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Assessing the reliability of Holocene relative palaeointensity estimates: a case study from Swedish varved lake sediments

Stanton, Tania LU ; Nilsson, Andreas LU ; Snowball, Ian LU and Muscheler, Raimund LU (2011) In Geophysical Journal International 187(3). p.1195-1214
Abstract
We present palaeomagnetic secular variation and relative palaeointensity estimates from multiple sediment cores recovered from a varved lake sediment sequence in Kalksjon, a lake in central west Sweden. Alternating field demagnetization of discrete samples reveals natural remanent magnetizations dominated by a stable, single component. Magnetic grain size indicators-which include Day plots and first-order reversal curves-indicate that the main carrier of the natural remanence is single-domain magnetite throughout the varved sequence, which extends to similar to 9200 cal. yr BP. The millennial-scale features of the Kalksjon relative palaeointensity, inclination and declination data are well matched against the Fennoscandian master curves... (More)
We present palaeomagnetic secular variation and relative palaeointensity estimates from multiple sediment cores recovered from a varved lake sediment sequence in Kalksjon, a lake in central west Sweden. Alternating field demagnetization of discrete samples reveals natural remanent magnetizations dominated by a stable, single component. Magnetic grain size indicators-which include Day plots and first-order reversal curves-indicate that the main carrier of the natural remanence is single-domain magnetite throughout the varved sequence, which extends to similar to 9200 cal. yr BP. The millennial-scale features of the Kalksjon relative palaeointensity, inclination and declination data are well matched against the Fennoscandian master curves FENNORPIS and FENNOSTACK, and a global dipole moment reconstruction curve. There is evidence, however, of environmental bias in the relative palaeointensity estimates during specific time intervals. We find that bias is particularly pronounced during the early Holocene, specifically between similar to 9000 and 7800 cal. yr BP. During this period the bias is apparent as a series of relative palaeointensity cycles, with a wavelength of similar to 300 years. Some bias is also evident between 7800 and 3200 cal. yr BP. By comparing Kalksjon's smoothed relative palaeointensity data with the reconstructed geomagnetic field intensity from C-14 on timescales longer than 500 years-thereby removing the effect of relatively high frequency environmental bias in the early Holocene-we suggest that a distinct peak in intensity at centred on similar to 8700 cal. yr BP is a true feature of the geomagnetic field. A minimum at similar to 7400 cal. yr BP and a maximum at similar to 2500 cal. yr BP are also robust features. Our main conclusion is that sedimentary-based relative palaeointensity reconstructions must be carefully assessed if short-term, centennial variations are to be examined. (Less)
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author
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Environmental magnetism, Magnetic field, Palaeointensity, Palaeomagnetic secular variation, Rock and mineral magnetism, Europe
in
Geophysical Journal International
volume
187
issue
3
pages
1195 - 1214
publisher
Wiley-Blackwell
external identifiers
  • wos:000297114400010
  • scopus:81755173465
ISSN
0956-540X
DOI
10.1111/j.1365-246X.2011.05049.x
project
MERGE
language
English
LU publication?
yes
id
eed73ed9-fd93-4dd0-bdc0-3b9cef986037 (old id 2239710)
date added to LUP
2011-12-22 13:03:23
date last changed
2017-01-01 04:00:07
@article{eed73ed9-fd93-4dd0-bdc0-3b9cef986037,
  abstract     = {We present palaeomagnetic secular variation and relative palaeointensity estimates from multiple sediment cores recovered from a varved lake sediment sequence in Kalksjon, a lake in central west Sweden. Alternating field demagnetization of discrete samples reveals natural remanent magnetizations dominated by a stable, single component. Magnetic grain size indicators-which include Day plots and first-order reversal curves-indicate that the main carrier of the natural remanence is single-domain magnetite throughout the varved sequence, which extends to similar to 9200 cal. yr BP. The millennial-scale features of the Kalksjon relative palaeointensity, inclination and declination data are well matched against the Fennoscandian master curves FENNORPIS and FENNOSTACK, and a global dipole moment reconstruction curve. There is evidence, however, of environmental bias in the relative palaeointensity estimates during specific time intervals. We find that bias is particularly pronounced during the early Holocene, specifically between similar to 9000 and 7800 cal. yr BP. During this period the bias is apparent as a series of relative palaeointensity cycles, with a wavelength of similar to 300 years. Some bias is also evident between 7800 and 3200 cal. yr BP. By comparing Kalksjon's smoothed relative palaeointensity data with the reconstructed geomagnetic field intensity from C-14 on timescales longer than 500 years-thereby removing the effect of relatively high frequency environmental bias in the early Holocene-we suggest that a distinct peak in intensity at centred on similar to 8700 cal. yr BP is a true feature of the geomagnetic field. A minimum at similar to 7400 cal. yr BP and a maximum at similar to 2500 cal. yr BP are also robust features. Our main conclusion is that sedimentary-based relative palaeointensity reconstructions must be carefully assessed if short-term, centennial variations are to be examined.},
  author       = {Stanton, Tania and Nilsson, Andreas and Snowball, Ian and Muscheler, Raimund},
  issn         = {0956-540X},
  keyword      = {Environmental magnetism,Magnetic field,Palaeointensity,Palaeomagnetic secular variation,Rock and mineral magnetism,Europe},
  language     = {eng},
  number       = {3},
  pages        = {1195--1214},
  publisher    = {Wiley-Blackwell},
  series       = {Geophysical Journal International},
  title        = {Assessing the reliability of Holocene relative palaeointensity estimates: a case study from Swedish varved lake sediments},
  url          = {http://dx.doi.org/10.1111/j.1365-246X.2011.05049.x},
  volume       = {187},
  year         = {2011},
}