4,647 research outputs found

    Letters of concern, condolences, and sympathy from friends and relatives upon the illness and subsequent death of Mr. Fleming on December 20, 1908.

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    Correspondents include L. McNeill. Letters with accompanying envelopes have written answered on them, 1908-12-16 - 1909-02-1

    Names of fungal species with the same epithet applied to different morphs: how to treat them

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    The abolition of the separate naming of different morphs of the same fungal species in 2011 will inevitably result in many name changes in some genera. The working practices commended here are intended to minimize one category of these changes, that which can arise as a consequence of an author using the epithet of an asexual morph when describing the sexual morph of the same species. We consider that name proposed for the sexual morph in such cases should be treated as a formal error for a new combination and not as a new species, and so be corrected. This is interpreted as applying even where the author indicated that a new species was being described and designated a type. We argue that those formalities were a result of the requirements of the rules then in force, as the author recognized that a morph of a named species was being described, and not a new hitherto unnamed species was being reported - but was barred from making a new combination so used the same epithet for the new morph name instead. Where a type with the sexual morph was designated for the sexual morph, under this interpretation that no longer has nomenclatural status, the type being that of the basionym. The material for the sexual morph indicated as a type, would be available for designation as an epitype, though a modern sequenced sample with both sexual and asexual morphs would be more informative as an epitype in many cases. A proposal to regularize the working practice commended here, and also the converse situation where the sexual morph typified name is the earlier, will be made to the 2017 Shenzhen Congress

    Alien Registration- Mcneill, Anna L. (Bath, Sagadahoc County)

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    https://digitalmaine.com/alien_docs/8906/thumbnail.jp

    The States Square Off in Arkansas v. Oklahoma - and the Winner Is ... The EPA

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    Using food intake records to estimate compliance with the Eatwell plate dietary guidelines

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    This work was supported by the Scottish Government's Rural and Environment Science and Analytical Services (RESAS) Division. The original studies, from which the current data were taken, were funded by the Food Standards Agency, UK, and the Biscuit, Cake, Chocolate and Confectionery Association, London, UK.Peer reviewedPostprin

    Reexamining evidence-based practice in community corrections: beyond 'a confined view' of what works

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    This article aims to reexamine the development and scope of evidence-based practice (EBP) in community corrections by exploring three sets of issues. Firstly, we examine the relationships between the contested purposes of community supervision and their relationships to questions of evidence. Secondly, we explore the range of forms of evidence that might inform the pursuit of one purpose of supervision—the rehabilitation of offenders—making the case for a fuller engagement with “desistance” research in supporting this process. Thirdly, we examine who can and should be involved in conversations about EBP, arguing that both ex/offenders’ and practitioners’ voices need to be respected and heard in this debate

    Early dolomitization of platform carbonates and the preservation of magnetic polarity

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    Results from a combination of techniques are presented to evaluate the nature of magnetization in shallow-water platform carbonates which have undergone recrystallization during early calcification and dolomitization. Magnetic grain separates, coercivity spectra, modified Lowrie-Fuller tests, magnetization efficiency, and magnetostratigraphic constraints indicate that the ultrafine-grained magnetite is preserved during early burial geochemical regimes, inversion from aragonite/high-magnesium calcite to low-magnesium calcite, and even pervasive dolomitization. These single-domain crystals are thought to occur as interacting multigrain clusters, some of which may exceed 1 ÎŒm in diameter. These large clusters may help prohibit magnetic reorientation during diagenesis. Furthermore, during both fabric preserving and fabric destructive dolomitization, the ultrafine-scale replacement process restricts reorientation of the clusters, thus preserving depositional or early postdeposition magnetic orientation. This early dolomitization (matrix stabilization) may even help protect and extend the subsurface lifespan of the original polarity
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