarctica) - Relation to modern environmental conditions. Marine Geology, 193(3-4), 253-271, https://doi.org/10.1016/S0025-3227(02)00659-X

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
Surface sediments from the Antarctic continental margin in the Bellingshausen and Amundsen seas (Pacific sector of the Southern Ocean) were investigated in order to decipher their capability to record modern environmental conditions. Spatial distribution of terrigenous sand and mud reflect regional differences in current-induced redeposition of glaciogenic debris. Clay mineral assemblages in the shelf sediments are controlled by the supply of terrigenous detritus from source rocks in the adjacent hinterland suggesting the occurrence of yet unknown sedimentary rocks in the hinterland of the Amundsen Sea. Clay mineral distribution on the continental rise in the Bellingshausen Sea points to the continuation of a bottom current from the Antarctic Peninsula rise to at least 94°W. Foraminifer-bearing and opal-poor deposits prevail on the continental margin in the western Bellingshausen Sea and the Amundsen Sea, whereas diatom-bearing and carbonate-free sediments characterize the eastern Bellingshausen Sea. Different modes of biological production, which were deduced from accumulation rates of biogenic barium during Marine Isotope Stage 1 and recent productivity measurements, obviously control the spatial pattern of opal- and carbonate-bearing sediments in the study area.
Coverage:
Median Latitude: -69.224833 * Median Longitude: -85.682034 * South-bound Latitude: -73.401667 * West-bound Longitude: -121.948333 * North-bound Latitude: -64.184000 * East-bound Longitude: -64.114333
Date/Time Start: 1987-11-28T12:40:00 * Date/Time End: 1994-03-08T10:47:00
Minimum DEPTH, sediment/rock: 0.010 m * Maximum DEPTH, sediment/rock: 0.010 m
Event(s):
PS1554-1 (PS12/185) * Latitude: -65.208667 * Longitude: -64.114333 * Date/Time: 1987-11-28T12:40:00 * Elevation: -400.0 m * Penetration: 0.41 m * Recovery: 0.41 m * Location: Argentine Islands * Campaign: ANT-VI/2 (PS12) * Basis: Polarstern * Method/Device: Giant box corer (GKG)
PS1555-1 (PS12/186) * Latitude: -65.751167 * Longitude: -69.049333 * Date/Time: 1987-11-30T12:43:00 * Elevation: -218.0 m * Penetration: 0.14 m * Recovery: 0.14 m * Location: Adelaide Island * Campaign: ANT-VI/2 (PS12) * Basis: Polarstern * Method/Device: Giant box corer (GKG)
PS1557-1 (PS12/193) * Latitude: -65.357667 * Longitude: -66.457500 * Date/Time: 1987-12-02T21:27:00 * Elevation: -458.0 m * Penetration: 0.46 m * Recovery: 0.46 m * Location: Anvers Island * Campaign: ANT-VI/2 (PS12) * Basis: Polarstern * Method/Device: Giant box corer (GKG)
Size:
378 data points

Download Data

Download dataset as tab-delimited text — use the following character encoding:

View dataset as HTML