Search results for "gla"

showing 10 items of 4378 documents

Paleogenetic and morphometric analysis of a Mesolithic individual from Grotta d'Oriente: An oldest genetic legacy for the first modern humans in Sici…

2020

Abstract Grotta d’Oriente, a coastal cave located on the island of Favignana (Sicily, Italy) is a key site for the study of the early human colonization of Sicily. Inside the cave, during different field excavations, three burials attributable to the Late Upper Palaeolithic and Mesolithic were found. The Mesolithic Oriente B individual, directly dated at 9,377 ± 25 uncal BP, was previously assigned to HV1 haplogroup using a traditional approach. However, it is well known that PCR based methods are prone to erroneous haplotype or haplogroup determination. In order to redefine the mitochondrial lineage of this Mesolithic hunter-gatherer and explore its phylogenetic position, we target-enriche…

010506 paleontologyArcheologyLineage (genetic)010504 meteorology & atmospheric sciencesMesolithic hunter-gatherersSettore BIO/08 - Antropologia01 natural sciencesHaplogroupCaveMorphometric analysisSicilyEcology Evolution Behavior and SystematicsMesolithic0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryAncient DNAHaplotypeGeologyLast Glacial MaximumArchaeologylanguage.human_languageGrotta d'OrienteAncient DNAlanguageSicilian
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Late Weichselian and Holocene record of the paleoenvironmental changes in a small river valley in Central Poland

2016

Abstract: The developmental history, from the Oldest Dryas to the Late Holocene, of a paleolake and mire located in a river valley in Central Poland was studied using high-resolution records of pollen, macrofossils, Cladocera, sedimentology, and geochemistry from a 14 C dated sediment core. We inferred temperature and water level dynamics using cladocerans and palynological and geochemical methods were employed to investigate natural fluvial activity, particularly for these elements that are difficult to find through sedimentological methods. Our research demonstrates how climate fluctuation in the Late Glacial and Holocene periods influenced the development of a paleolake and mire in a sma…

010506 paleontologyArcheologyOldest Dryasta1171010502 geochemistry & geophysics01 natural sciencesAllerød oscillationPaleontologyIce corePaleoclimatologypaleoclimateYounger DryasGlacial periodEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesGlobal and Planetary ChangeHoloceneMacrofossilGeology15. Life on landCladoceraLate Glacial13. Climate actionmultiproxy analysisPhysical geographyGeologyQuaternary Science Reviews
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Pleistocene paleoenvironmental reconstructions and mammalian evolution in South-East Asia: focus on fossil faunas from Thailand.

2006

16 pages; International audience; Mammalian faunal studies have provided various clues for a better reconstruction of hominid Quaternary paleoenvironments. Inthis work, two methods were used: (1) the cenogram method, based on a graphical representation of the mammalian communitystructure, and (2) the species richness of murine rodents to estimate climatic parameters. These methods were applied to Middle andLate Pleistocene mammalian faunas of South-East Asia, from South China to Indonesia. Special emphasis was laid on a fauna fromnorth-east Thailand dated back to approximately 170,000 years (i.e. a glacial period). This Thai fauna seems characteristic of aslightly open forested environment …

010506 paleontologyArcheologyPleistocene[SDE.MCG]Environmental Sciences/Global ChangesFauna010502 geochemistry & geophysics01 natural sciencesQuaternaryPaleontology[ SDV.EE.BIO ] Life Sciences [q-bio]/Ecology environment/BioclimatologyMammalian communityGlacial periodEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyPaleoenvironmementPalynologyGlobal and Planetary ChangeEcology[SDV.BID.EVO]Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]Geology15. Life on landThailand[ SDE.MCG ] Environmental Sciences/Global ChangesGeographyTaxon13. Climate actionInterglacialCenogram methodSpecies richness[SDV.EE.BIO]Life Sciences [q-bio]/Ecology environment/Bioclimatology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyQuaternarySpecies richness
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History of the reindeer (Rangifer tarandus) in the eastern Baltic region and its implications for the origin and immigration routes of the recent nor…

