http://www.cnr.it/ontology/cnr/individuo/prodotto/ID183246
Foraminiferal assemblages of the Bric della Muda laminites (Nizza Monferrato, Piedmont): Proxies of cyclic paleoenvironmental changes in the Lower Messinian of North-western Italy. (Articolo in rivista)
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- Foraminiferal assemblages of the Bric della Muda laminites (Nizza Monferrato, Piedmont): Proxies of cyclic paleoenvironmental changes in the Lower Messinian of North-western Italy. (Articolo in rivista) (literal)
- Anno
- 2007-01-01T00:00:00+01:00 (literal)
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Violanti D.; Gallo L.M.; Rizzi A. (2007)
Foraminiferal assemblages of the Bric della Muda laminites (Nizza Monferrato, Piedmont): Proxies of cyclic paleoenvironmental changes in the Lower Messinian of North-western Italy.
in GEOBIOS; Elsevier, Amsterdam (Paesi Bassi)
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- Violanti D.; Gallo L.M.; Rizzi A. (literal)
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- Istituto Geoscienze e Georisorse (literal)
- Titolo
- Foraminiferal assemblages of the Bric della Muda laminites (Nizza Monferrato, Piedmont): Proxies of cyclic paleoenvironmental changes in the Lower Messinian of North-western Italy. (literal)
- Abstract
- Foraminiferal assemblages in laminites cropping out at the Bric (i.e. Hill) della Muda (Nizza Monferrato, Piedmont, Northwestern Italy)
document deep marine conditions during the early Messinian, spanning a time-interval approximating, or slightly wider than the stratigraphic
range of Globorotalia nicolae (6.82-6.72 Ma). Fluctuations in abundance of planktonic warm-water oligotrophic taxa and cold-water eutrophic
species show a cyclical pattern, very comparable to variations measured in cyclically-bedded formations of the pre-evaporitic Messinian in the
Mediterranean area. A subtropical climate with cyclic warmer and cooler episodes, characterized by surface water stratification and vertical mixing
in the water column, respectively, is also documented. A depositional depth close to or larger than 1000 m is inferred on the basis of planktonic
assemblages yielding also the deep planktonic Hastigerinella digitata and of very high P/(P + B) ratios. Anoxic or strongly dysoxic bottom
conditions are indicated by the absence or rareness of benthic foraminifers, which are represented by taxa tolerant of low-oxygen or high organic
content (Bolivina pseudoplicata, Chilostomella oolina, Globobulimina affinis). A slight decrease in P/(P + B) ratios, and the presence of rare
shallow-water forms in the uppermost layers suggest a mild dysoxia and a probable shallowing, when compared with coeval events in Northern
Apennines and Southern Greece sections. (literal)
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