Search results for "holocene"

showing 10 items of 330 documents

How complex is the evolution of small mammal communities during the Late Glacial in southwest France?

2016

11 pages; International audience; The Late Glacial was a slow gradual warming associated with short, cold events that occurred between 18.0 and 11.7 ka cal. BP. Pollen analyses from deep-sea and lacustrine cores have well documented the evolution of floral communities in western Europe and suggest that climatic fluctuations influenced the evolution of terrestrial ecosystems. However, the exact impact of these climate changes on small faunal communities in southwest France is still poorly documented. Peyrazet Cave is an archaeological site located in the Lot (France) that has been excavated since 2008 and has yielded a Late Glacial sequence dated between 15.5 and 11.1 ka cal. BP. Thousands o…

Colonization0106 biological sciences010506 paleontologyBiogeographyClimate changeSicista betulinaRefugiaPeyrazet010603 evolutionary biology01 natural sciencesEuropean hamsterCaveGlacial periodCricetus cricetusHolocene[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesEarth-Surface Processesgeography.geographical_feature_categorybiologyEcologyLast Glacial Maximum15. Life on landbiology.organism_classificationGeographyBiogeography13. Climate actionNorthern birch mouse[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyQuaternary International
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Ecological implications of Cousinia Cass. (Asteraceae) persistence through the last two glacial–interglacial cycles in the continental Middle East fo…

2012

10p. gráficas

CousiniabiologyEcologyRange (biology)topographical heterogeneityinterglacial refugiaAllopatric speciationPaleontologybiology.organism_classificationQuaternary glaciationstectonic historySW AsiaInterglacialGlacial periodEndemismQuaternaryAllopatric speciationEcology Evolution Behavior and SystematicsHoloceneGeologyReview of Palaeobotany and Palynology
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Reventilation Episodes During the Sapropel S1 Deposition in the Eastern Mediterranean Based on Holococcolith Preservation

2019

Organic-rich layers (sapropels), preserved in eastern Mediterranean marine sediment records, represent pronounced perturbations to thermohaline circulation and environmental conditions in the basin, in response to enhanced African monsoon activity and subsequent massive freshwater discharge. During the most recent event, Sapropel S1 formed between 10.8 and 6.1 ka, when freshwater-driven stratification caused seafloor anoxia below ~1,800-m depth, as a result of both failure of deep water formation and enhanced productivity. Here we analyze coccolith assemblages from the open eastern Mediterranean that form a west-east transect across the basin and provide insights on past environmental chang…

DCMAtmospheric ScienceHolocenepreservationPaleontologySapropelOceanographyEastern mediterraneanOceanographyFlorisphaera profundaChristian ministryDeposition (chemistry)GeologyHolocenecoccolithPaleoceanography and Paleoclimatology
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Vulnerability of the North Water ecosystem to climate change

2021

High Arctic ecosystems and Indigenous livelihoods are tightly linked and exposed to climate change, yet assessing their sensitivity requires a long-term perspective. Here, we assess the vulnerability of the North Water polynya, a unique seaice ecosystem that sustains the world’s northernmost Inuit communities and several keystone Arctic species. We reconstruct mid-to-late Holocene changes in sea ice, marine primary production, and little auk colony dynamics through multi-proxy analysis of marine and lake sediment cores. Our results suggest a productive ecosystem by 4400–4200 cal yrs b2k coincident with the arrival of the first humans in Greenland. Climate forcing during the late Holocene, l…

