Arrecifes de coral hermatipicos (Cladocora caespitosa) en el relleno holoceno de la zona de Es Grau (Menorca, Mediterräneo Occidental)

dc.contributor.authorFornós Astó, Joan J.
dc.contributor.authorBarón, A.
dc.contributor.authorPons, G. X.
dc.date.accessioned2016-04-08T08:04:14Z
dc.date.available2016-04-08T08:04:14Z
dc.date.issued1996
dc.description.abstractThe sedimentologic study of six cores made in the beach-barrier and lagoon of the Albufera des Crau (northeastern Menorca), reveals the presence of the upper Pleistocene - Holocene sequence that starts with a terrigenous sedimentation over an erosion surface on the Carboniferous micasquist, that grades to restricted marine muddy sediments with the stablishment of banks of the zooxanthelate scleractinia Cladocora caespitosa. The Quaternary sedimentation ends with beach-dune sandsen_US
dc.identifier.urihttp://hdl.handle.net/10272/11809
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherCoral banken_US
dc.subject.otherReefen_US
dc.subject.otherHaermatipic coralen_US
dc.subject.otherCladocora caespitosaen_US
dc.subject.otherHoloceneen_US
dc.titleArrecifes de coral hermatipicos (Cladocora caespitosa) en el relleno holoceno de la zona de Es Grau (Menorca, Mediterräneo Occidental)en_US
dc.titleHolocene haermatypic coral banks (Cladocora caespitosa) in Es Gran zone (Menorca, Western Mediterranean)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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