Carbonate deposition and diagenesis in evaporitic environments: The evaporative and sulphur-bearing limestones during the settlement of the Messinian Salinity Crisis in Sicily and Calabria

Author:

Caruso A.,Pierre C.,Blanc-Valleron M.-M.,Rouchy J.M.

Funder

INSU, CNRS

Italian funds

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference70 articles.

1. Biomarker and isotope evidence for microbially-mediated carbonate formation from gypsum and petroleum hydrocarbons;Aloisi;Chem. Geol.,2013

2. Biogenic carbonates: are they a criterion for underlying hydrocarbon accumulations? An example from the Gulf of Suez region, Egypt;Aref;Am. Assoc. Pet. Geol. Bull.,1998

3. Evaporite carbonate cycles of the Messinian, Sicily: stable isotopes, mineralogy, textural features, and environmental implications;Bellanca;J. Sediment. Petrol.,1986

4. Isotope geochemistry, petrology and depositional environments of the diatomite-dominated Tripoli Formation (Lower Messinian), Sicily;Bellanca;Sedimentology,1986

5. Transition from marine to hypersaline conditions in the Messinian Tripoli Formation from the marginal areas of the central Sicilian Basin;Bellanca;Sediment. Geol.,2001

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