Triásico medio de Bugarra (Valencia. España) ...
DOI:
https://doi.org/10.3989/egeol.84405-6675Keywords:
Carbonate shelf, Tidal deposits, Mollusca, Muschelkalk, Triassic, Iberian Range, Valencia, Spain.Abstract
The Middle Triassic material sequence (Muschelkalk) nearly the village of Bugarra (Meridional lberian Range, Valencia, Spain) has been considered, in base its faunistic and litoestratigraphic aspects, as equivalent to the upper MuschelkaIk (M-3) of Catalan Ranges (Virgili, 1958). Several cycles, thickening and coarsening upward, made out the lower section, wich is formed by thin bedded micritic dolomites in its lower part. The same, D. cf. lommelii (WISS.) and Nautiloidea are present in that. The upper section of the series correspond to a very shallow sediment in a inter-supra tidal environment. It is formed by micritic dolomite with stromatolites, criptoalgal laminites, mudcracks, tepees, rain pits and evaporite pseudomorphs. A very rich bivalves comunity is presento in the boundary between the upper and lower sections. It is represented by: Neoschizodus laevigatus (GOLD.), Placunopsis teruelensis WURM, Bakevellia costata (SSHLO'TH.), Pseudocorbula gregaria (MUNST.). The occurrence of D. cf. lommeli permit us to date the studied series as middle-upper Ladinian.
Downloads
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 1984 Consejo Superior de Investigaciones Científicas (CSIC)
This work is licensed under a Creative Commons Attribution 4.0 International License.
© CSIC. Manuscripts published in both the print and online versions of this journal are the property of the Consejo Superior de Investigaciones Científicas, and quoting this source is a requirement for any partial or full reproduction.
All contents of this electronic edition, except where otherwise noted, are distributed under a Creative Commons Attribution 4.0 International (CC BY 4.0) licence. You may read here the basic information and the legal text of the licence. The indication of the CC BY 4.0 licence must be expressly stated in this way when necessary.
Self-archiving in repositories, personal webpages or similar, of any version other than the final version of the work produced by the publisher, is not allowed.
