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Title

Ostracoda and Mollusca biodiversity and hydrochemical features in Late Miocene brackish basins of Italy

AuthorsLigios, S.; Anadón, Pere ; Castorina, F.; D'Amico, C.; Esu, D.; Gliozzi, E.; Gramigna, P.; Mola, M.; Monegato, G.
KeywordsItaly
Molluscs
Late Tortonian-early Messinian
Stable isotopes
Trace elements
Ostracods
Issue Date2012
PublisherElsevier
CitationGeobios 45: 351- 367 (2012)
AbstractLate Miocene brackish ostracods and molluscs collected in three Italian basins show noticeable differences in their taxonomic composition, despite their capability of dispersing across wide geographic areas. In the Venetian-Friulian Basin (northern Italy), the upper Tortonian sediments contain oligotypic ostracod assemblages including Hemicyprideis dacica dacica, Hemicytheria pejinovicensis, and Loxoconcha cf. L. josephi and few gastropods referable to Planorbidae and Stenothyroides, which are typical of the central Paratethys. In central Italy, the brackish ostracods and molluscs recovered from upper Tortonian-lower Messinian deposits from four Tuscan basins (Volterra-Radicondoli, Velona, Baccinello-Cinigiano, and Valdelsa) display high affinity at a generic level but strong endemicity at a specific level. At Cessaniti (southern Italy), the upper Tortonian unit contains oligotypic brackish ostracods and molluscs: Mediocytherideis (Sylvestra) posterobursa, Cyprideis ruggierii, Loxoconcha cf. L. biformata, and Zonocypris membranae quadricella characterise the ostracod fauna, while Granulolabium bicinctum and Hydrobia frauenfeldi are the dominant molluscs. The recovered ostracods have a strong affinity with brackish species from central and eastern Palaeo-Mediterranean areas, whereas the molluscs present a Paratethyan origin. Despite the fact that the basins are all brackish and partly coeval, the systematics of these assemblages highlights the absence of common species among the three studied areas. Geochemical analyses (stable isotopes and trace elements) are performed on ostracods, and 87Sr/ 86Sr ratios are established in molluscs and echinoids. The results suggest brackish environments with different compositions and origins of solutes in the three different areas. The Tuscan basins are characterised by brackish waters, with NaCl-enriched waters coming from aquifers of Triassic evaporite bedrock. The brackish deposits of the Venetian-Friulian Basin and Cessaniti are true marginal marine environments, although the northern basin may have been influenced by both the Paratethyan Sava Basin and the northern portion of the Palaeo-Mediterranean water bodies. © 2012 Elsevier Masson SAS.
Publisher version (URL)http://dx.doi.org/10.1016/j.geobios.2011.10.008
URIhttp://hdl.handle.net/10261/97473
DOI10.1016/j.geobios.2011.10.008
Identifiersdoi: 10.1016/j.geobios.2011.10.008
issn: 0016-6995
Appears in Collections:(Geo3Bcn) Artículos
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