Fjords contain a significant quantity of sediments deposited in coastal zones over the last ~100,000 years. Studies of Northern Hemisphere fjords have shown that a large part of the high concentration of sedimentary organic matter (OMsed) is terrestrial in origin (OMterr), composed of a modern detrital fraction and an old mineral-associated fraction (OMfossil). These results suggest that fjords are disproportionately responsible, on a per area basis, for the burial of organic matter in coastal zones. This study, after a rigorous examination of CuO and GDGT biomarker methods used to quantify terrestrial organic matter in coastal environments, demonstrated this hypothesis in a Southern Hemisphere fjord system, Fiordland, New Zealand. CuO analysis of Doubtful Sound surface sediments indicated a large contribution of vascular plant material to fjord sediments. The BIT Index correlated strongly with both delta13C and C/N values in Doubtful Sound surface sediments, indicated that it may accurately trace the relative proportions of marine and soil organic matter (OMsoil) in Fiordland. However, a detailed analysis of the conversion of the BIT Index to quantitative estimates of terrestrial (soil) organic matter revealed that these values are overestimates. Reconstructions of the BIT Index and tetraethers in cores from two locations on the Louisiana continental shelf demonstrated the influence of the crenarchaeol term on BIT Index-based terrestrial organic matter estimates. The differences in the applicability of the BIT Index to these two coastal environments was most likely due to large seasonal changes in productivity on the Louisiana Continental Shelf as well as higher marine relative to terrestrial inputs. Six cores were reconstructed for contributions from marine OM (OMmar), OMfossil, and OMterrestrial representing the last ~500 years of sedimentation. Spatial variations were larger than temporal variations, owing to negligible development and deforestation in the region. OMterr was the dominant fraction in all but one core, and OMfossil inputs were significant. Additionally, source reconstructions from a variety of biomarkers indicated that Landslides deliver large volumes of detrital organic matter to fjord sediments. These results confirm that fjords bury quantitatively significant volumes of organic carbon on a global scale.

Cette thèse a pour but de reconstituer le climat des 100 000 dernières années en Europe de l’ouest. L’étude du climat du passé permet de mieux comprendre la variabilité naturelle du climat sur laquelle se surimpose aujourd’hui le réchauffement climatique d’origine anthropique. Ce sont des molécules fossiles bactériennes dont la structure varie en fonction des conditions environnementales qui ont permis dans cette étude de reconstituer le paléoclimat à partir des sédiments du lac St Front dans le Massif Central. Les indices dérivés de ces molécules révèlent la variabilité climatique à long terme mais également les évènements rapides de changement climatique ainsi qu’une forte action anthropique en surimposition des changements climatiques régionaux sur les 5000 dernières années. Ce travail montre l’importance de la compréhension de l’outil utilisé et du fonctionnement du système naturel dans lequel il est étudié, préalables indispensables à l’obtention d’une séquence climatique crédible / This thesis aims to reconstruct the climate of the last 100,000 years in western Europe. The study of past climate allows to better understand the natural variability of climate on which human-induced global warming is superimposed today. Bacterial fossil molecules whose structure varies according to the environmental conditions were used in this study to reconstruct the paleoclimate from the sediments of lake St Front in the Massif Central. The indices derived from these molecules reveal the long-term climatic variability but also the rapid events of climate change as well as a strong anthropogenic action in superimposition of the regional climatic changes over the last 5000 years. This work shows the importance of understanding the tool used and the functioning of the natural system in which it is studied, essential prerequisites for obtaining a credible climate reconstruction

