0000000000354192

AUTHOR

Matteo Vacchi

0000-0002-1569-7862

showing 4 related works from this author

Preservation of modern and mis 5.5 erosional landforms and biological structures as sea level markers: A matter of luck?

2021

The Mediterranean Basin is characterized by a significant variability in tectonic behaviour, ranging from subsidence to uplifting. However, those coastal areas considered to be tectonically stable show coastal landforms at elevations consistent with eustatic and isostatic sea level change models. In particular, geomorphological indicators—such as tidal notches or shore platforms—are often used to define the tectonic stability of the Mediterranean coasts. We present the results of swim surveys in nine rocky coastal sectors in the central Mediterranean Sea using the Geoswim approach. The entire route was covered in 22 days for a total distance of 158.5 km. All surveyed sites are considered to…

Marine isotope stageSettore BIO/07 - EcologiaErosion -- Mediterranean RegionBiological indicators; Coastal geomorphology; Geoswim; Landforms; Mediterranean Sea; MIS 5.5; Sea level change010504 meteorology & atmospheric sciencesGeography Planning and DevelopmentGeoswimAquatic ScienceCoastal geography010502 geochemistry & geophysicsBiological indicator01 natural sciencesBiochemistryNeotectonics -- Mediterranean RegionMediterranean seaMediterranean SeaSea level changeTD201-500Sea level0105 earth and related environmental sciencesWater Science and TechnologyShoregeographyPast sea levelgeography.geographical_feature_categorycoastal geomorphologyWater supply for domestic and industrial purposesCoast changes -- Mediterranean Region -- Case studiesSubsidenceHydraulic engineeringcoastal geomorphology MIS 5.5 landforms biological indicators sea level change Mediterranean Sea GeoswimSettore GEO/01 - Paleontologia E Paleoecologiabiological indicatorsCoastal geomorphologyMIS 5Sea level -- Mediterranean RegionMIS 5.5LandformInterglacialBeach erosion -- Mediterranean RegionPhysical geographyTC1-978landformssea level changeGeology
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Geoarchaeology as a tool to understand ancient navigation in the northern Persian Gulf and the harbour history of Siraf

2020

International audience; Historical texts and archaeological studies attest to the maritime and trade importance of the Persian Gulf since the Sassanid Empires. Nonetheless, there is a paucity of data regarding ancient navigation and the reasons for a shift in m aritim e trade from the western (e.g. Shatt-al-Arab) to eastern (Siraf) Persian Gulf by the Abbasid dynasty. For som e scholars, Siraf was occupied between 360 and 977 CE, after which tim e an earthquake en-trained the dem ise of the city. However, it is unclear when Siraf was founded and how natural navigation conditions changed for ocean-going vessels in harbours of the NW Persian Gulf. To address this knowledge gap, we here presen…

010506 paleontologyArcheologyPersian GulfSirafCoastal geographyHiatusSiraf Geoarchaeology Persian Gulf Shamal winds Coastal geomorphology Relative sea level01 natural sciencesNatural (archaeology)0601 history and archaeology14. Life underwaterShamalGeoarchaeology0105 earth and related environmental sciencescomputer.programming_language060102 archaeologyGeoarchaeology06 humanities and the artsDemiseArchaeologyCoastal geomorphologyCoastal erosionGeography13. Climate actionRelative sea levelHarbour[SDE]Environmental SciencesShamal windscomputer
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Geospatial modelling and map analysis allowed measuring regression of the upper limit of Posidonia oceanica seagrass meadows under human pressure

2018

Abstract Marine coastal ecosystems are facing structural and functional changes due to the increasing human footprint worldwide, and the assessment of their long-term changes becomes particularly challenging. Measures of change can be done by comparing the observed ecosystem status to a purposely defined reference condition. In this paper, a geospatial modelling approach based on 2D mapping and morphodynamic data was used to predict the natural position of the upper limit (i.e., the landward continuous front) of Posidonia oceanica seagrass meadows settled on soft bottom. This predictive model, formerly developed at the regional spatial scale, was here applied for the first time at the Medit…

Settore BIO/07 - Ecologia0106 biological sciencesMediterranean climateGeospatial analysis010504 meteorology & atmospheric sciencesMediterranean sea Morphodynamic sPosidonia oceanica Predictive modelling Reference conditions SeagrassAquatic ScienceOceanographycomputer.software_genre01 natural sciencesMorphodynamicZoologíaEcosystemSeagrasssPosidonia oceanica0105 earth and related environmental sciencesbiology010604 marine biology & hydrobiologySeagraPredictive modellingFragmentation (computing)Posidonia oceanicaReference conditionsbiology.organism_classificationSeagrass;Predictive modelling;Reference conditions;Morphodynamics;Posidonia oceanica;Mediterranean seaMorphodynamicsRegressionSeagrassPosidonia oceanicaSettore BIO/03 - Botanica Ambientale E ApplicataMediterranean seaSpatial ecologyEnvironmental scienceReference conditionPhysical geographycomputerEstuarine, Coastal and Shelf Science
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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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