Pertinence et calibration d'un nouveau marqueur paléohydrologique : le rapport isotopique de l'hydrogène mesuré sur la miliacine

This work aims at developing a new proxy of past hydrological conditions based on the hydrogen isotopic composition (δD) of a sedimentary biomarker that is specific for broomcorn millet (Panicum miliaceum), miliacin. Analysing the spatio-temporal relevancy of this proxy reveals that miliacin δD values of plants cultivated in the field, although dispersed, follow a Gaussian law. Soil miliacin δD values are the same as those found for plants grown the year before. Interannual variations in plant miliacin δD values roughly parallel those of precipitation δD values, slight differences being attributed to differences in relative humidity. The comparison of miliacin δD values in sediments deposited in two distinct settings at the same time in Lake le Bourget attests that this proxy homogeneously integrates climatic conditions over the whole catchment. Cultivation of millet plants in climatic chambers allowed demonstrating that, although source water δD is the principal controlling miliacin δD values, this later is closely correlated to leaf water δD. Slight differences in net biosynthetic fractionation between n-alcanes and miliacin under two relative humidity levels imply that the combined analysis of sedimentary biomarkers produced through distinct biosynthetic pathways could help discriminating between source water δD and relative humidity in paleoenvironmental studies.Ce travail a pour objectif de développer un nouvel indicateur quantitatif des conditions hydrologiques passées fondé sur la composition isotopique en hydrogène (δD) d’un biomarqueur sédimentaire spécifique du millet commun (Panicum miliaceum), la miliacine. L’étude de la pertinence spatio-temporelle de cet indicateur révèle que le δD miliacine de plants de millet dans un champ, bien que dispersé, suit une loi gaussienne. Le δD miliacine du sol correspond au δD miliacine des plantes cultivées l’année précédente. L’évolution interannuelle du δD miliacine est globallement parallèle à celle du δD des eaux météoriques, les différences pouvant être attribuées à des différences d’humidité. La comparaison des valeurs de δD miliacine dans des sédiments du même âge prélevés sur deux archives distinctes dans le Lac du Bourget témoigne que l’archivage de cet indicateur est intègre de manière homogène les conditions climatiques ayant régné dans le bassin versant. La culture de millet en chambre climatique démontre que, si le δD de l’eau de source est le principal facteur controlant le δD miliacine, ce dernier est très étroitement corrélé au δD de l’eau de la feuille. De légères différences de fractionnement biosynthétique net entre n-alcanes et miliacine sous deux conditions d’humidité laissent supposer que l’analyse combinée de biomarqueurs sédimentaires issus de voies synthétiques distinctes permettrait d’accéder à la fois aux variables paléoenvironnementales clé que sont le δD de l’eau de source et l’humidité

Combined δ13C - δD analysis of pentacyclic triterpenes and their derivatives

International audienceCompound-specific carbon and hydrogen analyses have been proposed to quantify environmental variables because they afford a remarkable constrain on the biological source through the selection of specific biomarkers

How to create analogue black hole or white fountain horizons and LASER cavities in experimental free surface hydrodynamics?

Transcritical flows in free surface hydrodynamics emulate black hole horizons and their timereversed versions known as white fountains. Both analogue horizons have been shown to emit Hawking radiation, the amplification of waves via scattering at the horizon. Here we report on an experimental validation of the hydrodynamic laws that govern transcritical flows, for the first time in a free surface water channel using an analogue space-time geometry controlled by a bottom obstacle. A prospective study, both experimental and numerical, with a second obstacle downstream of a first one is presented to test in the near-future the analogous black hole laser instability, namely the super-amplification of Hawking radiation by successive bounces on a pair of black and white horizons within cavities which allow the presence of negative energy modes necessary for the amplification process. Candidate hydrodynamic regimes are discussed thanks to a phase diagram based on the scaled relative heights of both obstacles and the ratio of flow to wave speed in the upstream region.Comment: 19 pages, 19 figure

Distribution of miliacin (olean-18-en-3β-ol methyl ether) and related compounds in broomcorn millet (Panicum miliaceum) and other reputed sources: Implications for the use of sedimentary miliacin as a tracer of millet

International audienceUsing sedimentary miliacin (olean-18-en-3β-ol methyl ether) as a molecular tracer of the history of Panicum miliaceum (broomcorn millet) cultivation depends upon broomcorn millet being sedimentary miliacin's dominant source. It also requires knowledge of the variability in miliacin concentration in broomcorn millet. Finally, it is affected by the presence of other pentacyclic triterpene methyl ethers (PTMEs) that may exist in conjunction with miliacin in other sources but not in broomcorn millet. Miliacin biosynthesis has been proposed for other Panicum species, Setaria italica (Italian or foxtail millet), Pennisetum sp., and Chaetomium olivaceum (an olive green mold). We found miliacin concentration in seeds of different varieties of P. miliaceum to be similarly high (with trace amounts of β- and α-amyrin methyl ethers). It was absent from hulls and roots, and nominally present in leaves and stems. The transfer of miliacin from plant to sediments is therefore mostly from seeds. it was abundant (often with larger amounts of β- and α-amyrin methyl ethers) in all other Panicum species studied, but only in some species of the genus Pennisetum and was absent from Setaria italica. Neither C. olivaceum nor its growth medium (rice) showed any trace of miliacin. Our results, with miliacin absent from S. italica and C. olivaceum, its high miliacin in seed of P. miliaceum relative to other PTMEs and to other grasses and, considering the high biomass that cultivated broomcorn millet has relative to other potential plant sources, support the use of sedimentary records of miliacin in some contexts to track past millet agricultural dynamics

Spatial variability of compound-specific δD at the field scale: A case study from miliacin in broomcorn millet (Panicum miliaceum).

