Search results for "coastal plain"

showing 10 items of 20 documents

Turia river delta and coastal barrier-lagoon of Valencia (Mediterranean coast of Spain): Geomorphological processes and global climate fluctuations s…

2019

Abstract Extensive drillings and 31 new C-14 datings were used to establish the geomorphological evolution of the Turia river delta and coastal barrier-lagoon system of Valencia (Spain) over the last three millennia. Integration of geomorphological, stratigraphic, malacological, sedimentological and geoarchaeological data enables us to relate river Turia avulsions and alluvial episodes to the development of coastal spits and barriers. Geomorphological changes in the study area may also be associated with global climate events, sea-level fluctuations or anthropogenic periods in the Turia catchment. Six phases may be differentiated: (1) a major early alluviation phase during the Iberian perio…

010506 paleontologyArcheologyGlobal and Planetary ChangegeographyRiver deltageography.geographical_feature_category010504 meteorology & atmospheric sciencesCoastal plainGeologyCoastal geography01 natural sciencesPaleoclimatologyBeach ridgeAlluviumPhysical geographyProgradationEcology Evolution Behavior and SystematicsHoloceneGeology0105 earth and related environmental sciencesQuaternary Science Reviews
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ISOTOPIC TEMPERATURES FROM THE EARLY AND MID-PLIOCENE OF THE US MIDDLE ATLANTIC COASTAL PLAIN, AND THEIR IMPLICATIONS FOR THE CAUSE OF REGIONAL MARIN…

2017

Mean seasonal extreme temperatures on the seafloor calculated from the shell d 18 Oofthescallop Placopecten clintonius from the basal part of the early Pliocene Sunken Meadow Member (Yorktown Formation) in Virginia are very similar to those from the same horizon at the latitude of Cape Hatteras in North Carolina ( ~ 210 km to the south). The lowest and highest temperatures calculated from each shell (using d 18 O seawater ¼þ 0.7 % )givemean values for winter and summer of 8.4 6 1.1 8 C( 6 1 r ) and 18.2 6 0.6 8 CinVirginia,and8.6 6 0.4 8 Cand16.5 6 1.1 8 C in North Carolina (respective median temperatures: 13.3 8 C and 12.6 8 C). Patterns of ontogenetic variation in d 18 O, d 13 C and micro…

010506 paleontologygeographygeography.geographical_feature_categoryδ13CYorktown Formationδ18OCoastal plainPaleontologyOceanic climate010502 geochemistry & geophysics01 natural sciencesGulf StreamOceanographySclerochronologyPaleoclimatologyEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciences
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The New Finding of a Mycenaean Tholos in the Alluvial Deposits of the Messina Coastal Plain (north-Eastern Sicily): Stratigraphic and Palaeoenvironme…

2012

Achaeology coastal plain Holocene Mycenaean tholos Strait of Messinacoastal plainHoloceneMycenaean tholosAchaeologyStrait of MessinaSettore BIO/08 - AntropologiaArchaeology coastal plain Holocene Mycenaean Tholos Strait of Messina Anthropology
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MIS 5.5 highstand and future sea level flooding at 2100 and 2300 in tectonically stable areas of central mediterranean sea: Sardinia and the pontina …

2021

Areas of the Mediterranean Sea are dynamic habitats in which human activities have been conducted for centuries and which feature micro-tidal environments with about 0.40 m of range. For this reason, human settlements are still concentrated along a narrow coastline strip, where any change in the sea level and coastal dynamics may impact anthropic activities. We analyzed light detection and ranging (LiDAR) and Copernicus Earth observation data. The aim of this research is to provide estimates and detailed maps (in three coastal plain of Sardinia (Italy) and in the Pontina Plain (southern Latium, Italy) of: (i) the past marine transgression occurred during MIS 5.5 highstand 119 kyrss BP

Coastal plainGeography Planning and DevelopmentSubmersion (coastal management)Aquatic ScienceSardiniaBiochemistryMediterranean seaPast (MIS 5.5) and future sea level at 2100 and 2300TD201-500Sea levelWater Science and Technologygeographygeography.geographical_feature_categoryWater supply for domestic and industrial purposesFlooding (psychology)Last Glacial MaximumFuture sea levelHydraulic engineeringCentral Mediterranean coastal plainspast (MIS 5.5) and future sea level at 2100 and 2300 Sardinia Pontina Plain central Mediterranean coastal plainsPhysical geographyTC1-978Central Mediterranean coastal plains; Past (MIS 5.5) and future sea level at 2100 and 2300; Pontina Plain; SardiniaGeologyMarine transgressionPontina Plain
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Relative sea-level rise and potential submersion risk for 2100 on 16 coastal plains of the mediterranean sea

2020

The coasts of the Mediterranean Sea are dynamic habitats in which human activities have been conducted for centuries and which feature micro-tidal environments with about 0.40 m of range. For this reason, human settlements are still concentrated along a narrow coastline strip, where any change in the sea level and coastal dynamics may impact anthropic activities. In the frame of the RITMARE and the Copernicus Projects, we analyzed light detection and ranging (LiDAR) and Copernicus Earth Observation data to provide estimates of potential marine submersion for 2100 for 16 small-sized coastal plains located in the Italian peninsula and four Mediterranean countries (France, Spain, Tunisia, Cypr…

