Search results for "Integrated stratigraphy"

showing 3 items of 3 documents

The lower and middle Pleistocene geological record of the San Lorenzo lacustrine succession in the Sant’Arcangelo Basin (Southern Apennines, Italy)

2005

The Sant’Arcangelo Basin is located in the southern part of the Apennine chain (Basilicata). It is filled by a siliciclastic sequence 3500m thick, dated to the Late Pliocene–Middle Pleistocene time interval. In this basin an Early Middle Pleistocene fluvio-lacustrine sequence, known as San Lorenzo Cycle, has been recognised. In the upper part of the sequence, in Rifreddo, a fairly diversified small vertebrate assemblage has been recovered. The occurrence of Mimomys savini allows to the fauna to be considered as Biharian. The presence of some faunal elements such as Microtus (Terricola) arvalidens, Microtus (Iberomys) ex gr. huescarensis-brecciensis, and Macroneomys cf. brachygnathus restric…

PalynologyPaleontologyPleistoceneOutcropQuaternary lacustrine depositis Integrated stratigraphy Southern ItalyBiochronologyFaciesSettore GEO/01 - Paleontologia E PaleoecologiaStructural basinGeologic recordGeologyEarth-Surface ProcessesFaunal assemblageQuaternary International
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The Burdigalian GSSP: the missing tile to complete the Neogene interval of the Geological Time Scale

2014

Integrated stratigraphyGSSPBurdigalian GSSBurdigalian; GSSP; Geological Time ScaleBurdigalianMediterranean BasinBurdigalian GSS; Integrated stratigraphy; Mediterranean Basin; Atlantic OceanAtlantic OceanGeological Time Scale
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Benthic foraminifera as indicators of relative sea-level fluctuations: Paleoenvironmental and paleoclimatic reconstruction of a Holocene marine succe…

2017

This study presents the results of an integrated stratigraphic analysis conducted on a marine gravity core (MSK-12 C4) recovered from the outer continental shelf (82 mwater depth) of western Calabria, ~2.6 km, NE of Capo Vaticano (Eastern Tyrrhenian margin). The gravity core MSK-12 C4 recovered a stratigraphic succession of 4.18 m beneath the seafloor representing the last ~11.1 ka. Sedimentological analysis, micropaleontological quantitative analysis on benthic foraminiferal assemblages, tephrostratigraphy, sequence stratigraphic analysis of high resolution reflection seismic data recorded in the core site area and AMS 14C absolute age determinations allowed reconstructing the marine recor…

Tyrrhenian Sea010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaHolocene climatic optimum010502 geochemistry & geophysics01 natural sciencesForaminiferaPaleontologyAbsolute datingSea levelHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesStable isotopesgeographyIntegrated stratigraphygeography.geographical_feature_categoryPaleoenvironmental and paleoclimatic reconstructionbiologyContinental shelfBenthic foraminiferaSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationStable isotopeSeafloor spreadingSettore GEO/08 - Geochimica E VulcanologiaOceanographyBenthic zoneLittle Ice AgeGeology
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