Variable Be-10 fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record?

A 650-yr-long sediment sequence from a crater lake on Tristan da Cunha, South Atlantic, was analysed for its Be-10 content. Based on C-14 dating, and sedimentary, geochemical, magnetic and palynological records, the period between 900 and 1450 AD appears to have been unusually stable in terms of sed...

Full description

Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Ljung, Karl, Björck, Svante, Muscheler, Raimund, Beer, Juerg, Kubik, Peter
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2007
Subjects:
Online Access:https://lup.lub.lu.se/record/689793
https://doi.org/10.1016/j.quascirev.2006.12.016
id ftulundlup:oai:lup.lub.lu.se:ad79feba-96a4-4729-af9e-59f68454de40
record_format openpolar
spelling ftulundlup:oai:lup.lub.lu.se:ad79feba-96a4-4729-af9e-59f68454de40 2023-05-15T16:39:11+02:00 Variable Be-10 fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record? Ljung, Karl Björck, Svante Muscheler, Raimund Beer, Juerg Kubik, Peter 2007 https://lup.lub.lu.se/record/689793 https://doi.org/10.1016/j.quascirev.2006.12.016 eng eng Elsevier https://lup.lub.lu.se/record/689793 http://dx.doi.org/10.1016/j.quascirev.2006.12.016 wos:000248732200001 scopus:34248326071 Quaternary Science Reviews; 26(7-8), pp 829-835 (2007) ISSN: 0277-3791 Geology contributiontojournal/article info:eu-repo/semantics/article text 2007 ftulundlup https://doi.org/10.1016/j.quascirev.2006.12.016 2023-02-01T23:32:33Z A 650-yr-long sediment sequence from a crater lake on Tristan da Cunha, South Atlantic, was analysed for its Be-10 content. Based on C-14 dating, and sedimentary, geochemical, magnetic and palynological records, the period between 900 and 1450 AD appears to have been unusually stable in terms of sedimentation and vegetation and therefore this period was chosen for analysis of the Be-10 content. During this period of highly organic sedimentation and closed vegetation, the pattern of Be-10 flux variations follows the Be-10 fluctuations from the GRIP ice core and estimated C-14 production rates well. However, before and after this stable period, variable sedimentation rates have to be accounted for to obtain results that are comparable to the established Be-10/C-14 records. Our data show not only the possibility of obtaining detailed enough Be-10 flux data from sedimentary sequences to reconstruct past solar forcing but also how sensitive this type of record is to sedimentary and environmental changes. If suitable archives can be found, they have the potential to improve reconstructions of solar activity far back in time. (c) 2007 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper ice core Lund University Publications (LUP) Crater Lake ENVELOPE(-60.667,-60.667,-62.983,-62.983) Tristan ENVELOPE(140.900,140.900,-66.735,-66.735) Quaternary Science Reviews 26 7-8 829 835
institution Open Polar
collection Lund University Publications (LUP)
op_collection_id ftulundlup
language English
topic Geology
spellingShingle Geology
Ljung, Karl
Björck, Svante
Muscheler, Raimund
Beer, Juerg
Kubik, Peter
Variable Be-10 fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record?
topic_facet Geology
description A 650-yr-long sediment sequence from a crater lake on Tristan da Cunha, South Atlantic, was analysed for its Be-10 content. Based on C-14 dating, and sedimentary, geochemical, magnetic and palynological records, the period between 900 and 1450 AD appears to have been unusually stable in terms of sedimentation and vegetation and therefore this period was chosen for analysis of the Be-10 content. During this period of highly organic sedimentation and closed vegetation, the pattern of Be-10 flux variations follows the Be-10 fluctuations from the GRIP ice core and estimated C-14 production rates well. However, before and after this stable period, variable sedimentation rates have to be accounted for to obtain results that are comparable to the established Be-10/C-14 records. Our data show not only the possibility of obtaining detailed enough Be-10 flux data from sedimentary sequences to reconstruct past solar forcing but also how sensitive this type of record is to sedimentary and environmental changes. If suitable archives can be found, they have the potential to improve reconstructions of solar activity far back in time. (c) 2007 Elsevier Ltd. All rights reserved.
format Article in Journal/Newspaper
author Ljung, Karl
Björck, Svante
Muscheler, Raimund
Beer, Juerg
Kubik, Peter
author_facet Ljung, Karl
Björck, Svante
Muscheler, Raimund
Beer, Juerg
Kubik, Peter
author_sort Ljung, Karl
title Variable Be-10 fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record?
title_short Variable Be-10 fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record?
title_full Variable Be-10 fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record?
title_fullStr Variable Be-10 fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record?
title_full_unstemmed Variable Be-10 fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record?
title_sort variable be-10 fluxes in lacustrine sediments from tristan da cunha, south atlantic: a solar record?
publisher Elsevier
publishDate 2007
url https://lup.lub.lu.se/record/689793
https://doi.org/10.1016/j.quascirev.2006.12.016
long_lat ENVELOPE(-60.667,-60.667,-62.983,-62.983)
ENVELOPE(140.900,140.900,-66.735,-66.735)
geographic Crater Lake
Tristan
geographic_facet Crater Lake
Tristan
genre ice core
genre_facet ice core
op_source Quaternary Science Reviews; 26(7-8), pp 829-835 (2007)
ISSN: 0277-3791
op_relation https://lup.lub.lu.se/record/689793
http://dx.doi.org/10.1016/j.quascirev.2006.12.016
wos:000248732200001
scopus:34248326071
op_doi https://doi.org/10.1016/j.quascirev.2006.12.016
container_title Quaternary Science Reviews
container_volume 26
container_issue 7-8
container_start_page 829
op_container_end_page 835
_version_ 1766029508870144000