Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2995
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dc.contributor.authorallSánchez-Almazo, I. M.; Departamento de Estratigrafı´a y Paleontologı´a, Universidad de Granada, Campus Fuentenueva s/n, 18002, Granadaen
dc.contributor.authorallBraga, J. C.; Departamento de Estratigrafı´a y Paleontologı´a, Universidad de Granada, Campus Fuentenueva s/n, 18002, Granadaen
dc.contributor.authorallDinarès-Turell, J.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallMartín, J. M.; Departamento de Estratigrafı´a y Paleontologı´a, Universidad de Granada, Campus Fuentenueva s/n, 18002, Granadaen
dc.contributor.authorallSpiro, B.; Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UKen
dc.date.accessioned2007-12-06T15:11:22Zen
dc.date.available2007-12-06T15:11:22Zen
dc.date.issued2007en
dc.identifier.urihttp://hdl.handle.net/2122/2995en
dc.description.abstractThe Cariatiz section lies at the toe of the palaeoslope of the Messinian Cariatiz fringing reef, at the northern margin of the Neogene Sorbas Basin in SE Spain. Distal-slope reef deposits in the upper part of the section can be traced laterally to the reef core of the last episodes of reef progradation. The underlying deposits are alternating diatomitic marl, marl and silty marl that intercalate with sandstone beds. Combined lithological changes, variations in proportions of warm-water planktic foraminifera and d18O values suggest that at least seven, probably precessional, cycles are recorded throughout the Cariatiz section. The correlation of seven cycles in the pelagic deposits to seven reef progradation cycles, and associated vertical shifts in reef facies, indicates relative sea-level oscillations of several tens of metres. Biostratigraphic and palaeomagnetic data suggest that both the Cariatiz section and the fringing reef formed during the reverse polarity Chron C3r. Surface-water temperatures seem to be the major factor controlling carbonate production in the reef system. Deposition of bioclastic calcirudite and calcarenite, with no active coral growth, took place at the lowest sea-level within each reef cycle during temperature minima within each precessional cycle. Porites framework and reef-slope deposits with Halimeda gravel, in contrast, formed during temperature rises and thermal maxima within precessional cycles.en
dc.language.isoEnglishen
dc.publisher.nameBLACKWELL PUBLISHINGen
dc.relation.ispartofSedimentologyen
dc.relation.ispartofseries/54 (2007)en
dc.subjectMessinianen
dc.subjectpaleoceanographyen
dc.titlePalaeoceanographic controls on reef deposition: the Messinian Cariatiz reef (Sorbas Basin, Almería, SE Spain)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber637–660en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.10. Stratigraphyen
dc.identifier.doi10.1111/j.1365-3091.2006.00853.xen
dc.description.obiettivoSpecifico2.2. Laboratorio di paleomagnetismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorSánchez-Almazo, I. M.en
dc.contributor.authorBraga, J. C.en
dc.contributor.authorDinarès-Turell, J.en
dc.contributor.authorMartín, J. M.en
dc.contributor.authorSpiro, B.en
dc.contributor.departmentDepartamento de Estratigrafı´a y Paleontologı´a, Universidad de Granada, Campus Fuentenueva s/n, 18002, Granadaen
dc.contributor.departmentDepartamento de Estratigrafı´a y Paleontologı´a, Universidad de Granada, Campus Fuentenueva s/n, 18002, Granadaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentDepartamento de Estratigrafı´a y Paleontologı´a, Universidad de Granada, Campus Fuentenueva s/n, 18002, Granadaen
dc.contributor.departmentDepartment of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UKen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartamento de Estratigrafía y Paleontología, Facultad de Ciencias, Campus de Fuentenueva s.n., Universidad de Granada, 18002 Granada, Spain-
crisitem.author.deptDepartamento de Estratigrafı´a y Paleontologı´a, Universidad de Granada, Campus Fuentenueva s/n, 18002, Granada-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptInstituto Andaluz de Geofísica, Universidad de Granada, Granada, Spain-
crisitem.author.deptDepartment of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK-
crisitem.author.orcid0000-0002-5546-2291-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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