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Frontiers in Marine Science · 2024 · Vol. 11 · Frontiers
In subterranean estuaries (STE), fresh and saline groundwater introduce dissolved organic matter (DOM) of different origin. This DOM serves as substrate for microorganisms that thrive in the STE. In high-energy beaches with dynamic porewater advection, microbial communities face frequent changes in groundwater composition, even at several meters depth. It is unknown how DOM from deep STE groundwater (> 5 m depth) is transforme...
Frontiers in Marine Science · 2023 · Vol. 10 · Frontiers
Subterranean estuaries are connective zones between inland aquifers and the open sea where terrestrial freshwater and circulating seawater mix and undergo major biogeochemical changes. They are biogeochemical reactors that modify groundwater chemistry prior to discharge into the sea. We propose that subterranean estuaries of high-energy beaches are particularly dynamic environments, where the effect of the dynamic boundary con...
Frontiers in Marine Science · 2022 · Vol. 8 · Frontiers
Coastal observatories are key to improve the understanding of processes within the coastal area and their interactions with regional and global environmental changes. The land-sea transition zone is an essential area that allows research on unique scientific questions under anthropogenic and natural influences. Amid the Wadden Sea UNESCO world natural heritage site – the largest tidal flat region worldwide – the barrier island...
Environmental Microbiology · 2006 · Vol. 8 · Issue 10 · Wiley
Summary Eastern Mediterranean sediments are characterized by the occurrence of distinct, organic‐rich layers, called sapropels. These harbour elevated microbial numbers in comparison with adjacent carbon‐lean intermediate layers. A recently obtained culture collection from these sediments was composed of 20% of strains closely related to Rhizobium radiobacter , formerly classified as Agrobacterium tumefaciens . To prove and qu...
Environmental Microbiology · 2006 · Vol. 8 · Issue 4 · Wiley
Summary Biogeochemical and microbiological processes in the upper sediment layers of tidal flats were analysed in many investigations, while deeper zones remained largely unexplored. Therefore, denaturant gradient gel electrophoresis (DGGE) analysis of 16S rRNA gene fragments along the depth profile of up to 5.5 m‐long sediment cores was performed in comparison with lithological and geochemical parameters. The investigation re...