Search results for "δ"

showing 10 items of 315 documents

Reconstruction of the paleoenvironmental changes around the Miocene-Pliocene boundary along a W-E transect across the Mediterranean

2006

Abstract In order to reconstruct the environmental changes at the end of the Messinian salinity crisis, a multidisciplinary study has been carried out with a high sampling resolution of the late Messinian–early Zanclean (Zone MPl 1) sediments along a West–East Mediterranean transect. The studied examples comprise sections from southern Spain (Vera/Almanzora), Balearic Basin (ODP Site 975), Tyrrhenian Basin (ODP Site 974), Sicily (Eraclea Minoa), Zakynthos (Kalamaki), Corfu (Aghios Stefanos), Crete (Aghios Vlasis). Previously analyzed sections from the Levantine Basin (Cyprus and ODP Sites 968 and 969) are used for comparison. The sections have been correlated using planktonic foraminiferal …

Mediterranean climate010506 paleontologySettore GEO/02 - Geologia Stratigrafica E Sedimentologicaδ18OStratigraphy[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]010502 geochemistry & geophysics01 natural sciencesMediterranean areaPlanktonic foraminiferMiocene–Pliocene transitionPaleontologyStratotype14. Life underwaterSedimentologyTransect0105 earth and related environmental sciencesSettore GEO/06 - Mineralogiaδ13CbiologyGeologySedimentologySettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationStable isotope6. Clean waterSettore GEO/08 - Geochimica E VulcanologiaAmmonia tepida13. Climate actionFaciesGeology
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Oxygen isotopes from limpet shells: Implications for palaeothermometry and seasonal shellfish foraging studies in the Mediterranean

2017

Limpet shells are common components of many archaeological sites in the Mediterranean. To test whether δ18O values from archaeological Patella caerulea shells can serve as a reliable palaeothermometer for the Mediterranean and a reliable archive of season of collection information, we collected live P. caerulea from eight Mediterranean locations in Croatia, Israel, Libya, Malta, Tunisia, and Turkey. Shell growth patterns were studied in section, and samples for oxygen isotope analysis were milled from the shells and used to calculate sea surface temperature (SST). As with other species of limpet, SST reconstructed from P. caerulea δ18O values were lower than expected from observational reco…

Mediterranean climate010506 paleontologybiologyδ18OLimpetPaleontology010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesSea surface temperatureOceanographyPatella caeruleaSclerochronologyCaeruleaArctica islandicaEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Paleoclimatic control of biogeographic and sedimentary events in Tethyan and peri-Tethyan areas during the Oxfordian (Late Jurassic)

2005

International audience; The paleobiogeographical distribution of Oxfordian ammonites and coral reefs in northern and Central Europe, the Mediterranean area, North and East Africa, and the Middle East and Central Asia is compared with the distribution in time and space of the most important lithofacies. Interest in the Oxfordian is focused on changes in facies and in biogeographical patterns that can be interpreted as the results of climatic events. Paleotemperature trends inferred from oxygen isotopes and paleoclimatic simulations are tested against fossil and facies data. A Late Callovian–Early Oxfordian crisis in carbonate production is indicated by the widespread absence of Lower Oxfordi…

Mediterranean climate010506 paleontologyδ18OHiatus010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyPaleobiogeography01 natural sciencesIsotopes of oxygenOxfordianchemistry.chemical_compoundPaleontologyAmmonites14. Life underwaterTethysPaleoclimates[SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processes[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologygeographygeography.geographical_feature_categoryPaleontologyCoral reefchemistry13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesCoralsCarbonateSedimentary rock[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology[ SDU.STU.AG ] Sciences of the Universe [physics]/Earth Sciences/Applied geology
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Ostracod palaeolimnological analysis reveals drastic historical changes in salinity, eutrophication and biodiversity loss in a coastal Mediterranean …

2013

The Albufera of Valencia, one of the largest oligohaline coastal lagoons of the Iberian Peninsula, has suffered hydrological and landscape modifications since medieval times. This paleolimnological study clears up the controversy about the factors, which drove the lake to its present state. Lithological descriptions, ostracod paleoassemblages and Cyprideis torosa (Jones, 1850) shell morphological variations and geochemistry (δ18O, δ13C and Sr/Ca) have been used to reconstruct the lake ecosystem evolution during the last two centuries. The sandy sediments at the bottom of L’Antina core (63 cm) presented a typical assemblage of brackish water ostracods, with shell-derived δ18O values, inferre…

Mediterranean climateArcheologyGlobal and Planetary ChangeEcologyBrackish waterδ13Cbiologyδ18OLake ecosystemPaleontologybiology.organism_classificationSalinityOceanographyOstracodEutrophicationGeologyEarth-Surface ProcessesThe Holocene
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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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Speleothem δ13C record suggests enhanced spring/summer drought in south-eastern Spain between 9.7 and 7.8 ka – A circum-Western Mediterranean anomaly?

