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PaleoMex Climat-Homme-Environnement • Objectives :document the Mediterranean climate (trends, variability, abrupt changes, extremes) and the water balance of the basin over the Holocene - Evaluate impacts on the surface and deep circulation, on the continental climate and their consequences on human societies. • Information of past climate using data from two differents time-scales • Historical climatology - high resolution documentary and proxy data over the past millenium • Paleoclimatology data on longer time scales (10,000 years) • Targets (LIA, MWP, RWP, 8200 ans, sapropèle 1, MHSL..) • Based on combined data model approach to provide an integrated model of the evolution of human societies in response to climate change and their impacts (sea level, land use, ecosystems and their biodiversity…) • Strongly multidisciplinary - large spectrum of expertise (OA, ST, SHS) : historians, archeologists, paleoclimatologists, paleoceanographers, statisticians, modelers,…
Letter of Intent • International workshop in spring 2009 • 1.1 1.The mechanisms of the Mediterranean climate • 1.2 2. Marine and continental hydrological cycles • 1.3 3.Extreme events, hazards and risks • 1.3 4. Coastal lines and sea-level changes • 1.5 5. A common chronology of Holocene changes • 1.5 6. Climate – environment – man interactions • 1.7 7. Impact on productivity and biodiversity of continental and marine ecosystems • Greece • 1. Hellenic Centre for Marine Research • 2. University of Athens • 3. University of the Aegean • Spain • 1. University of Madrid • Ricardo García Herrera, • 2. Universitat de Barcelona • Swizterland • 1.University of Bern • Oeschger Centre for Climate Change Research & NCCR Climate • 2. University of Geneva, • United Kingdom • 1.Southampton University • 2. School of Geography, Plymouth • 3. University of Reading • 4. University of East Anglia, Cimatic Research Unit • 5. University of Leeds • Italy • 1.Universita Politecnica delle Marche • 2. Padoue University • Turkey • Istanbul University • Marocco • Tanger University • Tunisia • Sfax university • Germany • GKSS - Inst Hydrophysics • USA 1. Laboratory of Tree-Ring Research, Tucson 2. Cornell University 3 . University of Massachusetts, 4. Yale University Egypt 1- Alexandria University 2- National Institute of Oceanography and Fisheries (NIOF)
The Historical Period in marine cores The Little Ice Age Lund et al., Nature 2006
Les proxies 1er exemple de reconstruction haute résolution en Méditerranée - 700 ans d’enregistrement avec une résol. temp. de 4 ans SSTs alcénones Profondeur: 200m 2.5 mm - 4 ans de résolution temporelle Versteegh, G^3, 2007
The historical period on continents Historical documents and geomorphological indicators provide information on Rhone and Durance floods. We see that the Little Ice Age was characterized by frequent floods
Historical periods: written documents and tree-ring analysis Le bassin méditerranéen, un secteur privilégié d’archives paléoenvironnementales - environnements contrastés - des archives très sensibles au changement climatique
The Holocene: data-model comparaison Mid-Holocene (6ka BP): reconstruction of annual temperature from pollen data (deviations from present climate) (Davis and Brewer, 2003) Deviations from present climate Mid-Holocene (6ka BP): simulation using IPSL climate model. The west-east and south-north gradients are in agreement with the data
Summer Palmer Drought Severity Index in the Mediterranean Basin Comparison of the smoothed reconstruction of summer PDSI (aridity index) with its simulation by the ECHO-G all forcing model (red). The curves are averaged on the whole Mediterranean Basin.
The Mediterranean Sea provides a unique opportunity to investigate the socio-environmental interactions at different time and spatial scales. To investigate their complexity, the plurality of human responses and solutions in mitigating social vulnerability to climate variability and thus explore new modelling approaches. Microscale studies covering a wide range of climatic forcing and level of political and social decision making.
End of the 20ème century… Beyond the Historical period Between 9000 et 7500 yrs BP
In the field, coring at sea and on land to retrieved ice cores, lacustrines cores In the labs, Screen technics like XRF, RX, magnetic parameters,…to heavier geochemical analyses Data managment and computer time and facilities,
Coring at sea Coring on land
Continental drilling and micropaleontological analyses One main tools for paleoenvironment investigations is lacustrine cores and determination of micro-organisms present in the samples
RX and XRF facilities National instrument at EPOC, Bordeaux
Geochemical analyses Molecular indicators, major and trace elements, O and C isotopes on bilcarbonates, speleothems, tree rings, tephrochronology…