30 research outputs found

    Rare and low-frequency coding variants alter human adult height

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    Height is a highly heritable, classic polygenic trait with ~700 common associated variants identified so far through genome - wide association studies . Here , we report 83 height - associated coding variants with lower minor allele frequenc ies ( range of 0.1 - 4.8% ) and effects of up to 2 16 cm /allele ( e.g. in IHH , STC2 , AR and CRISPLD2 ) , >10 times the average effect of common variants . In functional follow - up studies, rare height - increasing alleles of STC2 (+1 - 2 cm/allele) compromise d proteolytic inhibition of PAPP - A and increased cleavage of IGFBP - 4 in vitro , resulting in higher bioavailability of insulin - like growth factors . The se 83 height - associated variants overlap genes mutated in monogenic growth disorders and highlight new biological candidates ( e.g. ADAMTS3, IL11RA, NOX4 ) and pathways ( e.g . proteoglycan/ glycosaminoglycan synthesis ) involved in growth . Our results demonstrate that sufficiently large sample sizes can uncover rare and low - frequency variants of moderate to large effect associated with polygenic human phenotypes , and that these variants implicate relevant genes and pathways

    Construction progress of WEAVE: the next generation wide-field spectroscopy facility for the William Herschel Telescope

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    We present an update on the overall construction progress of the WEAVE next-generation spectroscopy facility for the William Herschel Telescope (WHT), now that all the major fabrication contracts are in place. We also present a summary of the current planning behind the 5-year initial phase of survey operations, and some detailed end-to-end science simulations that have been effected to evaluate the final on-sky performance after data processing. WEAVE will provide optical ground-based follow up of ground-based (LOFAR) and space-based (Gaia) surveys. WEAVE is a multi-object and multi-IFU facility utilizing a new 2-degree prime focus field of view at the WHT, with a buffered pick-and-place positioner system hosting 1000 multi-object (MOS) fibres, 20 integral field units, or a single large IFU for each observation. The fibres are fed to a single (dual-beam) spectrograph, with total of 16k spectral pixels, located within the WHT GHRIL enclosure on the telescope Nasmyth platform, supporting observations at R 5000 over the full 370-1000nm wavelength range in a single exposure, or a high resolution mode with limited coverage in each arm at R 20000. The project has experienced some delays in procurement and now has first light expected for the middle of 2019

    Toward a dynamic representation of hydrological connectivity at the hillslope scale in semiarid areas.

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    [1] Hydrological connectivity has emerged as an effective means to understand and manage fluxes of water and transport of nutrients and sediment at the catchment scale, especially as fluxes are modified by changing climate and land use. However, hydrology has not yet adopted it as a unifying concept given uncertainties regarding different conceptions and gaps in understanding of how connectivity functions at different temporal and spatial scales. This paper outlines a conceptual model of hydrological connectivity for semiarid hillslopes and highlights the direction that future attempts to quantify dynamic hydrological connectivity might take. Rainfall-runoff analysis emphasizes the influence of antecedent moisture and temporal storm structure on hillslope-scale flood generation. Plot-scale field flume experiments demonstrate the spatial and temporal variability of flow resistance. The morphological runoff zone framework is presented as a method to upscale such results to the hillslope and incorporate the broader-scale issue of hillslope form. The need to design field experiments to inform attempts to model feedbacks between runoff depth and flow resistance forms the central argument of this paper. Patterns of infiltration and resistance across entire flow paths and their variability throughout a storm event are the key to understanding dynamic hydrological connectivity at the hillslope scale
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