A historical record of benthic foraminifera in seasonally anoxic Lake Grevelingen, the Netherlands
Lake Grevelingen is a former branch of the Rhine-Meuse-Scheldt estuary, which was artificially transformed into a salt-water lake by a dam in 1971. This transformation induced profound changes in the biological community of the basin, which have been described as an ecodisaster, with seasonal hypoxia/anoxia occurring in the deepest parts of the lake. Here, we investigate a sediment core sampled in 2012 in the Den Osse Basin (34 m depth) of Lake Grevelingen, recording the last ~50 years and including the transition from an estuary to a salt-water lake. Sediment molybdenum (Mo) concentrations we... Mehr ...
Verfasser: | |
---|---|
Dokumenttyp: | Artikel |
Erscheinungsdatum: | 2022 |
Schlagwörter: | Anoxia / Cable bacteria / Foraminifera / Historical record / Lake Grevelingen / Taverne / Oceanography / Ecology / Evolution / Behavior and Systematics / Earth-Surface Processes / Palaeontology |
Sprache: | Englisch |
Permalink: | https://search.fid-benelux.de/Record/base-29203116 |
Datenquelle: | BASE; Originalkatalog |
Powered By: | BASE |
Link(s) : | https://dspace.library.uu.nl/handle/1874/421458 |