22 research outputs found

    An experimental study on the response of blanket bog vegetation and water tables to ditch blocking

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    We studied the effect of ditch blocking on vegetation composition and water-table depths in a blanket peatland. Measurements were made for a period of four years (water tables) and five years (vegetation) in the inter-ditch areas of three experimental treatments: (i) open ditches, (ii) ditches blocked with closely-spaced dams and (iii) ditches partially infilled with peat and blocked with dams. It is often assumed that ditch blocking will lead to an increase in the abundance of Sphagnum and, potentially, a reduction in the abundance of sedges, particularly the cotton grasses. However, our data show no treatment effects on the abundance of either group. We did find an effect of time, with the abundance of both sedges and Sphagnum spp. varying significantly between some years. For the sedges there was no systematic change over time, while for the Sphagnum spp. abundance tended to increase through the study period. This systematic change was not related to a measure of the vigour of the sedges, although vigour was lower towards the end of the study compared to the beginning. Our vegetation data are consistent with our water-table data. As with plant type abundance, we did not find any statistically significant differences in water-table depths between treatments, both for annual averages and summer averages. We comment on why ditch blocking does not seem to have affected water tables and vegetation composition at our study site

    Spherulites and Aspiring Elites: The Identification, Distribution, and Consumption of Giali Obsidian (Dodecanese, Greece)

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    International audienceThis paper details the results of a survey of the obsidian sources on the island of Giali in the Dodecanese, Greece, together with a review of these raw materials' use from the Mesolithic to the Late Bronze Age (ninth to second millennium Cal bc). Elemental characterization of 76 geological samples from 11 sampling locations demonstrates the existence of two geochemically distinct sources, termed `Giali A', and `Giali B'. The latter material, available in small cobble form on the island's southwestern half, seems to have only been exploited by local residents during the Final Neolithic (fourth millennium Cal bc). In contrast, Giali A obsidian comprises a distinctive white-spotted raw material, available in large boulders on the northeastern half of Giali, whose use changed significantly over time. During the Mesolithic to later Neolithic it was mainly used for flake-based tool-production by local Dodecanesian populations. Further away, handfuls of Giali A obsidian are documented from Early Neolithic to Early Bronze Age sites in Crete, the Cyclades, and western Anatolia. The distribution of this material is likely indicative of population movement, and regional socio-economic interaction more generally, rather than a significant desire for, and trade of, the material itself. This changed in the Middle Bronze Age (second millennium Cal bc), when Giali A obsidian was reconceptualized as a valued raw material, and used by Cretan palace-based lapidaries to make prestige goods. This radical shift in traditions of consumption resulted from Cretan factions appropriating Anatolian and Egyptian elite value regimes and craft practices as a means of creating new means of social distinction within a larger Eastern Mediterranean political arena

    Wolfram syndrome 1 gene negatively regulates ER stress signaling in rodent and human cells

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    Wolfram syndrome is an autosomal-recessive disorder characterized by insulin-dependent diabetes mellitus, caused by nonautoimmune loss of β cells, and neurological dysfunctions. We have previously shown that mutations in the Wolfram syndrome 1 (WFS1) gene cause Wolfram syndrome and that WFS1 has a protective function against ER stress. However, it remained to be determined how WFS1 mitigates ER stress. Here we have shown in rodent and human cell lines that WFS1 negatively regulates a key transcription factor involved in ER stress signaling, activating transcription factor 6α (ATF6α), through the ubiquitin-proteasome pathway. WFS1 suppressed expression of ATF6α target genes and repressed ATF6α-mediated activation of the ER stress response element (ERSE) promoter. Moreover, WFS1 stabilized the E3 ubiquitin ligase HRD1, brought ATF6α to the proteasome, and enhanced its ubiquitination and proteasome-mediated degradation, leading to suppression of ER stress signaling. Consistent with these data, β cells from WFS1-deficient mice and lymphocytes from patients with Wolfram syndrome exhibited dysregulated ER stress signaling through upregulation of ATF6α and downregulation of HRD1. These results reveal a role for WFS1 in the negative regulation of ER stress signaling and in the pathogenesis of diseases involving chronic, unresolvable ER stress, such as pancreatic β cell death in diabetes
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