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Unravelling the anthropogenic pressures in deep waters of the N Iberian Peninsula in the last centuries through the study of sediment cores
Summary
Researchers analyzed sediment cores from eight deep-sea sites in the NW Mediterranean and Cantabrian Sea, using lead-210 dating and chemical analysis to reconstruct centuries of marine pollution history. Microplastics appeared in cores from the mid-20th century onward, with metal and plastic pollution accelerating sharply after industrialization and intensifying since the 1970s.
The greatest degradation of marine ecosystems has occurred in the last two centuries, coinciding with changes in economic and production models such as the industrialisation. We reconstructed the recent history (last centuries) of marine pollutants (metals and microplastics) in the deep sea of the NW Mediterranean and the Cantabrian Sea (NE Atlantic), analysing 8 sites (cores) at depths between 87 and 1151 m with different levels of terrestrial/oceanic influence. The Pb dating showed higher sedimentation rates (MAR) in the upper slope and/or closer to the mainland (0.063-0.078 g/cm/yr off Barcelona; 0.107 g/cm/yr in Mallorca at 420 m depth) than in deeper and more open marine stations (MAR = 0.054-0.035 g/cm/yr), including the Valencia seamount (VS). In terms of metal pollution history, Hg and Pb were good markers of industrial activity, at all stations, including those at 1100-1150 m off Mallorca and on the VS summit. As (arsenic) peaked in the late 19th-early 20th centuries, due to the use of coal as a fuel in steamboats. The role of other metals (e.g. V, Cr, Cd, or Cu) is interpreted locally, depending on the type of industry developed in each area. The rapid and widespread emergence and use of microplastics also made them a good historical marker for sediments. The lithogenic metals Li and Al were good tracers of natural changes (freshwater input, precipitation regime) as their concentration in deep sediments is linked to advective fluxes reaching the seafloor. Both showed a general decline after the middle of the 20th century (1960s), due to a reduction in rainfall and river discharge, as well as an increase in river damming. The observed changes can therefore be explained by a combination of natural variability and the impact of human activities.
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