Search results for "sea-level changes"

showing 3 items of 3 documents

Quaternary marine and continental unconformity-bounded stratigraphic units of the NW Sicily coastal belt

2017

In the coastal sector of NW Sicily, the regional correlation of relevant unconformities recognised within the Quaternary sedimentary successions allowed the mapping of seven unconformity-bounded stratigraphic units (UBSUs). The regional unconformities are marine or subaerial erosional surfaces, as well as non-depositional surfaces, locally marked by paleosoils. The erosional surfaces were produced from marine abrasion, surface water overland/concentrated flow, river erosion, karst solution, mass movement, or wind erosion. The main lithofacies of the Quaternary UBSUs consist of: (a) marine and coastal bioclastic calcarenites, (b) aeolian sandstones, (c) river deposits, (d) colluvial deposits…

010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaNW Sicilyquaternary continental and marine depositsGeography Planning and DevelopmentGeochemistryquaternary continental and marine deposit010502 geochemistry & geophysics01 natural sciencesUnconformitylcsh:G3180-9980Earth and Planetary Sciences (miscellaneous)tectonicsclimateGeomorphologyUnconformity-bounded stratigraphic unit0105 earth and related environmental sciencesColluviumlcsh:Mapsgeographygeography.geographical_feature_categoryUnconformity-bounded stratigraphic unitsKarsttectonicsea-level changeTectonicsSubaerialErosionSedimentary rocksea-level changesQuaternaryGeologyUnconformity-bounded stratigraphic units; quaternary continental and marine deposits; tectonics; sea-level changes; climate; NW SicilyJournal of Maps
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8000 years of coastal changes on a western Mediterranean island: A multiproxy approach from the Posada plain of Sardinia

2018

Abstract A multi-proxy palaeoenvironmental investigation was conducted to reconstruct the Holocene history of coastal landscape change in the lower Posada coastal plain of eastern Sardinia. In the Mediterranean region, coastal modifications during the Holocene have been driven by a complex interplay between climate, geomorphological processes and human activity. In this paper, millennial-scale human-sea level-environment interactions are investigated near Posada, one of the largest coastal plains in eastern Sardinia. Biostratigraphic and palynological approaches were used to interpret the chrono-stratigraphy exhibited by a series of new cores taken from the coastal plain. This new study elu…

Mediterranean climate010506 paleontologyCoastal evolution010504 meteorology & atmospheric sciencesHUMAN IMPACTCoastal plainpalaeoenvironmental reconstructionsCLIMATE CHANGESPALEOENVIRONMENTAL RECONSTRUCTIONOceanographyPalaeoenvironmental reconstructions01 natural scienceseastern sardiniaPrehistoryGeochemistry and PetrologyMediterranean Seacoastal evolution; palaeoenvironmental reconstructions; sea-level changes; pollen; eastern sardinia; mediterranean seaBRONZE-AGEmediterranean seaHolocene0105 earth and related environmental sciencesSea-level changesShorePalynologygeographygeography.geographical_feature_categoryLAST 6000 YEARSSedimentGeologyEastern SardiniaRECONSTRUCTING PAST LANDSCAPESGEOARCHAEOLOGICAL EVIDENCEpollenTYRRHENIAN COASTPeriod (geology)PollenPhysical geographyALIMINI PICCOLOsea-level changesGeologycoastal evolution
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Sea-level changes during the last 41,000 years in the outer shelf of the southern Tyrrhenian Sea: Evidence from benthic foraminifera and seismostrati…

2011

Abstract An integrated high resolution study based both on a seismostratigraphic approach and on a sedimentary core (VIB 10), collected in the outer shelf (127 m depth) from the southern Tyrrhenian Sea (Gulf of Termini, Sicily), provides new data about climatic, eustatic and paleoenvironmental changes during the last ∼41,000 years. The results based on the interpretation of a seismic profile, on benthic foraminifera assemblages and on δ18O records, allowed recognition of two drastic sea-level falls during the Last Glacial Maximum (LGM) and the Younger Dryas (YD). The short deglacial event, between LGM and YD, known as Bolling/Allerod, played an important role in the sea-level rise that prod…

Tyrrhenian Sea010506 paleontologySettore GEO/02 - Geologia Stratigrafica E Sedimentologicaδ18O[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Holocene climatic optimumbenthic foraminifera[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]010502 geochemistry & geophysics01 natural sciencesAllerød oscillationstable isotopes.ForaminiferaSea-level changeSea-level changes; Tyrrhenian Sea; benthic foraminifera; seismostratigraphic analysis; stable isotopes.14. Life underwaterYounger DryasSea levelComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyLast Glacial MaximumSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationOceanography13. Climate actionBenthic zoneseismostratigraphic analysiGeology
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