Published January 15, 2013 | Version v1
Journal article

Improving the 210Pb-chronology of Pb deposition in peat cores from Chao de Lamoso (NW Spain)

  • 1. Departament de Física, Universitat Autònoma de Barcelona, E-08193 Bellaterra (Spain)
  • 2. Department of Ecology and Environmental Science, Umeå University, SE-901 87 Umeå (Sweden)
  • 3. Institut de Ciència i Tecnologia Ambientals (ICTA), Universitat Autònoma de Barcelona, E-08193 Bellaterra (Spain)
  • 4. Departamento de Edafoloxía e Química Agrícola, Universidade de Santiago de Compostela, E-15782 Santiago de Compostela (Spain)

Description

The natural radionuclide 210Pb is commonly used to establish accurate and precise chronologies for the recent (past 100–150 years) layers of peat deposits. The most widely used 210Pb-dating model, Constant Rate of Supply (CRS), was applied using data from three peat cores from Chao de Lamoso, an ombrotrophic mire in Galicia (NW Spain). On the basis of the CRS-chronologies, maximum Pb concentrations and enrichment factors (EFs) occurred in the 1960s and late 1970s, consistent with the historical use of Pb. However, maximum Pb fluxes were dated in the 1940s and the late 1960s, 10 to 20 years earlier. Principal component analysis (PCA) showed that, although the 210Pb distribution was mainly (74%) controlled by radioactive decay, about 20% of the 210Pb flux variability was associated with atmospheric metal pollution, suggesting an extra 210Pb supply source and thus invalidating the main assumption of the CRS model. When the CRS-ages were recalculated after correcting for the extra input from the 210Pb inventory of the uppermost peat layers of each core, Pb flux variations were consistent with the historical atmospheric Pb deposition. Our results not only show the robustness of the CRS model to establish accurate chronologies of recent peat deposits but also provide evidence that there are confounding factors that might influence the calculation of reliable peat accumulation rates (and thus also element accumulation rates/fluxes). This study emphasizes the need to verify the hypotheses of 210Pb-dating models and the usefulness of a full geochemical interpretation of peat bog records. - Highlights: ► Peat cores collected in NW Spain were used to reconstruct recent Pb deposition. ► Applicability of 210Pb-dating models (CRS) in bogs is discussed based on PCA results. ► Results showed that ∼ 20% of the 210Pb flux was related to anthropogenic metal pollution. ► Geochemical analysis of bogs is useful to interpret the historical peat record

Availability note (English)

Available from http://dx.doi.org/10.1016/j.scitotenv.2012.10.107

Additional details

Identifiers

DOI
10.1016/j.scitotenv.2012.10.107;
PII
S0048-9697(12)01426-X;

Publishing Information

Journal Title
Science of the Total Environment
Journal Volume
443
Journal Page Range
p. 597-607
ISSN
0048-9697
CODEN
STENDL

Optional Information

Copyright
Copyright (c) 2012 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.