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- W2890955879 abstract "A detailed study of the latest Tortonian and earliest Messinian (Miocene) strata of North Central Sicily reveals the presence of a trans -gressive episode immediately prior to the salinity crisis. In detail two reef events are present, an earlier one (Late Tortonian) with diverse coral faunas, and a second (Early Messinian) reef episode containing both relatively diverse Porites-Tarbellastraea dominated reefs and monogeneric Porites reefs, together with the earliest diatomite deposits (Tripoli Formation). The diatomites are associated with partly isolated embayments which were the sites of algal and bacterial blooms. These probably periodically generated toxic conditions. Leakage from the diatom aceou s embayment waters into the open marine, but virtually static water, reefal areas during the Early Messinian is believed to have given a selective advantage to stromatolitic microbial mat growth. Only the rod-like growth-form of Porites ultimately was able to thrive under increasingly tranquil water conditions and strong competition from microbial mats. This was achieved by a growth strategy involving rapid apical growth of slender vertical orientated branches. The juxtapositioning of algal dominated diatom basins and coral reef basins by Late Miocene times was due to a combination of plate margin synsedimentary tectonic deformation associated with Afro-European plate collision, and normal marine eustatic events connected with the initiation of dessication of the Palaeomediterranean Basin. The model presented is applicable to all Mediterranean, late Miocene coral reef ares flanking the alpine chain affected by synsedimentary tectonism." @default.
- W2890955879 created "2018-09-27" @default.
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- W2890955879 date "1994-01-01" @default.
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- W2890955879 title "A model for the Late Miocene reef-Tripolaceous associations of Sicily and its relevance to aberrant coral growth-forms and reduced biological diversity within the Palaeomediterranean" @default.
- W2890955879 doi "https://doi.org/10.3406/geolm.1994.1501" @default.
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