DYNAMICS010504 meteorology & atmospheric sciencesEcosystem ecologyGeneral Physics and AstronomyPalaeoclimate01 natural sciencespalaeoceanographyPalaeoceanographyTEMPERATURESilmastoHOLOCENEHolocene[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere0303 health sciencesarktinen alueMultidisciplinaryEcologyAquatic ecosystemQClimate-change ecologyecosystem ecologyRECORDGREENLANDVARIABILITY[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologylämpeneminenSEA-ICEEcosystem ecologyATLANTIC OSCILLATIONSEDIMENTSclimate-change ecologyScienceGrönlantiClimate changeinuititpalaeoclimateGeneral Biochemistry Genetics and Molecular BiologyArticle03 medical and health sciencesddc:570EcosystemRECONSTRUCTION14. Life underwaterKeystone species1172 Environmental sciences[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography030304 developmental biology0105 earth and related environmental sciencesGlobal warmingGeneral Chemistry15. Life on landilmastonmuutoksetekosysteemit (ekologia)Arctic13. Climate actionmerijääpaleoklimatologiaNature Communications
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Integrating fire-scar, charcoal and fungal spore data to study fire events in the boreal forest of northern Europe

2019

Fire is a major disturbance agent in the boreal forest, influencing many current and future ecosystem conditions and services. Surprisingly few studies have attempted to improve the accuracy of fire-event reconstructions even though the estimates of the occurrence of past fires may be biased, influencing the reliability of the models employing those data (e.g. C stock, cycle). This study aimed to demonstrate how three types of fire proxies – fire scars from tree rings, sedimentary charcoal and, for the first time in this context, fungal spores of Neurospora – can be integrated to achieve a better understanding of past fire dynamics. By studying charcoal and Neurospora from sediment cores f…

DYNAMICS010506 paleontologyArcheologyPeat010504 meteorology & atmospheric sciencesPEATLONG-TERM HISTORYnon-pollen palynomorphs01 natural sciencesRussiaTREE-RING RECORDSBOGHOLOCENEEcosystemFire ecologyCharcoalBogFinland1172 Environmental sciences0105 earth and related environmental sciencesEarth-Surface ProcessesGlobal and Planetary Changegeography4112 Forestrygeography.geographical_feature_categoryEcologyTaigaPaleontologyForestry15. Life on landPICEA-ABIESTAIGA FORESTNeurosporatree ringsDisturbance (ecology)13. Climate actionvisual_artforest hollowvisual_art.visual_art_mediumEnvironmental scienceWoody plant
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Towards understanding the abundance of non-pollen palynomorphs : A comparison of fossil algae, algal pigments and sedaDNA from temperate lake sedimen…

2018

Given the increased interest in non-pollen palynomorphs (microscopic objects other than pollen identified from pollen slides) in palaeoecological studies, it is necessary to seek a deeper understanding of the reliability of these results. We combined quantitative information of algal pigments and sedimentary ancient DNA (sedaDNA) of phylotaxonomical resolution to validate the richness and abundance of fossil algae in the sediment of a small temperate lake. For the first time, fossil and sedaDNA algae data were combined in a composite data-set and used to reconstruct algae turnover rates over the last 14,500 years. This comparison serves as both an example of howfossil algae can be used to a…

DYNAMICS1171 Geosciences010506 paleontologycommunity richness010504 meteorology & atmospheric sciencesCLIMATE CHANGESBiologymedicine.disease_causePediastrum114 Physical sciences01 natural sciencesBPEASTERN LATVIAAlgaeAbundance (ecology)PollenHOLOCENEmedicinenon-pollen palynomorphRECONSTRUCTIONsedaDNARECORDSEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesPOLANDEcologypalaeopigmentPaleontologySedimentbiology.organism_classificationPHYTOPLANKTON RESPONSEPEDIASTRUMAncient DNAarticlesSpecies richness
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Surface–bottom relationships in the Gulf of Salerno (Tyrrhenian Sea) over the last 34 kyr: Compositional data analysis of palaeontological proxies an…

2009

The palaeontological, geochemical and mineralogical records of core GNS84-C106 were analysed in order to reconstruct palaeohydrological changes and palaeoproductivity patterns in the Gulf of Salerno for the last 34 kyr. This approach, including compositional analysis of planktonic and benthic assemblages, gave an insight into the relationships between continental, sea surface and bottom environmental changes. The main source of variability of planktonic and benthic assemblages is related respectively to sea surface temperature and palaeobathymetry. Interrelated changes in surface salinity, nutrients, density gradient in the water column and organic fluxes at the bottom act as a secondary fa…

