Acoustic facies on the inner Kara Sea Shelf: implications for late Weichselian to Holocene sediment dynamics
We studied the impact of the last glacial (late Weichselian) sea level cycle on sediment architecture in theinner Kara Sea using high-resolution acoustic sub-bottom profiling. The acoustic lines were ground-truthedwith dated sediment cores. Furthermore we refined the location of the eastern LGM ice...
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Online Access: | https://epic.awi.de/id/eprint/14633/ https://doi.org/10.1016/j.margeo.2008.06.004 https://hdl.handle.net/10013/epic.39240 |
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ftawi:oai:epic.awi.de:14633 2024-09-15T18:16:08+00:00 Acoustic facies on the inner Kara Sea Shelf: implications for late Weichselian to Holocene sediment dynamics Dittmers, Klaus 2008 https://epic.awi.de/id/eprint/14633/ https://doi.org/10.1016/j.margeo.2008.06.004 https://hdl.handle.net/10013/epic.39240 unknown ELSEVIER SCIENCE BV Dittmers, K. (2008) Acoustic facies on the inner Kara Sea Shelf: implications for late Weichselian to Holocene sediment dynamics , Marine Geology, 254 (3-4), pp. 197-215 . doi:10.1016/j.margeo.2008.06.004 <https://doi.org/10.1016/j.margeo.2008.06.004> , hdl:10013/epic.39240 EPIC3Marine Geology, ELSEVIER SCIENCE BV, 254(3-4), pp. 197-215, ISSN: 0025-3227 Article isiRev 2008 ftawi https://doi.org/10.1016/j.margeo.2008.06.004 2024-06-24T03:58:50Z We studied the impact of the last glacial (late Weichselian) sea level cycle on sediment architecture in theinner Kara Sea using high-resolution acoustic sub-bottom profiling. The acoustic lines were ground-truthedwith dated sediment cores. Furthermore we refined the location of the eastern LGM ice margin, by new subbottom profiles. New model results of post-Last Glacial Maximum (LGM) isostatic rebound for this area allowa well-constrained interpretation of acoustic units in terms of sequence stratigraphy. The lowstand (orregressive) system tract sediments are absent but are represented by an unconformity atop of Pleistocenesediments on the shelf and by a major incised dendritic paleo-river network. The subsequent transgressiveand highstand system tracts are best preserved in the incised channels and the recent estuaries while onlyminor sediment accumulation on the adjacent shelf areas is documented. The Kara Sea can be subdividedinto three areas: estuaries (A), the shelf (B) and (C) deeper lying areas that accumulated a total of 114 x1010 t of Holocene sediments. Article in Journal/Newspaper Kara Sea Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Marine Geology 254 3-4 197 215 |
institution |
Open Polar |
collection |
Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
We studied the impact of the last glacial (late Weichselian) sea level cycle on sediment architecture in theinner Kara Sea using high-resolution acoustic sub-bottom profiling. The acoustic lines were ground-truthedwith dated sediment cores. Furthermore we refined the location of the eastern LGM ice margin, by new subbottom profiles. New model results of post-Last Glacial Maximum (LGM) isostatic rebound for this area allowa well-constrained interpretation of acoustic units in terms of sequence stratigraphy. The lowstand (orregressive) system tract sediments are absent but are represented by an unconformity atop of Pleistocenesediments on the shelf and by a major incised dendritic paleo-river network. The subsequent transgressiveand highstand system tracts are best preserved in the incised channels and the recent estuaries while onlyminor sediment accumulation on the adjacent shelf areas is documented. The Kara Sea can be subdividedinto three areas: estuaries (A), the shelf (B) and (C) deeper lying areas that accumulated a total of 114 x1010 t of Holocene sediments. |
format |
Article in Journal/Newspaper |
author |
Dittmers, Klaus |
spellingShingle |
Dittmers, Klaus Acoustic facies on the inner Kara Sea Shelf: implications for late Weichselian to Holocene sediment dynamics |
author_facet |
Dittmers, Klaus |
author_sort |
Dittmers, Klaus |
title |
Acoustic facies on the inner Kara Sea Shelf: implications for late Weichselian to Holocene sediment dynamics |
title_short |
Acoustic facies on the inner Kara Sea Shelf: implications for late Weichselian to Holocene sediment dynamics |
title_full |
Acoustic facies on the inner Kara Sea Shelf: implications for late Weichselian to Holocene sediment dynamics |
title_fullStr |
Acoustic facies on the inner Kara Sea Shelf: implications for late Weichselian to Holocene sediment dynamics |
title_full_unstemmed |
Acoustic facies on the inner Kara Sea Shelf: implications for late Weichselian to Holocene sediment dynamics |
title_sort |
acoustic facies on the inner kara sea shelf: implications for late weichselian to holocene sediment dynamics |
publisher |
ELSEVIER SCIENCE BV |
publishDate |
2008 |
url |
https://epic.awi.de/id/eprint/14633/ https://doi.org/10.1016/j.margeo.2008.06.004 https://hdl.handle.net/10013/epic.39240 |
genre |
Kara Sea |
genre_facet |
Kara Sea |
op_source |
EPIC3Marine Geology, ELSEVIER SCIENCE BV, 254(3-4), pp. 197-215, ISSN: 0025-3227 |
op_relation |
Dittmers, K. (2008) Acoustic facies on the inner Kara Sea Shelf: implications for late Weichselian to Holocene sediment dynamics , Marine Geology, 254 (3-4), pp. 197-215 . doi:10.1016/j.margeo.2008.06.004 <https://doi.org/10.1016/j.margeo.2008.06.004> , hdl:10013/epic.39240 |
op_doi |
https://doi.org/10.1016/j.margeo.2008.06.004 |
container_title |
Marine Geology |
container_volume |
254 |
container_issue |
3-4 |
container_start_page |
197 |
op_container_end_page |
215 |
_version_ |
1810454110604886016 |