Outcrops of late Quaternary deposits along the north–east coast of Mallorca were examined, and a high resolution chronological framework established using optically stimulated luminescence of quartz and feldspar grains. Coastal sections at Es Barrancar and Cala Mata record a complex succession of alluvial fan deposition with a minor aeolian component, mainly deposited during the last two glacial cycles. For the last ~200ka different orbital configurations appear to have produced a series of subtly different climatic scenarios that resulted in great variations in the regional availability of moisture. In turn, each of these climatic scenarios set in motion a distinct set of sedimentary processes, which imprinted themselves upon the character of fluvial system response recorded in the alluvial archives on Mallorca. Within the resulting complex of sediments were units of fluvially reworked aeolianite which, although truncated in places, were traceable laterally along wide sections of the sea front outcrops of both fan systems. These archives yielded 47 new OSL and pIRIR290 ages which suggest a number of previously unrecognised periods of enhanced fluvial activity. Luminescence ages identify significant ephemeral fluvial activity taking place during MIS 6, MIS 5 sub-stages d/c, b/a, and across the MIS 5/4 boundary. Another major phase of reworking corresponds with the middle part of MIS 3, and continued sporadically into the Last Glacial Maximum. These fluvial reworking events have been interpreted as having taken place during cold arid climatic intervals, when vegetation was at a minimum, precipitation was low and displayed a much higher degree of seasonality, enhancing the effects of runoff.

Ce projet de recherche porte sur l’étude de la contamination de la côte libanaise par les composés organiques (HAP, DDE) et par les éléments-trace métalliques (Hg, Pb principalement). Les travaux sur les compartiments sédimentaires et biologiques de la côte libanaise constituent deux parties aux problématiques et aux approches distinctes autour desquelles s’articule cette thèse. Dans la première partie, l’analyse d’une carotte sédimentaire datée prélevée sur le plateau continental du Sud du Liban a permis de reconstituer l’historique de contamination dans le bassin Levantin. Les analyses de contaminants dans les sédiments de la carotte C1 combinés à la datation aux 210Pb et 137Cs ont permis d’obtenir un enregistrement fiable des variations du dépôt de mercure, de plomb et de HAP sur le plateau continental libanais, dans le bassin Levantin. Bien que les concentrations et les flux soient relativement faibles, une augmentation en deux phases des concentrations est bien mise en évidence par le profil sédimentaire de C1. Le charbon est identifié comme source principale de Pb, de Hg et de HAP dans le bassin Levantin entre la moitié du 19ème siècle et la moitié du 20ème siècle. Les résultats des ratios isotopiques du Pb et des ratios diagnostiques de HAP appuient ce constat. Les archives sédimentaires dans la carotte C1 fournissent un signal du dépôt de contaminants à l’échelle globale probablement lié aux sources d’émissions atmosphériques en provenance d’Europe Centrale et de l’Est. Dans la seconde partie, une étude de la contamination par les HAP du littoral libanais est menée suite à la marée noire résultant du conflit armé israélo-libanais en 2006. Une approche de biomonitoring sur trois ans utilisant l’espèce de moules invasives Brachidontes variabilis a été développée. Les résultats indiquent une décroissance progressive des concentrations de HAP dans l’écosystème intertidal du littoral libanais. La contamination par les HAP du fioul en zone subtidale en 2007 est nettement plus faible. Cependant la signature des HAP dans les tissus de moules prélevées trois ans après la marée noire indique toujours la présence des composés du fioul de Jiyeh. La contamination est particulièrement persistante dans certaines zones fortement touchées par la nappe de fioul en 2006. Il apparaît que l’état initial pré-marée noire n’a pas été atteint, même trois ans après la marée noire de Jiyeh. L’examen détaillé de l’évolution spatiale et temporelle de la contamination par les HAP de l’environnement intertidal est présenté dans ce volet de notre étude. / This research project aims at the study of the contamination of the Lebanese coast by PAHs, DDE, Hg and Pb. The research work is divided into two distinct parts concerning two environmental compartments (sedimentary and biological) and it addresses different questions and approaches. In the first part, the study of a dated sediment core raised from the continental shelf in southern Lebanese coast allowed reconstructing the contamination history in the Levantine basin. The contaminants’ analysis as well as 210Pb and 137Cs datation allowed obtaining a reliable record of mercury, lead and PAHs sedimentary deposition in the Lebanese continental margin in the Levantine basin. Although concentrations and fluxes are relatively low, a two-phase increase of concentration is found using C1 core sedimentary profiles. Coal was identified as the main source of Pb, Hg and PAHs in the Levantine basin between the mid 19th and the mid 20th century. Ratios of Pb stable isotopes and PAH diagnostic ratios support this assumption. The studied sedimentary archives provide also information on the deposition of contaminants on a global scale possibly related to atmospheric emissions mainly from Central and Eastern Europe. In the second part of the thesis, the study of contamination by PAHs of the Lebanese coast was undertaken following an oil spill in the south of Lebanon, which occurred after the bombardment by the Israeli military of the electric power plant in Jiyeh in 2006. We have set-up a biomonitoring program with an invasive mussel specie Brachidontes variabilis over a three-year study. Results indicate a progressive decrease of PAH concentrations in the intertidal ecosystem of the Lebanese coast. Contamination of the subtidal zone in 2007 by Jiyeh fuel oil was significantly lower. However, Jiyeh fuel oil signature was still detectable in mussel tissues even three years after the oil spill. Contamination was found to be particularly persistent in some of the highly oiled sites. It appears that pre-spill state was still not reached even three years following the oil spill. Detailed investigation of spatio-temporal changes of intertidal mussels contamination by PAH is also presented in this part of the thesis.