1 - (A) Overview of cave openings in Mesozoic dolomite-limestone.1, 2, 3: Santuario della Madonna Cave openings; 4: Cardini or Fumarolo CaveFig.1 - (B) Holocene stratigraphic succession excavated in the Grotta della Madonna Cave (see text for details).Table 1. J.-C.: conséquences sédimentologiques et géoarchéologiques le long de la presqu’île sorrentineSpécificité des milieux continentaux et volcaniquesThe role of human impacts and Holocene climate change in the Santuario della Madonna Cave (Calabria)Di Donato V., Esposito P., Russo Ermolli E., Cheddadi R., ScaranoEllwood B.B., Petruso K.M., Harrold F.B., SchuldenreinGonzález-Pérez J.A., González-Vila F.J., Almendros G., KnickerSauro U., Borsato A., Frisia S., Madonna G., Piccini L., Tuccimei P., Camuffo D., Cucchi F., Forti P., Macaluso T., Miorandi R., Paladini M., Salzano R., Shopov Y., Spötl C., Stoykova D., Zini LEvidence of climate change and its effects in the MediterraneanSegregation in the cities of the European MediterraneanGeomorphology and geoarchaeology of Black Sea coastsMediterranean coastal wetlands: dynamics and management issuesChanging spaces of economic activities in the Mediterranean basinThe quality of the environment in urban zones: a multidisciplinary assessmentAgrarian aeras: landscape dynamics, ground laws, parties involved and planningMediterranean rivers and their margins: processes and mangementNorth Africa and Globalization - Subalternity, territorial fragmentationMediterranean Coastline: withdraw towns back from the coastline; protect ourselves from the sea?Migrations and territories of mobility in the MediterraneanPort cities, Projections 2020: rising the stakes of developmentBulgaria-Romania: the new Balkan boundaries of the European UnionTerroirs : characterization, territorial developement and governanceNew dynamics of rural development in the Southern AlpsEnterprises in Méditerranean: inheritances, models, redeploymentsThe great natural site in the metropolitan regions of MediterraneanPublished in Ce site karstique correspond à un affleurement de calcaire dolomitique tertiaire remodelé par la mer au Quaternaire. We use cookies to help provide and enhance our service and tailor content and ads. La variation des températures moyennes semble avoir diminué rapidement avec la latitude, ce qui fait qu'il n'y eu que peu de changement… ScienceDirect ® is a registered trademark of Elsevier B.V.Enregistrements marins des variations climatiques de l'HolocèneCopyright © 2004 Académie des sciences. Celles-ci peuvent être interprétées comme une réponse linéaire aux changements de l'insolation moyenne annuelle. and potential CO2 forcingHolocene variability of the East Asian summer monsoon from Chinese cave records: A re-assessmentChinese stalagmite δ18O controlled by changes in the Indian monsoon during a simulated Heinrich eventHigh-precision and high-resolution carbonate 230th dating by MC-ICP-MS with SEM protocolsPaleo-climatic changes in the Qinghai Lake area during the last 18,000 yearsClimates and environments of the Holocene Mega thermal Maximum in ChinaA Chinese cave links climate change, social impacts, and human adaptation over the last 500 yearsSummer monsoon precipitation variations in central China over the past 750 years derived from a high-resolution absolute-dated stalagmiteCirculation effect: Climatic significance of the short term variability of the oxygen isotopes in stalagmites from monsoonal ChinaSiberian caves recorded the history of permafrost occurrence during the past 450,000 yearsPalaeosol development in the Chinese Loess Plateau as an indicator of the strength of the East Asian summer monsoon: Evidence for a mid-Holocene maximumNortheastern Brazil wet periods linked to distant climate anomalies and rainforest boundary changesThe Holocene Asian monsoon: Links to solar changes and North Atlantic climateMillennial- and orbital- scale changes in the East Asian Monsoon over the past 224,000 yearsChanges in East Asian summer monsoon during the Holocene recorded by stalagmite δ18O records from Liaoning ProvinceHydrology of Dali Lake in central-eastern Inner Mongolia and Holocene East Asian monsoon variabilityConcordant monsoon-driven postglacial hydrological changes in peat and stalagmite records and their impacts on prehistoric cultures in central ChinaHolocene stalagmite δ18O records in the East Asian monsoon region and their correlation with those in the Indian monsoon regionEast Asian Summer Monsoon variations in the past 12.5 ka: High-resolution δ18O record from a precisely dated aragonite stalagmite in central ChinaTiming and duration of the East Asian summer monsoon maximum during the Holocene based on stalagmite data from North ChinaA test of climate, sun, and culture relationships from an 1810-year Chinese cave recordHigh-resolution evidence from southern China of an early Holocene Optimum and a mid-Holocene dry event during the past 18,000 years


Les résultats fournis par les assemblages de Chironomidae sont par ailleurs en accord avec l'âge de l'optimum climatique holocène compris entre 6000 et 7000 cal. The e-mail addresses that you supply to use this service will not be used for any other purpose without your consent.Create a link to share a read only version of this article with your colleagues and friends. Archaeological findings in the sedimentary infilling attest to human settlement since prehistoric times. Members of _ can log in with their society credentials belowXunlin Yang, Hong Yang, Baoyan Wang, Li-Jung Huang, Chuan-Chou Shen, R Lawrence Edwards, and Hai ChengXunlin Yang, Hong Yang, Baoyan Wang, Li-Jung Huang, Chuan-Chou Shen, R Lawrence Edwards, and Hai ChengMembers of _ can log in with their society credentials below
en The last 5000 years.

This site uses cookies. The site is a karst cave formed in Tertiary dolomite-limestone, reshaped by the sea during the Quaternary. Entre 2650 et 2000 avant aujourd'hui, les langues glaciaires s'arrêtaient à une altitude supérieure d'au moins trois cents mètres : cela correspond à l’optimum climatique romain. Rinvenimenti archeologici nei depositi di riempimento della grotta ne attestano la frequentazione antropica sin dall’epoca preistorica.


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