Sedimentology on two cores from Scoresby Sund, Greenland ...
Reconstruction of the postglacial palaeoenvironmental evolution was the main objective of marine geological investigations in the Scorcsby Sund fjord system. For this purpose, samples of marine sediments, taken on RV Polarstern cruises ARK-V/3b and ARK-VII/3b in 1988 and 1990, have been analysed. Al...
Main Author: | |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA
1992
|
Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.763190 https://doi.pangaea.de/10.1594/PANGAEA.763190 |
id |
ftdatacite:10.1594/pangaea.763190 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.1594/pangaea.763190 2024-09-15T18:04:19+00:00 Sedimentology on two cores from Scoresby Sund, Greenland ... Marienfeld, Peter 1992 application/zip https://dx.doi.org/10.1594/pangaea.763190 https://doi.pangaea.de/10.1594/PANGAEA.763190 en eng PANGAEA https://dx.doi.org/10.2312/bzp_0096_1991 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type ARK-V/3b Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN article Collection Supplementary Publication Series of Datasets 1992 ftdatacite https://doi.org/10.1594/pangaea.76319010.2312/bzp_0096_1991 2024-07-03T13:10:33Z Reconstruction of the postglacial palaeoenvironmental evolution was the main objective of marine geological investigations in the Scorcsby Sund fjord system. For this purpose, samples of marine sediments, taken on RV Polarstern cruises ARK-V/3b and ARK-VII/3b in 1988 and 1990, have been analysed. All investigated fjord sediments are paratills. However, remarkable changes in sediment fabric and composition occur with depth in cores. They are attributable to different modes of sediment deposition. Therefore, a subdivision of the postglacial palaeoenvironmental history into periods of considerably different sedimentary conditions is feasible.The change of sedimentary fades with time is interpreted by deposition under changing climatic conditions during the postglacial. Displacements of cyclonic and anticyclonic centers in the atmosphere change amount of precipitation at the east coast of Greenland. Precipitation strongly influences extension of local ice caps of coastal areas and duration of coverage of the ... : Supplement to: Marienfeld, Peter (1992): Postglacial sedimentary history of Scoresby Sund, East Greenland. Polarforschung, 60(3), 181-195 ... Article in Journal/Newspaper East Greenland Greenland Scoresby Sund DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Gravity corer Kiel type ARK-V/3b Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
spellingShingle |
Gravity corer Kiel type ARK-V/3b Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN Marienfeld, Peter Sedimentology on two cores from Scoresby Sund, Greenland ... |
topic_facet |
Gravity corer Kiel type ARK-V/3b Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
description |
Reconstruction of the postglacial palaeoenvironmental evolution was the main objective of marine geological investigations in the Scorcsby Sund fjord system. For this purpose, samples of marine sediments, taken on RV Polarstern cruises ARK-V/3b and ARK-VII/3b in 1988 and 1990, have been analysed. All investigated fjord sediments are paratills. However, remarkable changes in sediment fabric and composition occur with depth in cores. They are attributable to different modes of sediment deposition. Therefore, a subdivision of the postglacial palaeoenvironmental history into periods of considerably different sedimentary conditions is feasible.The change of sedimentary fades with time is interpreted by deposition under changing climatic conditions during the postglacial. Displacements of cyclonic and anticyclonic centers in the atmosphere change amount of precipitation at the east coast of Greenland. Precipitation strongly influences extension of local ice caps of coastal areas and duration of coverage of the ... : Supplement to: Marienfeld, Peter (1992): Postglacial sedimentary history of Scoresby Sund, East Greenland. Polarforschung, 60(3), 181-195 ... |
format |
Article in Journal/Newspaper |
author |
Marienfeld, Peter |
author_facet |
Marienfeld, Peter |
author_sort |
Marienfeld, Peter |
title |
Sedimentology on two cores from Scoresby Sund, Greenland ... |
title_short |
Sedimentology on two cores from Scoresby Sund, Greenland ... |
title_full |
Sedimentology on two cores from Scoresby Sund, Greenland ... |
title_fullStr |
Sedimentology on two cores from Scoresby Sund, Greenland ... |
title_full_unstemmed |
Sedimentology on two cores from Scoresby Sund, Greenland ... |
title_sort |
sedimentology on two cores from scoresby sund, greenland ... |
publisher |
PANGAEA |
publishDate |
1992 |
url |
https://dx.doi.org/10.1594/pangaea.763190 https://doi.pangaea.de/10.1594/PANGAEA.763190 |
genre |
East Greenland Greenland Scoresby Sund |
genre_facet |
East Greenland Greenland Scoresby Sund |
op_relation |
https://dx.doi.org/10.2312/bzp_0096_1991 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.76319010.2312/bzp_0096_1991 |
_version_ |
1810441810426724352 |