Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland.
Coastal cliffs and stream cut sections at Langelandselv on Jameson Land show a 22 m thick sedimentary succession reflecting the development of shallow marine and fluvial environments during the last interglaciation. The shallow marine sediments were deposited in upper shoreface, back-barrier, and de...
Published in: | Boreas |
---|---|
Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
1994
|
Subjects: | |
Online Access: | https://eprints.lancs.ac.uk/id/eprint/22221/ https://doi.org/10.1111/j.1502-3885.1994.tb00608.x |
id |
ftulancaster:oai:eprints.lancs.ac.uk:22221 |
---|---|
record_format |
openpolar |
spelling |
ftulancaster:oai:eprints.lancs.ac.uk:22221 2023-08-27T04:09:12+02:00 Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. Vosgerau, H. Funder, S. Kelly, M. Knudsen, K.-L. Kronborg, C. Madsen, H. B. Sejrup, H. P. 1994 https://eprints.lancs.ac.uk/id/eprint/22221/ https://doi.org/10.1111/j.1502-3885.1994.tb00608.x unknown Vosgerau, H. and Funder, S. and Kelly, M. and Knudsen, K.-L. and Kronborg, C. and Madsen, H. B. and Sejrup, H. P. (1994) Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. Boreas, 23 (4). pp. 398-411. ISSN 1502-3885 Journal Article NonPeerReviewed 1994 ftulancaster https://doi.org/10.1111/j.1502-3885.1994.tb00608.x 2023-08-03T22:18:17Z Coastal cliffs and stream cut sections at Langelandselv on Jameson Land show a 22 m thick sedimentary succession reflecting the development of shallow marine and fluvial environments during the last interglaciation. The shallow marine sediments were deposited in upper shoreface, back-barrier, and delta environments during a rise in the relative sea level from 0 to 18 m. The interglacial succession ends with glaciotectonically dislocated fluvial sand, and is capped by alternating beds of lodgement till and fluvial sand, deposited during the Early Weichselian. The age is determined by palacoceanographic correlation of molluse and foraminifer faunas with isotopic substage 5e in the deep sea record, supported by luminescencs and U/Th dates and amino acid analysis. Article in Journal/Newspaper East Greenland Greenland Lancaster University: Lancaster Eprints Greenland Jameson Land ENVELOPE(-23.500,-23.500,71.167,71.167) Langelandselv ENVELOPE(-23.617,-23.617,70.517,70.517) Boreas 23 4 398 411 |
institution |
Open Polar |
collection |
Lancaster University: Lancaster Eprints |
op_collection_id |
ftulancaster |
language |
unknown |
description |
Coastal cliffs and stream cut sections at Langelandselv on Jameson Land show a 22 m thick sedimentary succession reflecting the development of shallow marine and fluvial environments during the last interglaciation. The shallow marine sediments were deposited in upper shoreface, back-barrier, and delta environments during a rise in the relative sea level from 0 to 18 m. The interglacial succession ends with glaciotectonically dislocated fluvial sand, and is capped by alternating beds of lodgement till and fluvial sand, deposited during the Early Weichselian. The age is determined by palacoceanographic correlation of molluse and foraminifer faunas with isotopic substage 5e in the deep sea record, supported by luminescencs and U/Th dates and amino acid analysis. |
format |
Article in Journal/Newspaper |
author |
Vosgerau, H. Funder, S. Kelly, M. Knudsen, K.-L. Kronborg, C. Madsen, H. B. Sejrup, H. P. |
spellingShingle |
Vosgerau, H. Funder, S. Kelly, M. Knudsen, K.-L. Kronborg, C. Madsen, H. B. Sejrup, H. P. Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. |
author_facet |
Vosgerau, H. Funder, S. Kelly, M. Knudsen, K.-L. Kronborg, C. Madsen, H. B. Sejrup, H. P. |
author_sort |
Vosgerau, H. |
title |
Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. |
title_short |
Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. |
title_full |
Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. |
title_fullStr |
Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. |
title_full_unstemmed |
Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. |
title_sort |
palaeoenvironments and changes in the relative sea level during the last interglaciation at langelandselv, jameson land, east greenland. |
publishDate |
1994 |
url |
https://eprints.lancs.ac.uk/id/eprint/22221/ https://doi.org/10.1111/j.1502-3885.1994.tb00608.x |
long_lat |
ENVELOPE(-23.500,-23.500,71.167,71.167) ENVELOPE(-23.617,-23.617,70.517,70.517) |
geographic |
Greenland Jameson Land Langelandselv |
geographic_facet |
Greenland Jameson Land Langelandselv |
genre |
East Greenland Greenland |
genre_facet |
East Greenland Greenland |
op_relation |
Vosgerau, H. and Funder, S. and Kelly, M. and Knudsen, K.-L. and Kronborg, C. and Madsen, H. B. and Sejrup, H. P. (1994) Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. Boreas, 23 (4). pp. 398-411. ISSN 1502-3885 |
op_doi |
https://doi.org/10.1111/j.1502-3885.1994.tb00608.x |
container_title |
Boreas |
container_volume |
23 |
container_issue |
4 |
container_start_page |
398 |
op_container_end_page |
411 |
_version_ |
1775350352486334464 |