Articles | Volume 31, issue 1
https://doi.org/10.1144/0262-821X11-010
https://doi.org/10.1144/0262-821X11-010
01 Feb 2012
 | 01 Feb 2012

Late Permian (Changsingian) ostracods of the Bellerophon Formation at Seis (Siusi) (Dolomites, Italy)

Wolfgang Mette and Parvaneh Roozbahani

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Cited articles

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G., Becker and M. J. M., Bless: Biotope-indicative features in Palaeozoic ostracodes: A global phenomenonIn: (Ed.), Ostracoda and Global EventsChapman & Hall, London, 421–436., 1990.
C., Bennett: A review of the Carboniferous colonisation of non-marine environments by ostracods, Senckenbergiana lethaea, 88, 37-46, 2008.
M. J. M., Bless: Late Devonian and Carboniferous ostracode assemblages and their relationship to the depositional environment, Bulletin de la Société belge de Gèologie, 92, 31-53, 1983.
M. J. M., Bless, M., Streel and G., Becker: Distribution and palaeoenvironment of Devonian to Permian ostracode assemblages in Belgium with reference to some Late Famennian to Permian marine nearshore to “brackish-water” assemblages dated by miospores, Annales de la Société géologique de Belgique, 110, 347-362, 1987.