Search results for "Calcareous plankton"

showing 5 items of 5 documents

The Calabrian Stage redefined

2008

The name Calabrian was introduced in the geological literature by the French stratigrapher Maurice Gignoux in 1910, and later described in his important monograph (633 pages) "Les formations marines pliocènes et quaternaires de l'Italie du sud et de la Sicile" published in 1913. Detailed data were provided on several sections (Santa Maria di Catanzaro, Caraffa, Monasterace, Palermo) and on their fossil content. The Calabrian Stage has commonly been used for over fifty years as the oldest subdivision of the Quaternary, notably in the time scales of Berggren & van Couvering (1974) and Haq & Eysinga (1987). However, after the GSSP for the Pliocene/Pleistocene boundary (P/P) was approved by INQ…

BIOSTRATIGRAFIAPleistoceneQUATERNARIOMAGNETOSTRATIGRAFIABiostratigraphyStratigraphy Quaternary calcareous plankton biostratigraphyCRONOSTRATIGRAFIA STANDARDGlobal Boundary Stratotype Section and PointPaleontologyStratotypeStage (stratigraphy)ISOTOPI STABILICalabrian Stage redefinedIce ageGeneral Earth and Planetary SciencesQuaternaryGeologyMagnetostratigraphyEpisodes
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Variability in the vertical structure of the water column and paleoproductivity reconstruction in the central-western Mediterranean during the Late P…

2008

Abstract A sedimentary sequence spanning Marine Isotope Stage (MIS) 6 to MIS 2 in core LC07, recovered in the central Mediterranean, has been investigated in order to produce a high-resolution paleoceanographic reconstruction. The changes in productivity deduced from calcareous plankton relative abundances and independently confirmed by the Ba XS fluctuations are linked to the stability of the water column which is mainly controlled by the water mass temperature. During glacial intervals, productivity was generally enhanced. Oligotrophic and warmer water masses with a deepened seasonal thermocline can be inferred for most of MIS5. The magnetic properties of the sediment show increased occur…

Marine isotope stageWater massPleistocenePaleontologyMineral dustOceanographyPaleontologyWater columnOceanographyCalcareous Plankton Paleoceanography Late PleistoceneInterglacialGlacial periodThermoclineGeology
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Centennial- to millennial-scale climate oscillations in the Central-Eastern Mediterranean Sea between 20,000 and 70,000 years ago: Evidence from a hi…

2012

Abstract Here we present a high-resolution faunal, floral and geochemical (stable isotopes and trace elements) record from the sediments of Ocean Drilling Program Site 963 (central Mediterranean basin), which shows centennial/millennial-scale resemblance to the high-northern latitude rapid temperature fluctuations documented in the Greenland ice cores between 20 and 70 kyr BP. Oxygen and carbon isotopes, planktic foraminifera and calcareous nannofossil distributions suggest that Dansgaard–Oeschger (D/O) and Heinrich events (HE) are distinctly expressed in the Mediterranean climate record. Moreover, recurrent though subdued oscillations not previously identified in the Lateglacial Mediterran…

Mediterranean climateArcheologyGlobal and Planetary ChangeHeinrich eventsbiologySicily ChannelLast glacialδ18OGeologybiology.organism_classificationD-O eventsMediterranean BasinForaminiferaOceanographyPaleoceanographyIce coreCalcareous planktonCentral-eastern MediterraneanBa/Ca ratiosThermohaline circulationStadialEcology Evolution Behavior and SystematicsGlobigerinoidesGeologyStable isotopes
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ASTROCHRONOLOGY OF LATE MIDDLE MIOCENE MEDITERRANEAN SECTIONS

2004

Mediterranean climateAstrochronologyTortonianCyclostratigraphyCyclostratigraphy; Calcareous plankton; Neogene; BiostratigraphyBiostratigraphySerravallianSettore GEO/01 - Paleontologia E PaleoecologiaBiostratigraphyCyclostratigraphyNeogenePaleontologyCalcareous planktonMiddle Miocene disruptionPlanktonic ForaminiferaNeogeneGeology
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The barren Messinian Tripoli in Sicily and its palaeoenvironmental evolution: suggestions on the exploration potential

2016

New observations on the Sicily Messinian Tripoli have yielded a variably thick diatomitic, calcareous and shaly rock interval marked by an upwards disappearance of calcareous and siliceous plankton (barren lithosome), coexisting with a variability in vegetal remains and significant amounts of amorphous organic matter (AOM). Facies analysis associated with biostratigraphy and palaeoecology of the several field and borehole sections has been framed in a well-accepted chronological scheme that points to this barren interval coinciding with the stratigraphic upper and younger part of some Tripoli sections (bituminous Tripoli) located in the northern part of the study area. Biostratigraphically,…

Messinian Tripoli010506 paleontologyCalcareous Plankton BiostratigraphyPalaeoecologyGeologyDiachronousBiostratigraphy010502 geochemistry & geophysics01 natural sciencesPaleontologyTectonicsFuel TechnologyStratigraphyGeochemistry and PetrologyFaciesMagmatismEarth and Planetary Sciences (miscellaneous)PaleoecologyEconomic GeologyFacies analysiPalaeogeographyGeology0105 earth and related environmental sciencesPetroleum Geoscience
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