2006

A total of 45 subfossil reindeer (Rangifer tarandus) antlers and bones - artefacts excluded - have been found over the years in the Baltic countries of Estonia, Latvia and Lithuania. The relatively high number of specimens suggests a stable residence of the species in the eastern Baltic region. For the first time, 12 of these finds were radiocarbon-dated. The ages of the samples range between 12085 and 9970 C-14 yr BP (14180-11280 cal. yr BP), and cover the Lateglacial and early Holocene, a time period during which climatic conditions shifted from periglacial to temperate. The dates suggest a rapid colonization of the area during the deglaciation period and a local extinction around the Ple…

010506 paleontologyArcheologySubfossil010504 meteorology & atmospheric sciences060102 archaeologyRange (biology)EcologyGeology06 humanities and the arts15. Life on landArchaeology01 natural sciencesLocal extinctionDeglaciationTemperate climatePeriod (geology)Colonization0601 history and archaeologyHoloceneGeologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciences
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Volcanic climate forcing preceding the inception of the Younger Dryas: Implications for tracing the Laacher See eruption

2021

Climatic warming from the last glacial maximum to the current interglacial period was punctuated by a similar to 1300 years long cold period, commonly referred to as the Younger Dryas (YD). Several hypotheses have been proposed for the mechanism triggering the abrupt inception of the YD, including freshwater forcing, an extra-terrestrial impact, and aerosols from volcanic eruptions. Here, we use synchronised sulphate and sulphur records from both Greenland and Antarctic ice cores to reconstruct volcanic forcing between 13,200-12,800 a BPGICC05 (years before 1950 CE on the Greenland Ice Core Chronology 2005; GICC05). This continuous reconstruction of stratospheric sulphur injections highligh…

010506 paleontologyArcheologyYounger Dryas010504 meteorology & atmospheric sciences530 PhysicsCIRCULATIONIce cores; Laacher See eruption; Sulphate; Volcanic radiative forcing; Younger DryasSULFURForcing (mathematics)01 natural sciencesVolcanic radiative forcingANTARCTIC ICE-CORESOCEANIce coreCHRONOLOGYYounger Dryas550 Earth sciences & geologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryGeologyLast Glacial MaximumRECORDWAIS DIVIDESulphateRadiative forcingGREENLANDLaacher See eruptionVolcano13. Climate actionIce coresClimatologySYNCHRONIZATIONInterglacialClimate modelSULFATEGeologyQuaternary Science Reviews
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The first archaeometric characterization of obsidian artifacts from the archaeological site of Samshvilde (South Georgia, Caucasus)

2019

This paper presents the first results about the provenance of obsidian fragments recovered in the archaeological site of Samshvilde (South Georgia, Caucasus) with the aim to obtain knowledge related to the network distribution and procurement of obsidian in Georgia. The geochemical characterization of thirty archaeological finds was obtained by the LA-ICP-MS method, an almost non-destructive technique capable of chemically characterizing the volcanic glass. A comparison of geochemical results obtained on both archaeological artefacts and geological samples collected from Chikiani outcrop in Georgia, together with literature data of southern Caucasus and eastern Turkey, allowed us to define …

010506 paleontologyArcheologygeographyProvenancegeography.geographical_feature_category060102 archaeologyOutcrop06 humanities and the arts01 natural sciencesArchaeologyVolcanic glassObsidian Trace elements LA-ICP-MS Samshvilde GeorgiaVolcanoAnthropology0601 history and archaeologySettore GEO/09 -Georis. Miner.e Appl.Mineral.-Petrogr. per l'Ambi.ed i B.Cult.Geology0105 earth and related environmental sciencesArchaeological and Anthropological Sciences
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Diving into the Past: A Paleo Data–Model Comparison Workshop on the Late Glacial and Holocene

2019

Understanding changes in the climate of the late Pleistocene and the Holocene has long been a research topic. Studies rely on different sources of information, ranging from terrestrial and marine archives to a hierarchy of climate modeling activities. In contrast to the climate of the last millennium, novel approaches are necessary to bridge the different temporal and spatial representations of the various archives and the climate models, and to achieve a robust understanding of climate variability and climate processes on centennial-to-millennial time scales.

