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RESEARCH ARTICLE

Temporal variation of trace elements, rare earth elements and Pb isotope ratios in sediment core from Kiel Bay, western Baltic Sea

Anna Maria Orani A , Emilia Vassileva https://orcid.org/0000-0002-7835-5640 A E , Sabine Schmidt B , Sylvain Berail C D and Julien P. G. Barre D
+ Author Affiliations
- Author Affiliations

A International Atomic Energy Agency, Environment Laboratories, 4 Quai Antoine 1er, 98000 Monaco, Principality of Monaco.

B CNRS, OASU, UMR 5805, Environnements et Paléoenvironnements Océaniques et Continentaux (EPOC), 33615 Pessac, France.

C Université de Pau et des Pays de l’Adour, E2S UPPA, CNRS, IPREM, 64053 Pau, France.

D Advanced Isotopic Analysis, Technopole Hélioparc, 2 Avenue du Président Pierre Angot, 64000 Pau, France.

E Corresponding author. Email: e.vasileva-veleva@iaea.org

Environmental Chemistry 17(8) 579-593 https://doi.org/10.1071/EN20078
Submitted: 1 June 2020  Accepted: 15 July 2020   Published: 17 August 2020

Environmental context. Trace elements in coastal environments represent an environmental concern and their monitoring in sediment cores provides insight into their historical sources. A well-dated core from Kiel Bay, western Baltic Sea, provided trace element data, including lead, cadmium, rare earth elements, mercury and methyl mercury. Lead and mercury isotope ratios were useful for the apportionment of pollution sources, indicating that coal burning was a major contributor.

Abstract. We present a comprehensive study on the variation of trace elements (TEs) and rare earth elements (REEs) in a well-dated sediment core from Kiel Bay, western Baltic Sea. Mass fractions of 34 elements (major and trace) together with other relevant parameters, such as organic carbon and grain size, were determined in a 20-cm core that covers the last century. Enrichment factors and geoaccumulation indices were determined to assess the possible influence of anthropogenic inputs on element distribution. The obtained results show that the highest enrichment of TEs occurred in the period 1917–1970 especially for the priority elements as Hg, Cd and Pb. Determination of methylmercury (MeHg) was also performed, as it showed the highest content in surface samples. The MeHg percentages ranged from 0.02 to 1.2 % of the total Hg. REEs, which are nowadays considered as new emerging contaminants, did not reveal high enrichment attributable to anthropogenic influences, but provided useful baseline information for future monitoring of the area. The study of the Pb isotopic composition proved to be a valuable tool in determining the Pb pollution source, and revealed Pb in the layers that showed the highest enrichment came mainly from coal burning. Mercury isotopic signatures in the sediment core were used as a tool to identify the sources of Hg pollution. An isotope mixing model based on mass-dependent (MDF) and mass-independent fractionations (MIF) identified coal burning as the most probable dominant source for Hg anthropogenic contamination in the area.

Additional keywords: Hg isotope ratios, marine pollution, mercury, methylmercury, monitoring study.


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