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Updated: Oct 15, 2025

An Anaerobic Biosensor Assay for the Detection of Mercury and Cadmium
Published on: December 17, 2018
Approaching mercury distribution in burial environment using PLS-R modelling
Noemi Álvarez-Fernández1, Antonio Martínez Cortizas2, Zaira García-López2
1CRETUS, EcoPast (GI-1553), Universidade de Santiago de Compostela, 15782, Santiago, Spain. n.alvarez.fernandez@usc.es.
Archaeological skeletons reveal past mercury levels. Body decomposition released mercury into burial soils, influencing soil properties and mercury retention over time.
Area of Science:
- Environmental Science
- Archaeology
- Toxicology
Background:
- Mercury's environmental cycle and toxicology are extensively studied.
- Historical mercury pollution necessitates understanding past trends for present-day context.
- Archaeological skeletons offer insights into past mercury exposure and loads.
Purpose of the Study:
- To investigate mercury distribution and accumulation in ancient burial soils.
- To elucidate the factors controlling mercury behavior within burial environments.
- To understand the role of decomposing human remains in mercury cycling.
Main Methods:
- A multi-sampling soil approach was used in two 5th-6th century AD burials.
- Principal Local Regression Smoothing (PLRS) modeling was applied to analyze mercury distribution.
- Analysis focused on the relationship between skeletal remains and soil mercury content.
Main Results:
- PLRS modeling explained 72% of mercury variance in the soils.
- Body decomposition was identified as the primary mercury source, altering soil properties and mercury retention.
- Mercury accumulation resulted from complex interactions between decomposing bodies and soil components.
- Variability in mercury levels correlated with proximity to the thoracic area and skeletal mass.
Conclusions:
- Decomposing skeletons act as both a source and temporary sink for mercury in burial soils.
- The fine soil fraction (silt + clay) is crucial for understanding mercury cycling in coarse-textured soils.
- Characterizing the burial soil environment is essential for comprehending soil-skeleton interactions in mercury cycling.
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