2019

South-eastern Spain is one of the driest regions in Europe and thus, prone to drought. Terrestrial climate records covering the late Glacial and Holocene from this area are sparse. Here, we present a flowstone record from Cueva Victoria, south-eastern Spain, which covers the late Glacial (15 ka) to the mid-Holocene (7 ka) including the Younger Dryas (YD). Between the onset of the Bølling/Allerød (B/A) and the early Holocene, flowstone δ18O values progressively decrease in accordance with sea-surface temperatures in the Alboran Sea, indicating an increase in precipitation in south-eastern Spain and a supra-regional signal of North Atlantic temperature change. At the same time, decreasing δ13…

Mediterranean climateArcheologyGlobal and Planetary Changegeographygeography.geographical_feature_categoryEcologyδ13CAnomaly (natural sciences)PaleontologySpeleothemOceanographySpring (hydrology)Glacial periodGeologySouth easternHoloceneEarth-Surface ProcessesThe Holocene
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5. Introduction — palaeoclimate reconstructions and dating

2007

Publisher Summary This chapter describes four interglacials preceding the Holocene—that is, during the time from about 100 to 450 kyr. The first knowledge on this time has been extracted almost 40 years ago from marine deep sea cores with a sampling resolution of several thousand of years. Deep ocean sediments can be easily dated, because δ18O stratigraphy can be applied all over the ocean basins and tuned directly to the ice volume/sea-level master curve of SPECMAP, which is based on the beat of the orbital insolation cyclicities. This dynamic climate evolution of the past interglacial must have been of high importance also for the evolution of mankind. Neanderthal hominids lived and hunte…

Mediterranean climateEemiangeographyNeanderthalgeography.geographical_feature_categorybiologyδ18ODeep seaPaleontologyOut of africabiology.animalInterglacialOceanic basinGeology
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Holocene paleoclimate inferred from salinity histories of adjacent lakes in southwestern Sicily (Italy)

2016

Marked uncertainties persist regarding the climatic evolution of the Mediterranean region during the Holocene. For instance, whether moisture availability gradually decreased, remained relatively constant, or increased during the last 7000 years remains a matter of debate. To assess Holocene limnology, hydrology and moisture dynamics, the coastal lakes Lago Preola and Gorgo Basso, located in southwestern Sicily, were investigated through several stratigraphic analyses of ostracodes, including multivariate analyses of assemblages, transfer functions of salinity, and biochemical analyses of valves (Sr/Ca, δ18O and δ13C). During the early Holocene, the Gorgo Basso and Lago Preola ostracode rec…

Mediterranean climateSettore BIO/07 - Ecologia010506 paleontologyArcheology010504 meteorology & atmospheric sciencesPaleoclimateδ18OLimnologySettore BIO/05 - ZoologiaMediterranean580 Plants (Botany)01 natural sciencesPaleoclimatologySicilyEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesGlobal and Planetary Changeδ13CHoloceneArcheology (arts and humanities)PaleohydrologyGeologyEcology Evolution Behavior and SystematicSalinityOceanographyPaleosalinityOstracodeGeology
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Hydrodynamic effects on the origin and quality of organic matter for bivalves: an integrated isotopic, biochemical and transplant study

2006

Different hydrodynamic conditions can affect both the origin and the quality of organic matter available to bivalve molluscs. I chose 2 environments with very different hydrodynamics (a Mediterranean lagoon open to flow and a closed pond), but similar with regard to temperature, salinity, depth, wind exposure and algae coverage, to investigate this. The lagoon was characterised by active flow and bivalve molluscs, whereas the pond was closed off from the lagoon’s main flow but characterised by mussel beds of the highest density ever observed in the western Mediterranean. Biochemical features, 13C and 15N contents of particulate and sedimentary organic matter, and isotopic signatures of domi…

Mediterranean climateSettore BIO/07 - EcologiaFood availabilitymedia_common.quotation_subjectAquatic ScienceMediterraneanPhysical factors; Food availability; Mollusc; δ13C; δ15N; POM; SOM; MediterraneanOrganic matterQuality (business)Ecology Evolution Behavior and Systematicsmedia_commonchemistry.chemical_classificationPOMEcologyδ13CFood availabilityEcologyδ15NSOMOceanographychemistryδ13CEnvironmental scienceMolluscPhysical factorδ15N
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Effects of a small seagull colony on trophic status and primary production in a Mediterranean coastal system (Marinello ponds, Italy)

2012

Abstract Colonies of seabirds have been shown to influence nutrient cycling and primary production of coastal areas, but knowledge is still limited above all for smaller colonies. This study evaluates the influence of a small resident seagull colony (Larus michahellis Naumann, 1840) on a Mediterranean coastal system (Marinello ponds, Sicily, Italy). The presence of ornithogenic organic matter from seagull guano was first assessed at increasing distances from the colony using δ15N to indicate the effects of guano on the trophic status and primary production. The pond directly affected by guano deposition showed an anomalous water and sediment chemistry, especially regarding physico-chemical …

Mediterranean climateSettore BIO/07 - EcologiaNutrient cyclebiologyEcologyfungiδ15NAquatic ScienceOceanographyLarus michahellisbiology.organism_classificationDeposition (geology)Fisherytransitional environments yellow-legged gull seabird trophic status primary production stable isotopesbiology.animalparasitic diseasesGuanoEnvironmental scienceSeabirdTrophic level
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