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- W1966070385 abstract "Well preserved laminated structures occur within the Upper Ordovician of the Cellon section in the Carnic Alps (Austria), a world-famous reference section for Silurian conodont biostratigraphy. Microfacies from the Upper Ordovician Uqua Formation were characterised by using optical and scanning electron microscopy (SEM), an environmental scanning electron microscopy coupled with microanalyses (SEM/ESEM-EDX) and a confocal laser Raman microscopy. Ferruginous laminated structures overgrowing specific skeletal fragments occur in the lower part of the studied unit in the form of finely red-to greenish coatings composed of chamosite and goethite alternating with calcite bands. Laminae have arborescent to dendrolitic morphologies. Such morphologies suggest a biomediated genesis and the existence of a potential microbial factory acting in a nearby location from which coated material was later redeposited. These ferruginous coatings around organisms are not documented within the latest Ordovician Plöcken Formation at Cellon or in the coeval Wolayer Formation elsewhere." @default.
- W1966070385 created "2016-06-24" @default.
- W1966070385 creator A5009223187 @default.
- W1966070385 creator A5014990922 @default.
- W1966070385 creator A5060562910 @default.
- W1966070385 creator A5080692436 @default.
- W1966070385 date "2009-03-01" @default.
- W1966070385 modified "2023-09-23" @default.
- W1966070385 title "Phanerozoic organic-carbon-rich marine sediments: Overview and future research challenges" @default.
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