Coastal plainMediterranean climateMediterranean Sea coastal plains relative sea-level rise 2100 marine submersionlcsh:Hydraulic engineering010504 meteorology & atmospheric sciencesCoastal plainRelative sea-level riseGeography Planning and DevelopmentSubmersion (coastal management)Aquatic Science010502 geochemistry & geophysics01 natural sciencesBiochemistryMediterranean sealcsh:Water supply for domestic and industrial purposesPeninsulalcsh:TC1-978Human settlementSea level0105 earth and related environmental sciencesWater Science and Technologygeographylcsh:TD201-5002100geography.geographical_feature_categoryCoastal plainsMarine submersion2100; Coastal plains; Marine submersion; Mediterranean sea; Relative sea-level riseTectonicsMediterranean seaPhysical geographyMediterranean Sea; coastal plains; relative sea-level rise; 2100; marine submersion
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Quantifying submarine groundwater discharge in the coastal zone via multiple methods

2006

Submarine groundwater discharge (SGD) is now recognized as an important pathway between land and sea. As such, this flow may contribute to the biogeochemical and other marine budgets of near-shore waters. These discharges typically display significant spatial and temporal variability making assessments difficult. Groundwater seepage is patchy, diffuse, temporally variable, and may involve multiple aquifers. Thus, the measurement of its magnitude and associated chemical fluxes is a challenging enterprise. A joint project of UNESCO and the International Atomic Energy Agency (IAEA) has examined several methods of SGD assessment and carried out a series of five intercomparison experiments in di…

Environmental EngineeringUnited NationsCoastal plainNew YorkFresh WaterAquiferEnvironmentWater MovementsEnvironmental ChemistryTemporal scalesWaste Management and DisposalHydrologyShoregeographyHydrogeologygeography.geographical_feature_categoryEcologyGeographyWestern AustraliaGroundwater rechargePollutionSubmarine groundwater dischargeItalyMauritiusBrazilGeologyGroundwaterScience of The Total Environment
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Life history, environment and extinction of the Scallop Carolinapecten Eboreus (Conrad) in the Plio-Pleistocene of the U.S. Eastern Seaboard

2019

Plio-Pleistocene mass extinction of marine bivalves on the U.S. eastern seaboard has been attributed to declines in temperature and primary production. We investigate the relationship of growth rate in the scallop Carolinapecten eboreus to variation in these parameters to determine which contributed to its extinction. We use ontogenetic profiles of shell δ18O to estimate growth rate and seasonal temperature, microgrowth-increment data to validate δ18O-based figures for growth rate, and shell δ13C to supplement assemblage evidence of production. Postlarval growth started in the spring/summer in individuals from the Middle Atlantic Coastal Plain but in the autumn/ winter in some from the Gulf…

Extinction event010506 paleontologygeographygeography.geographical_feature_categoryExtinctionδ13CCoastal plainEcologyPaleontologyPlio-PleistoceneBiology010502 geochemistry & geophysics01 natural sciencesPredationScallopGrowth rateEcology Evolution Behavior and Systematics0105 earth and related environmental sciences
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Sedimentary features reveal transport paths for Holocene sediments on the Kristianstad coastal plain, SE Sweden.

2017

AbstractWe have investigated coastal and aeolian deposits on the Kristianstad plain in southernmost Sweden by a combination of methods that has yielded data on sedimentary features such as grain-size variations, shape and character of quartz grain surfaces (determined in light microscope and scanning electron microscope), and mineralogical composition. Such sedimentary techniques have been not applied to coastal deposits in this part of the Baltic Sea region before. The littoral, foredune and parabolic dune sands are sedimentologically similar, only a slight grain-size transformation by aeolian processes in the foredune was observed. Sand in straight-crested dunes, on the other hand, origin…

Foredunegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesCoastal plainMaturity (sedimentology)GeochemistryPaleontologyGeology010502 geochemistry & geophysics01 natural sciencesPaleosolLittoral zoneAeolian processesSedimentary rockQuartzGeomorphologyGeology0105 earth and related environmental sciences
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Historical morphogenesis of the Turia River coastal flood plain in the Mediterranean littoral of Spain

2011

Abstract The cross-referencing of sedimentological, stratigraphic, geoarchaeological and radiocarbon data enables us to establish the geomorphologic evolution of the Late Holocene coastal flood plain of the Turia River. The Holocene marine transgression formed a coastal barrier lagoon environment in the coastal plain. During the Late Holocene, increased sediments supplied to the low reach of the river promoted: (a): the progradation of deltaic coastal sandy ridges on the coastline and (b): the aggradation of the floodplain on top of the sedimentary sequence. Four phases are clearly recognised in the geoarchaeological record of the flood plain. (1): High magnitude flooding events (2800 BP to…

Hydrologygeographygeography.geographical_feature_categoryFloodplainFlood mythCoastal plainAggradationPhysical geographyProgradationCoastal floodGeologyHoloceneEarth-Surface ProcessesMarine transgressionCATENA
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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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