010506 paleontologyAtmospheric Science010504 meteorology & atmospheric sciences13. Climate actionPhysical geographyGlacial periodData model (GIS)01 natural sciencesGeologyHolocene0105 earth and related environmental sciences
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Late Quaternary palaeoenvironmental reconstruction of sediment drift accumulation in the Malta Graben (central Mediterranean Sea)

2018

The Malta Graben is a deep tectonic depression in the Sicily Channel, bounded by NW-SE normal faults and filled by thick Pliocene-Quaternary deposits. A previous analysis of a giant piston core (LC09) from the Malta Graben had revealed a wide range of sedimentary features (carbonate turbidites, bioturbated mud and scours), although the chronostratigraphic constraint of the stacking pattern has remained elusive. After establishing a reliable chronological framework based on seven radiocarbon dates for a shorter core from the Malta Graben (ANSIC03-735), a down-core analysis of planktonic foraminifer and coccolith abundance, stable isotopes and sediment grain size was carried out. Since the la…

010506 paleontologyDeep chlorophyll maximum010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaMalta Graben; Stratigraphy; Sedimentary FeaturesLast Glacial MaximumEnvironmental Science (miscellaneous)OceanographyGeotechnical Engineering and Engineering Geology01 natural sciencesGrabenPaleontologyMediterranean seaEarth and Planetary Sciences (miscellaneous)Glacial periodYounger DryasQuaternaryHoloceneGeology0105 earth and related environmental sciences
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A low seasonality scenario in the Mediterranean Sea during the Calabrian (Early Pleistocene) inferred from fossil Arctica islandica shells

2017

Understanding past seasonal temperature variability in the ocean is essential to evaluate the effects of future climate change on marine ecosystems. Here, we estimate seasonal water temperature amplitudes from stable oxygen isotope (δ18Oshell) values of fossil shells of Arctica islandica (assuming δ18Owater= + 0.9 ± 0.1‰ V-SMOW). Specimens were collected from three Pleistocene successions (Emilian and Sicilian substages of the Calabrian) in Central and Southern Italy (i.e., Rome, Lecce and Sicily). Biostratigraphic analyses from Rome Quarry deposits indicate an age between 1.6 and 1.2 Ma, whereas Sicily and Lecce successions are slightly more recent (between 1.1 and 0.62 Ma). Prior to …

010506 paleontologyEarly PleistoceneStable oxygen isotope010504 meteorology & atmospheric sciencesPleistoceneengineering.materialOceanography01 natural sciencesPaleontologyMediterranean seaSclerochronologySclerochronology14. Life underwaterGlacial periodArctica islandicaSicilyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyAragonitePaleontologybiology.organism_classificationEcology Evolution Behavior and Systematiclanguage.human_languagePaleotemperature reconstructionOceanography13. Climate actionEarth-Surface ProcesseengineeringlanguageSicilianGeology
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Direct terrestrial–marine correlation demonstrates surprisingly late onset of the last interglacial in central Europe

2011

AbstractAn interdisciplinary study of a small sedimentary basin at Neumark Nord 2 (NN2), Germany, has yielded a high-resolution record of the palaeomagnetic Blake Event, which we are able to place at the early part of the last interglacial pollen sequence documented from the same section. We use this data to calculate the duration of this stratigraphically important event at 3400 ± 350 yr. More importantly, the Neumark Nord 2 data enables precise terrestrial–marine correlation for the Eemian stage in central Europe. This shows a remarkably large time lag of ca. 5000 yr between the MIS 5e ‘peak’ in the marine record and the start of the last interglacial in this region.

010506 paleontologyEemiangeographyPaleomagnetismgeography.geographical_feature_category010504 meteorology & atmospheric sciencesAardwetenschappenBlake EventMIS 5ePalaeomagnetismLast interglacialTime lagLate onsetEemianSedimentary basin01 natural sciencesSequence (geology)PaleontologyArts and Humanities (miscellaneous)InterglacialShort PaperGeneral Earth and Planetary SciencesGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary Research
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