Stable lead (Pb) isotopes and concentrations - A useful independent dating tool for Baltic Sea sediments

The prehistory of the Baltic Sea has for a long time suffered from imprecise dating, due to the large uncertainties associated with bulk radiocarbon dating of Baltic Sea sediments. To constrain the timing of environmental changes in the Baltic Sea it is critical to apply new dating approaches. This...

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Published in:Quaternary Geochronology
Main Authors: Zillén, Lovisa, Lenz, Conny, Jilbert, Tom
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2012
Subjects:
Online Access:https://lup.lub.lu.se/record/2516998
https://doi.org/10.1016/j.quageo.2011.11.001
id ftulundlup:oai:lup.lub.lu.se:c81dc113-418e-4e0b-a6c0-25e27d7e3f23
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spelling ftulundlup:oai:lup.lub.lu.se:c81dc113-418e-4e0b-a6c0-25e27d7e3f23 2023-05-15T16:27:59+02:00 Stable lead (Pb) isotopes and concentrations - A useful independent dating tool for Baltic Sea sediments Zillén, Lovisa Lenz, Conny Jilbert, Tom 2012 https://lup.lub.lu.se/record/2516998 https://doi.org/10.1016/j.quageo.2011.11.001 eng eng Elsevier https://lup.lub.lu.se/record/2516998 http://dx.doi.org/10.1016/j.quageo.2011.11.001 wos:000301311900005 scopus:84856595588 Quaternary Geochronology; 8, pp 41-45 (2012) ISSN: 1871-1014 Geology Isochrones Holocene Chronology Lead concentration Stable lead isotopes Baltic Sea contributiontojournal/article info:eu-repo/semantics/article text 2012 ftulundlup https://doi.org/10.1016/j.quageo.2011.11.001 2023-02-01T23:26:50Z The prehistory of the Baltic Sea has for a long time suffered from imprecise dating, due to the large uncertainties associated with bulk radiocarbon dating of Baltic Sea sediments. To constrain the timing of environmental changes in the Baltic Sea it is critical to apply new dating approaches. This study identifies lead pollution isochrones in Baltic Sea sediments, which have previously been recorded in lake sediment and peat deposits in northern Europe and ice cores from Greenland. These isochrones have formed through the deposition of atmospheric lead associated with historic lead production and silver mining in Europe, and more recently with the increased industrial emissions that peaked in the 1970's. Lead concentration and stable lead isotope analyses ((206)pb/Pb-207 ratios) reveal three distinct lead pollution horizons in the Baltic Sea, i.e. a Roman peak at 1 AD, a Medieval peak at 1200 AD and a peak in the 1970s. The new data will improve the chronological accuracy and precision of paleoenvironmental studies in the Baltic Sea, and for the first time, allow synchronization of Baltic Sea geological records within the basin and across Europe and the North Atlantic region (including Greenland). (C) 2011 Elsevier B.V. All rights reserved. Article in Journal/Newspaper Greenland North Atlantic Lund University Publications (LUP) Greenland Quaternary Geochronology 8 41 45
institution Open Polar
collection Lund University Publications (LUP)
op_collection_id ftulundlup
language English
topic Geology
Isochrones
Holocene
Chronology
Lead concentration
Stable lead isotopes
Baltic Sea
spellingShingle Geology
Isochrones
Holocene
Chronology
Lead concentration
Stable lead isotopes
Baltic Sea
Zillén, Lovisa
Lenz, Conny
Jilbert, Tom
Stable lead (Pb) isotopes and concentrations - A useful independent dating tool for Baltic Sea sediments
topic_facet Geology
Isochrones
Holocene
Chronology
Lead concentration
Stable lead isotopes
Baltic Sea
description The prehistory of the Baltic Sea has for a long time suffered from imprecise dating, due to the large uncertainties associated with bulk radiocarbon dating of Baltic Sea sediments. To constrain the timing of environmental changes in the Baltic Sea it is critical to apply new dating approaches. This study identifies lead pollution isochrones in Baltic Sea sediments, which have previously been recorded in lake sediment and peat deposits in northern Europe and ice cores from Greenland. These isochrones have formed through the deposition of atmospheric lead associated with historic lead production and silver mining in Europe, and more recently with the increased industrial emissions that peaked in the 1970's. Lead concentration and stable lead isotope analyses ((206)pb/Pb-207 ratios) reveal three distinct lead pollution horizons in the Baltic Sea, i.e. a Roman peak at 1 AD, a Medieval peak at 1200 AD and a peak in the 1970s. The new data will improve the chronological accuracy and precision of paleoenvironmental studies in the Baltic Sea, and for the first time, allow synchronization of Baltic Sea geological records within the basin and across Europe and the North Atlantic region (including Greenland). (C) 2011 Elsevier B.V. All rights reserved.
format Article in Journal/Newspaper
author Zillén, Lovisa
Lenz, Conny
Jilbert, Tom
author_facet Zillén, Lovisa
Lenz, Conny
Jilbert, Tom
author_sort Zillén, Lovisa
title Stable lead (Pb) isotopes and concentrations - A useful independent dating tool for Baltic Sea sediments
title_short Stable lead (Pb) isotopes and concentrations - A useful independent dating tool for Baltic Sea sediments
title_full Stable lead (Pb) isotopes and concentrations - A useful independent dating tool for Baltic Sea sediments
title_fullStr Stable lead (Pb) isotopes and concentrations - A useful independent dating tool for Baltic Sea sediments
title_full_unstemmed Stable lead (Pb) isotopes and concentrations - A useful independent dating tool for Baltic Sea sediments
title_sort stable lead (pb) isotopes and concentrations - a useful independent dating tool for baltic sea sediments
publisher Elsevier
publishDate 2012
url https://lup.lub.lu.se/record/2516998
https://doi.org/10.1016/j.quageo.2011.11.001
geographic Greenland
geographic_facet Greenland
genre Greenland
North Atlantic
genre_facet Greenland
North Atlantic
op_source Quaternary Geochronology; 8, pp 41-45 (2012)
ISSN: 1871-1014
op_relation https://lup.lub.lu.se/record/2516998
http://dx.doi.org/10.1016/j.quageo.2011.11.001
wos:000301311900005
scopus:84856595588
op_doi https://doi.org/10.1016/j.quageo.2011.11.001
container_title Quaternary Geochronology
container_volume 8
container_start_page 41
op_container_end_page 45
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