Abstract: Within a single animal species, different morphs can allow for differential exploitation of foraging niches between populations, while sexual size dimorphism can provide each sex with access to different resources. Despite being potentially important agents of evolution, resource polymorphisms, and the way they operate in wild populations, remain poorly understood. In this study, we examine how trophic factors can select for different body sizes between populations and sexes in a diving endotherm. Dive depth and duration are positively related to body size in diving birds and mammals, a relationship explained by a lower mass-specific metabolic rate and greater oxygen stores in larger individuals. Based on this allometry, we predict that selection for exploiting resources situated at different depths can drive the evolution of body size in species of diving endotherms at the population and sexual level. To test this prediction, we studied the foraging ecology of Blue-eyed Shags, a group of cormorants with male-biased sexual size dimorphism from across the Southern Ocean. We found that mean body mass and relative difference in body mass between sexes varied by up to 77% and 107% between neighbouring colonies, respectively. Birds from colonies with larger individuals dived deeper than birds from colonies with smaller individuals, when accounting for sex. In parallel, males dived further offshore and deeper than females and the sexual difference in dive depth reflected the level of sexual size dimorphism at each colony. We argue that body size in this group of birds is under intense selection for diving to depths of profitable benthic prey patches and that, locally, sexual niche divergence selection can exaggerate the sexual size dimorphism of Blue-eyed Shags initially set up by sexual selection. Our findings suggest that trophic resources can select for important geographic micro-variability in body size between populations and sexes.

Abstract: With the aim to investigate the production and destruction mechanisms of formaldehyde (HCHO) on a seasonal scale in the remote troposphere, HCHO was monitored over a 13-months period at Dumont d’Urville station, located near the East Coast of the Antarctic continent. Monthly means of 50 ppt in winter and up to 200 ppt in summer were measured. In spring, summer and autumn, a daily variation was detected with amplitude of ≈40 ppt and a maximum during the afternoon. The analytical instrument (Aerolaser, AL4021) deployed for the measurements, was found to be extremely sensitive to ambient temperature variations. The origin of the temperature dependence was investigated, and the deployed analytical method was adapted to eliminate this artefact. The impact of local contamination sources at the measurement site was explored in detail. Anthropogenic combustions were found to have a limited impact (maximum 150 pptv on hourly means) versus a local emission source from ornithogenic soils, induced by the omni-presence of Adelie penguins on the site in summer (maximum 200 pptv on hourly means). From november to march, these sources can introduce an overestimation by a factor 5 of the daily HCHO amplitude, while the influence on the monthly averaged budget can account up to 100 ppt. The raw dataset was thoroughly filtered using local meteorological criteria to eliminate any potential contamination. HCHO measurements were compared to simulations made with a numerical box model developed on the base of the current understanding of the photochemical sources and sinks of HCHO. During summer, methane oxidation was found to be the major source of HCHO production, likely due to enhanced levels of oxidants such as hydroxyl radical (OH) or nitrogen oxide (NO) occurring at DDU since this coastal site is under strong continental influence. Snow emissions and HCHO formation via methyl-hydroperoxyde oxidation complete the summer budget (respectively 10 to 20% of the CH4 oxidation). In contrary to what was observed for the Weddell Sea area, halogens chemistry is probably unlikely to contribute significantly at Dumont d’Urville (<10% of the CH4 oxidation). Finally, the initially attended summer source originating from non-methane hydrocarbons oxidation was found to be inefficient and to contribute only with less than 5 % of the CH4 oxidation. During winter the snowpack source was found to be preponderant (70% of CH4 oxidation) versus the gas phase chemistry sources of HCHO. Model investigations, performed on a seasonal and daily scale have shown that gas phase processes together with deposition and snow emission have to be considered to achieve a correct reconstruction of the observations.

Abstract: With its imaged debris disk of dust, its evaporating exocomets, and an imaged giant planet, the young (~23 Myr) β Pictoris system is a unique proxy for detailed studies of planet formation processes as well as planet–disk interactions. Here, we study ten years of European Southern Observatory/High Accuracy Radial Velocity Planet Searcher (HARPS) high-resolution spectroscopic data of β Pictoris. After removing the radial velocity (RV) signals arising from the δ Scuti pulsations of the star, a ~1,200-d periodic signal remains, which, within our current knowledge, we can only attribute to a second planet in the system. The β Pic c mass is about nine times the mass of Jupiter; it orbits at ~2.7 au on an eccentric (e ~ 0.24) orbit. More RV data are needed to obtain more precise estimates of the properties of β Pic c. The current modelling of the planet’s properties and the dynamic of the whole system has to be reinvestigated in light of this detection.

Abstract: With climate change, the strong seasonality and tight pelagic-benthic coupling in the Arctic is expected to change in the next few decades. It is currently unclear how the benthos will be affected by changes of environmental conditions such as supplies of organic matter (OM) from the water column. In the last decade, Kongsfjorden (79°N), a high Arctic fjord in Svalbard influenced by several glaciers and Atlantic water inflow, has been a site of great interest owing to its high sensitivity to climate change, evidenced by a reduction in ice cover and an increase in melting freshwater. To investigate how spatial and seasonal changes in vertical fluxes can impact the benthic compartment of Kongsfjorden, we studied the organic matter characteristics (in terms of quantity and quality) and prokaryotic distribution in sediments from 3 stations along a transect extending from the glacier into the outer fjord in 4 different seasons (spring, summer, autumn and winter) in 2012–2013. The biochemical parameters used to describe the sedimentary organic matter were organic carbon (OC), total nitrogen, bulk stable isotope ratios, pigments (chorophyll-a and phaeopigments) and biopolymeric carbon (BPC), which is the sum of the main macromolecules, i.e. lipids, proteins and carbohydrates. Prokaryotic abundance and distribution were estimated by 4′,6-diamidino-2-phenylindole (DAPI) staining. This study identifies a well-marked quantitative gradient of biogenic compounds throughout all seasons and also highlights a discrepancy between the quantity and quality of sedimentary organic matter within the fjord. The sediments near the glacier were organic-poor (<0.3%OC), however the high primary productivity in the water column displayed during spring was reflected in summer sediments, and exhibited higher freshness of material at the inner station compared to the outer basin (means C-chlorophyll-a/OC ~5 and 1.5%, respectively). However, sediments at the glacier front were depleted in BPC (~0.2–0.3mgCg−1DW) by 4.5 and 9 times compared to sediments from the inner and outer stations. δ13C values in sedimentary organic matter of Kongsfjorden varied between −23.8 and −19.3‰ and reflected distinct sources of organic matter between basins. Bacterial total cell numbers in sediments of Kongsfjorden were <2×108cellsml−1 and the prokaryotic community structure was strongly influenced by the marked environmental biogenic gradients. Overall, the spatial variability prevailed over the seasonal variability in sediments of Kongsfjorden suggesting that glacier inputs prominently control the functioning of this benthic ecosystem and its communities. Regional index terms: Norway, Svalbard, Kongsfjorden.

Abstract: William Smith Meeting : Observations and Causes of Sea-Level Changes on Millennial to Decadal Timescales, 1-2 Sept. 2008, London.