Deep chlorophyll maximumbiologyfungiAnalisi dei dati composizionaliPaleontologybiology.organism_classificationgeochimicaForaminiferaBottom waterpaleoproduttivitàPaleontologyOceanographyWater columnMediterranean seaSpace and Planetary ScienceBenthic zoneGlacial periodgeographic locationsGeologyHoloceneGeobios
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Short communication: Driftwood provides reliable chronological markers in Arctic coastal deposits

2021

Originating from the boreal forest and often transported over large distances, driftwood characterizes many Arctic coastlines. Here we present a combined assessment of radiocarbon (14C) and dendrochronological (ring width) age estimates of driftwood samples to constrain the progradation of two Holocene beach-ridge systems near the Lena Delta in the Siberian Arctic (Laptev Sea). Our data show that the 14C ages obtained on syndepositional driftwood from beach deposits yield surprisingly coherent chronologies for the coastal evolution of the field sites. The dendrochronological analysis of wood from modern drift lines revealed the origin and recent delivery of the wood from the Lena River catc…

Delta010506 paleontology010504 meteorology & atmospheric scienceslcsh:QE1-996.5TaigaDriftwood01 natural scienceslaw.inventionlcsh:Geologylcsh:StratigraphyArctic13. Climate actionlaw14. Life underwaterPhysical geographyRadiocarbon datingProgradationRiver catchmentHoloceneGeologylcsh:QE640-6990105 earth and related environmental sciencesGeochronology
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On the generation and degradation of emerged coral reef terrace sequences: First cosmogenic 36Cl analysis at Cape Laundi, Sumba Island (Indonesia)

2021

(IF 4.45: Q1); International audience; The emerged coral reef terrace sequence at Cape Laundi, on the north coast of Sumba Island (Indonesia), with at least 18 successive strandlines, remains poorly dated in spite of numerous previous data. The age discrepancies within these coral reef terraces (CRTs) were previously explained by their polycyclic nature, triggered by marine erosion and reoccupation of old coral colonies by new ones. This study aims at highlighting these processes, as well as the continental denudation that participates in the partial stripping of the thin superficial coral reef layer overlying the pre-existing surface, exhuming older coral colonies. For this purpose, we use…

Denudation rateArcheology010504 meteorology & atmospheric sciencesCoralU–Th series[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysicsCoastal erosion01 natural sciencesQuaternaryPaleontology36Cl cosmogenic isotopeDeglaciation14. Life underwater[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/GeomorphologyEcology Evolution Behavior and SystematicsHoloceneComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryU-Th seriesCoral reef terraceCl-36 cosmogenic isotopeGeologyCoral reefSoutheastern asiaMIS 5Coastal erosionTerrace (geology)Denudation[SDU]Sciences of the Universe [physics]InterglacialGeologySoutheastern Asia
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The natural hydrous sodium silicates from the northern bank of Lake Chad : occurrence, petrology and genesis

2005

Abstract Hydrous sodium silicates sometimes associated with zeolites, form in an alkaline environment, in which there is a high concentration of dissolved silica. Such an environment existed during the Holocene in N'Guigmi interdunal depressions (Lake Chad), which led to the precipitation of various types of hydrous sodium silicates, including magadiite, kenyaite, and zeolites. Scanning electron and optical microscope observations allow several microstructures to be distinguished. These microstructures result from either precipitation sequences or a transformation along a diagenetic gradient. New petrological, microstructural and geochemical data confirm the transformation of magadiite into…

Dissolved silicaStratigraphySodiumGeochemistrychemistry.chemical_elementMineralogyGeologyDebrisDiagenesischemistrySilicate mineralsSedimentary rockPrecipitationHoloceneGeology
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