http://www.cnr.it/ontology/cnr/individuo/prodotto/ID28557
Late Messinian Lago-mare ostracod palaeoecology: a correspondence analysis approach. (Articolo in rivista)
- Type
- Label
- Late Messinian Lago-mare ostracod palaeoecology: a correspondence analysis approach. (Articolo in rivista) (literal)
- Anno
- 2008-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.palaeo.2007.03.055 (literal)
- Alternative label
GLIOZZI, E. a,b; & GROSSI, F a (2008)
Late Messinian Lago-mare ostracod palaeoecology: a correspondence analysis approach.
in Palaeogeography, palaeoclimatology, palaeoecology
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- GLIOZZI, E. a,b; & GROSSI, F a (literal)
- Pagina inizio
- Pagina fine
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- Rivista
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- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- a Dipartimento di Scienze Geologiche, Università degli Studi Roma Tre, Largo S. Leonardo Murialdo, 1, I-00146 Roma, Italy;
b Istituto di Geologia Ambientale e Geoingegneria, C.N.R., c/o Dipartimento di Scienze della Terra, Università \"La Sapienza\", P.le A. Moro, 5, I-00185, Roma, Italy (literal)
- Titolo
- Late Messinian Lago-mare ostracod palaeoecology: a correspondence analysis approach. (literal)
- Abstract
- In this paper two different Italian late Messinian lago-mare ostracod assemblages, dominated mainly by
extinct Paratethyan species, have been analysed by means of Detrended Correspondence Analysis (DCA). The
obtained plots have been compared and, with the help of the limited autoecological data on similar living
species and geochemical data on the sediments in which they were included, the autoecology and
synecology of the lago-mare assemblages have been inferred. In particular, it seems reasonable to suppose
that: 1) assemblages made only by pointed candonids are typical of rather deep (possibly less than one
hundred meters of depth) and freshwater/oligohaline environments; 2) assemblages mainly composed of
Leptocytheridae point to shallow (probably few tens of meters of depth) and mesohaline waters; 3)
diversified and even assemblages made both by pointed candonids and Leptocytheridae are common in
rather deep (less than one hundred meters of depth) but oligo/low mesohaline environments; 4) Caspiocypris
seems rather tolerant of brackish salinities, but prefers shallow environments; 5) Tyrrhenocythere could be an
indicator of shallow and fresh/oligohaline waters. 6) Cyprideis is an indicator of shallow waters but can
withstand a very wide salinity range. (literal)
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