Afin de mieux comprendre la sensibilité du continent européen aux changements climatiques, le potentiel des tétraéthers de glycérol ramifiés (ou « méthylés »), supports de nouveaux indicateurs de température et du pH des sols, a été étudié dans 2 archives sédimentaires. Ces 2 carottes de sédiments marins prélevées à l’embouchure de grands fleuves (Danube et paléo fleuve Manche) de part et d’autre de l’ancienne calotte glaciaire fennoscandinave, offrent l’opportunité d’obtenir des enregistrements contenant une information intégrée à l’échelle de vastes bassins versants depuis le dernier cycle glaciaire. Des reconstitutions continues des températures glaciaires obtenues à partir de l’analyse des tétraéthers ramifiés dans ces carottes sont présentées. Ces enregistrements sont interprétés avec précaution du fait de la relative méconnaissance des organismes producteurs des tétraéthers ramifiés et leur possible production en milieu aquatique. La haute résolution temporelle des reconstitutions permet toutefois de mieux comprendre la variabilité climatique abrupte de la dernière période glaciaire, de part l’estimation des températures associées aux évènements de Heinrich et cycles de Dansgaard-Oeschger, notamment par une estimation quantitative en Europe centrale-est. De plus, l’apport des tétraéthers à la reconstitution du pH des paléosols de cette partie du continent est étudié. Par ailleurs, une méthode automatisée de purification des échantillons, préalable à l’analyse des tétraéthers par HPLC-MS a été mise au point, afin de faciliter le travail préparatoire et promouvoir l’analyse de paléo séquences à haute résolution temporelle utilisant les tétraéthers. / In order to better understand the sensibility of the European continent to climate changes, the potential of branched tetraether lipids, as bases of temperature and soil pH proxies, has been studied in two sedimentary archives. These two marine sediment cores have been chosen for their location at the mouth of major rivers (Danube and paleo Channel river) on both sides of the ancient Fennoscandian ice sheet. Indeed, they enable to get records containing information integrated at large drainage basin scale, since the last glacial cycle. Thus, continuous temperature reconstructions of the last glacial period in Europe, based on branched tetraethers extracted from these cores, are presented. These records are carefully interpreted, notably because of the uncertainties on the tetraether producers and their likely production in the aquatic environment. The high temporal resolution of the reconstruction however enables insights into the last glacial abrupt climate variability, with temperature estimates of Heinrich events and Dansgaard-Oeschger cycles, and especially, quantitative estimations in central eastern Europe. Moreover, the reconstruction of past soil pH in this part of the continent is investigated. Last, an automated purification method for archaeal and bacterial tetraethers in soils and sediments has been developed in order to contribute to enhancing the time resolution of paleosequences based on tetraether biomarkers.

Eastern Africa has experienced strong climatic changes since the last deglaciation (15 000 years ago). The driving mechanisms and teleconnections of these spatially complex climate variations are yet not fully understood. Although previous studies on lake systems have enhanced our knowledge of Holocene precipitation variation in eastern Africa, relatively few studies have reconstructed the terrestrial temperature history of eastern Africa from lake archives. Here, we present (i) a new branched glycerol dialkyl glycerol tetraether (brGDGT) temperature calibration that includes Bale Mountains surface sediments and (ii) a quantitative record of mean annual air temperature (MAT) over the past 12 ka cal BP using brGDGTs in a sediment core collected from Garba Guracha (3950ma.s.l.) in the Bale Mountains. After adding Bale Mountains surface sediment (n = 11) data (Baxter et al., 2019) to the existing East African lake dataset, additional variation in 6-methyl brGDGTs was observed, which necessitated modifying the MBT'5ME calibration (MBT denotes methylation of branched tetraethers) by adding 6-methyl brGDGT IIIa0 (resulting in the MBT Bale Mountains index, r² = 0:93, p < 0:05). Comparing the MBT'5ME and the new MBT Bale Mountains index, our high-altitude Garba Guracha temperature record shows that warming occurred shortly after the Holocene onset when the temperature increased by more than 3.0°C in less than 600 years. The highest temperatures prevailed between 9 and 6 ka cal BP, followed by a temperature decrease until 1.4 ka cal BP. The reconstructed temperature history is linked to supraregional climatic changes associated with insolation forcing and the African Humid Period (AHP), as well as with local anomalies associated with catchment deglaciation and hydrology.