Structural equation modeling of long-term controls on mercury and bromine accumulation in Pinheiro mire (Minas Gerais, Brazil).

Bromine Late Pleistocene-Holocene Mercury Structural equation modeling

Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
25 Feb 2021
Historique:
received: 26 08 2020
revised: 08 11 2020
accepted: 16 11 2020
pubmed: 16 12 2020
medline: 16 12 2020
entrez: 15 12 2020
Statut: ppublish

Résumé

The application of statistical modeling is still infrequent in mercury research in peat, despite the ongoing debate on the weight of the diverse factors (climate, peat decomposition, vegetation changes, etc.) that may affect mercury accumulation. One of the few exceptions is the Hg record of Pinheiro mire (souheast Brazil). Previous studies on this mire modeled mercury using principal components regression and partial least squares. These methods assume independence between factors, which is seldom the case in natural systems, thus hampering the identification of mediating effects and interactions. To overcome these limitations, in this reserach we use structural equation modeling (PLS-SEM) to model mercury and bromine peat records - bromine has been used in some investigations to normalize mercury accumuation. The mercury model explained 83% of the variance and suggested a complex control: increased peat decomposition, dust deposition and humid climates enhanced mercury accumulation, while increased mineral fluxes resulted in a decrease in mercury accumulation. The bromine model explained 90% of the variation in concentrations: increased dust deposition and peat decomposition promoted bromine accumulation, while time (i.e. peat age) promoted bromine depletion. Thus, although mercury and bromine are both organically bound elements with relevant atmospheric cycles the weights of the factors involved in their accumulation differed significantly. Our results suggest caution when using bromine to normalize mercury accumulation. PLS-SEM results indicate a large time dependence of peat decomposition, catchment mineral fluxes, long-term climate change, and atmospheric deposition; while atmospheric dust, mineral fluxes and peat decomposition showed high to moderate climate dependency. In particular, they also point to a relevant role of autogenic processes (i.e. the build up and expansion of the mire within the catchment), which controlled local mineral fluxes; an aspect that has seldom been considered.

Identifiants

pubmed: 33321335
pii: S0048-9697(20)37471-4
doi: 10.1016/j.scitotenv.2020.143940
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

143940

Informations de copyright

Crown Copyright © 2020. Published by Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

Antonio Martínez Cortizas (A)

Ecopast (GI-1553), Facultade de Bioloxía, Universidade de Santiago de Compostela, Santiago de Compostela, Spain. Electronic address: antonio.martinez.cortizas@usc.es.

Ingrid Horák-Terra (I)

Instituto de Ciências Agrárias, Universidade Federal dos Vales do Jequitinhonha e Mucuri, Unaí, Brazil.

Marta Pérez-Rodríguez (M)

Institut für Geoökologie, Technische Universität Braunschweig, Braunschweig, Germany.

Richard Bindler (R)

Department of Ecology and Environmental Science, University of Umea, Umea, Sweden.

Colin A Cooke (CA)

Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Canada.

Malin Kylander (M)

Department of Geological Sciences, Stockholm University, Stockholm, Sweden.

Classifications MeSH