International audienceThe hydrogen isotopic composition (δD) of individual compounds preserved in lake sediments has been proposed as a proxy of the hydrological conditions that prevailed at time of their synthesis. Numerous parameters are susceptible of influencing this parameter, the first of them being the δD of environmental waters. Then, the combination of environmental (aridity, soil properties...) and biological parameters alter the δD of leaf water that is finally used for the biosynthesis of organic molecules that fractionate hydrogen isotopes through enzymatic reactions. Lake sediments accumulate organic matter produced at catchment scale, thus produced by various organisms developed on soils of potentially different properties. The spatial variability of δD in plants at a catchment scale is rarely taken into account (Hou et al., 2007), although it might represent a serious source of uncertainty on the paleoclimatic interpretation of sedimentary lipids δD

Holocene land-use evolution and associated soil erosion in the French Prealps inferred from Lake Paladru sediments and archaeological evidences

International audienceA source-to-sink multi-proxy approach has been performed within Lake Paladru (492 m a.s.l., French Prealps) catchment and a six-meter long sediment sequence retrieved from the central lacustrine basin. The combination of minerogenic signal, specific organic markers of autochthonous and allochthonous supply and archaeological data allows the reconstruction of a continuous record of past human disturbances. Over the last 10000 years, the lacustrine sedimentation was dominated by autochthonous carbonates and the watershed was mostly forest-covered. However, seven phases of higher accumulation rate, soil erosion, algal productivity and landscape disturbances have been identified and dated from 8400-7900, 6000-4800, 4500-3200, 2700-2050 cal BP as well as AD 350-850, AD 1250-1850 and after AD 1970. Before 5200 cal BP, soil erosion is interpreted as resulting from climatic deterioration phases toward cooler and wetter conditions. During the Mid-Late Holocene period, erosion fluxes and landscape disturbances are always associated with prehistorical and historical human activities and amplified by climatic oscillations. Such changes in human land-used led to increasing minerogenic supply and nutrients loading that affected lacustrine trophic levels, especially during the last 1600 years. In addition, organic and molecular markers document previously unknown human settlements around Lake Paladru during the Bronze and the Iron Ages

Can we estimate catchment-scale biomass production from sedimentary biomarkers? An attempt with miliacin in Late Bronze Age levels from Lake le Bourget (French Alps).

International audienceThe evaluation of demography for proto- and prehistoric times remains complex due to the rareness of human remains. Here we propose an original approach based on the combination of geophysical and organic geochemical techniques applied to the Late Bronze Age sedimentary infill of Lake le Bourget. Deep sediments were mapped and their volume estimated by sub-bottom seismic profiling calibrated (accoustically and chronologically) on piston cores. Multibeam bathymetry combined to a subaquatic archaeological survey allowed to precisely identify the extension of Late Bronze Age palafittic stations in shallow waters and to determine the volume of the associated organic rich deposits

Relating Habitat and Climatic Niches in Birds

Predicting species' responses to the combined effects of habitat and climate changes has become a major challenge in ecology and conservation biology. However, the effects of climatic and habitat gradients on species distributions have generally been considered separately. Here, we explore the relationships between the habitat and thermal dimensions of the ecological niche in European common birds. Using data from the French Breeding Bird Survey, a large-scale bird monitoring program, we correlated the habitat and thermal positions and breadths of 74 bird species, controlling for life history traits and phylogeny. We found that cold climate species tend to have niche positions in closed habitats, as expected by the conjunction of the biogeographic history of birds' habitats, and their current continent-scale gradients. We also report a positive correlation between thermal and habitat niche breadths, a pattern consistent with macroecological predictions concerning the processes shaping species' distributions. Our results suggest that the relationships between the climatic and habitat components of the niche have to be taken into account to understand and predict changes in species' distributions

Combining literature-based and data-driven fuzzy models to predict brown trout (salmo trutta l.) spawning habitat degradation induced by climate change

[EN] A fuzzy rule-based system combining empirical data on hydraulic preferences and literature information on temperature requirements was used to foresee the brown trout (Salmo trutta L.) spawning habitat degradation induced by climate change. The climatic scenarios for the Cabriel River (Eastern Iberian Peninsula) corresponded to two Representative Concentration Pathways (4.5 and 8.5) for the short (2011¿2040) and mid (2041¿2070) term horizons. The hydraulic and hydrologic modelling were undertaken with process-based numerical models (i.e., River2D© and HBV-light) while the water temperature was modelled by assembling the predictions of three machine learning techniques (M5, Multi-Adaptive Regression Splines and Support Vector Regression). The predicted rise in the water temperature will not be compensated by the more benign lower flows. Consequently, the suitable spawning habitat will be reduced between 15.4¿48.7%. The entire population shall suffer the effects of climate change and will probably be extirpated from the downstream segments of the river.The study has been partially funded by the IMPADAPT project (CGL2013-48424-C2-1-R) with Spanish MINECO (Ministerio de Economía y Competitividad) and FEDER funds and by the Confederación Hidrográfica del Júcar (Spanish Ministry of Agriculture, Food and Environment). The authors thank AEMET and UC for the data provided for this work (dataset Spain02). Finally, we are grateful to the colleagues who worked in the field and in preliminary data analyses; especially Marcello Minervini (funded by the EU programme of Erasmus Traineeships, at the Dept. of Hydraulic Engineering and Environment, Universitat Politècnica de València).Muñoz Mas, R.; Marcos-García, P.; Lopez-Nicolas, A.; Martínez-García, F.; Pulido-Velazquez, M.; Martinez-Capel, F. (2018). Combining literature-based and data-driven fuzzy models to predict brown trout (salmo trutta l.) spawning habitat degradation induced by climate change. Ecological Modelling. 386:98-114. https://doi.org/10.1016/j.ecolmodel.2018.08.012S9811438