Dynamic sea‐level change during the last deglaciation of northern Iceland
Rundgren, M., Ingólfsson, Ó., Björck, S., Jiang, H. & Haflioason, H. 1997 (September): Dynamic sea‐level change during the last deglaciation of northern Iceland. Boreas , Vol. 26, pp. 201–215. Oslo. ISSN 0300–9483. A detailed reconstruction of deglacial relative sea‐level changes at the northern...
Published in: | Boreas |
---|---|
Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
1997
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1111/j.1502-3885.1997.tb00852.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1997.tb00852.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1997.tb00852.x |
id |
crwiley:10.1111/j.1502-3885.1997.tb00852.x |
---|---|
record_format |
openpolar |
spelling |
crwiley:10.1111/j.1502-3885.1997.tb00852.x 2024-10-13T14:08:06+00:00 Dynamic sea‐level change during the last deglaciation of northern Iceland RUNDGREN, MATS INGÓLFSSON, ÓLAFUR BJÖRCK, SVANTE JIANG, HUI HAFLIDASON, HAFLIDI 1997 http://dx.doi.org/10.1111/j.1502-3885.1997.tb00852.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1997.tb00852.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1997.tb00852.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 26, issue 3, page 201-215 ISSN 0300-9483 1502-3885 journal-article 1997 crwiley https://doi.org/10.1111/j.1502-3885.1997.tb00852.x 2024-09-23T04:36:41Z Rundgren, M., Ingólfsson, Ó., Björck, S., Jiang, H. & Haflioason, H. 1997 (September): Dynamic sea‐level change during the last deglaciation of northern Iceland. Boreas , Vol. 26, pp. 201–215. Oslo. ISSN 0300–9483. A detailed reconstruction of deglacial relative sea‐level changes at the northern coast of Iceland, based on the litho‐ and biostratigraphy of lake basins, indicates an overall fall in relative sea level of about 45 m between 11300 and 9100 BP, corresponding to an isostatic rebound of 77 m. The overall regression was interrupted by two minor transgressions during the late Younger Dryas and in early Preboreal, and these were probably caused by a combination of expansions of local ice caps and readvances of the Icelandic inland ice‐sheet margin. Maximum absolute uplift rates are recorded during the regressional phase between the two transgressions (10000–9850 BP), with a mean value of c . 15 cm 14 C yr ‐1 or 11–12 cm cal. yr ‐1 . Mean absolute uplift during the regressional phase following the second transgression (9700–9100 BP) was around 6 cm 14 C yr ‐1 , corresponding to c . 3 cm cal. yr ‐1 , and relative sea level dropped below present‐day sea level at 9000 BP. Article in Journal/Newspaper Ice Sheet Iceland Wiley Online Library Boreas ENVELOPE(-3.933,-3.933,-71.300,-71.300) Boreas 26 3 201 215 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
Rundgren, M., Ingólfsson, Ó., Björck, S., Jiang, H. & Haflioason, H. 1997 (September): Dynamic sea‐level change during the last deglaciation of northern Iceland. Boreas , Vol. 26, pp. 201–215. Oslo. ISSN 0300–9483. A detailed reconstruction of deglacial relative sea‐level changes at the northern coast of Iceland, based on the litho‐ and biostratigraphy of lake basins, indicates an overall fall in relative sea level of about 45 m between 11300 and 9100 BP, corresponding to an isostatic rebound of 77 m. The overall regression was interrupted by two minor transgressions during the late Younger Dryas and in early Preboreal, and these were probably caused by a combination of expansions of local ice caps and readvances of the Icelandic inland ice‐sheet margin. Maximum absolute uplift rates are recorded during the regressional phase between the two transgressions (10000–9850 BP), with a mean value of c . 15 cm 14 C yr ‐1 or 11–12 cm cal. yr ‐1 . Mean absolute uplift during the regressional phase following the second transgression (9700–9100 BP) was around 6 cm 14 C yr ‐1 , corresponding to c . 3 cm cal. yr ‐1 , and relative sea level dropped below present‐day sea level at 9000 BP. |
format |
Article in Journal/Newspaper |
author |
RUNDGREN, MATS INGÓLFSSON, ÓLAFUR BJÖRCK, SVANTE JIANG, HUI HAFLIDASON, HAFLIDI |
spellingShingle |
RUNDGREN, MATS INGÓLFSSON, ÓLAFUR BJÖRCK, SVANTE JIANG, HUI HAFLIDASON, HAFLIDI Dynamic sea‐level change during the last deglaciation of northern Iceland |
author_facet |
RUNDGREN, MATS INGÓLFSSON, ÓLAFUR BJÖRCK, SVANTE JIANG, HUI HAFLIDASON, HAFLIDI |
author_sort |
RUNDGREN, MATS |
title |
Dynamic sea‐level change during the last deglaciation of northern Iceland |
title_short |
Dynamic sea‐level change during the last deglaciation of northern Iceland |
title_full |
Dynamic sea‐level change during the last deglaciation of northern Iceland |
title_fullStr |
Dynamic sea‐level change during the last deglaciation of northern Iceland |
title_full_unstemmed |
Dynamic sea‐level change during the last deglaciation of northern Iceland |
title_sort |
dynamic sea‐level change during the last deglaciation of northern iceland |
publisher |
Wiley |
publishDate |
1997 |
url |
http://dx.doi.org/10.1111/j.1502-3885.1997.tb00852.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1997.tb00852.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1997.tb00852.x |
long_lat |
ENVELOPE(-3.933,-3.933,-71.300,-71.300) |
geographic |
Boreas |
geographic_facet |
Boreas |
genre |
Ice Sheet Iceland |
genre_facet |
Ice Sheet Iceland |
op_source |
Boreas volume 26, issue 3, page 201-215 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1502-3885.1997.tb00852.x |
container_title |
Boreas |
container_volume |
26 |
container_issue |
3 |
container_start_page |
201 |
op_container_end_page |
215 |
_version_ |
1812814718824349696 |