390 research outputs found

    Aquatic ecosystem response to climate, fire, and the demise of montane rainforest, Tasmania, Australia

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    The 2019/2020 southeast Australian fires ravaged the environment and threatened endemic vegetation groups, including the Tasmanian montane rainforest. This endemic biome, dominated by Athrotaxis species and Nothofagus gunnii, is declining due to increased aridity and fire frequency (years between fire events). Little is known about the impacts of fire and the montane rainforest decline on aquatic ecosystems in the region, yet aquatic ecosystems are strongly reliant on the terrestrial environment for nutrients and humic acids to support their ecosystem health. Here we evaluate the impacts of repeat fires and decline in montane rainforest species on the aquatic ecosystem of Lake Osborne, Tasmania, Australia, during the past 6500 years using a palaeoecological approach. Newly obtained data including organic carbon (δ13C) and nitrogen (δ15N) isotope composition, visible reflectance spectroscopy (R650–700 as a measure of chlorophyll a and derivatives), and diatom remains are compared with previously published charcoal, pollen, micro-X-Ray fluorescence, magnetic susceptibility, and organic carbon and nitrogen elemental data. Results suggest repeat fire occurrence from 6300 to 4200 years ago caused a decline in montane rainforest, increased erosion, and high aquatic productivity, pH, and conductivity (as indicated by diatoms Epithemia species, Fragilaria type species, Karayevia clevei, and Tabellaria flocculosa). Recovery of montane rainforest due to low fire activity from 4200 to 3000 years ago caused an anomalous assemblage of diatoms dominated by Aulacoseira species along with a less productive aquatic environment (inferred from low δ13C and δ15N, R650–700, and percent macrophytes and algal remains), higher lake level and clearer waters at Lake Osborne. A fire event 2500 years ago caused the removal of montane rainforest and a shift to Eucalyptus dominance within the catchment, leading to an increase in aquatic productivity, and a shift toward benthic diatom taxa dominant in clearer waters-characteristic of eastern Tasmanian sites. The aquatic environment at Lake Osborne for the past 6500 years has responded to increased fire frequency, declines in the montane rainforest and climate change. Fire disturbance removes montane rainforest, burns the underlying soils resulting in erosion of terrigenous material and increases aquatic productivity with communities that favour higher conductivity and low light conditions. With projected increases in fire frequency and loss of rainforest, freshwater ecosystems are vulnerable to changes in physical characteristics, productivity, species assemblages, and ecological resilience

    Effect of Metformin Added to Insulin on Glycemic Control Among Overweight/Obese Adolescents With Type 1 Diabetes: A Randomized Clinical Trial

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    Importance Previous studies assessing the effect of metformin on glycemic control in adolescents with type 1 diabetes have produced inconclusive results. Objective To assess the efficacy and safety of metformin as an adjunct to insulin in treating overweight adolescents with type 1 diabetes. Design, Setting, and Participants Multicenter (26 pediatric endocrinology clinics), double-blind, placebo-controlled randomized clinical trial involving 140 adolescents aged 12.1 to 19.6 years (mean [SD] 15.3 [1.7] years) with mean type 1 diabetes duration 7.0 (3.3) years, mean body mass index (BMI) 94th (4) percentile, mean total daily insulin 1.1 (0.2) U/kg, and mean HbA1c 8.8% (0.7%). Interventions Randomization to receive metformin (n = 71) (≤2000 mg/d) or placebo (n = 69). Main Outcomes and Measures Primary outcome was change in HbA1c from baseline to 26 weeks adjusted for baseline HbA1c. Secondary outcomes included change in blinded continuous glucose monitor indices, total daily insulin, BMI, waist circumference, body composition, blood pressure, and lipids. Results Between October 2013 and February 2014, 140 participants were enrolled. Baseline HbA1c was 8.8% in each group. At 13-week follow-up, reduction in HbA1c was greater with metformin (−0.2%) than placebo (0.1%; mean difference, −0.3% [95% CI, −0.6% to 0.0%]; P = .02). However, this differential effect was not sustained at 26-week follow up when mean change in HbA1c from baseline was 0.2% in each group (mean difference, 0% [95% CI, −0.3% to 0.3%]; P = .92). At 26-week follow-up, total daily insulin per kg of body weight was reduced by at least 25% from baseline among 23% (16) of participants in the metformin group vs 1% (1) of participants in the placebo group (mean difference, 21% [95% CI, 11% to 32%]; P = .003), and 24% (17) of participants in the metformin group and 7% (5) of participants in the placebo group had a reduction in BMI z score of 10% or greater from baseline to 26 weeks (mean difference, 17% [95% CI, 5% to 29%]; P = .01). Gastrointestinal adverse events were reported by more participants in the metformin group than in the placebo group (mean difference, 36% [95% CI, 19% to 51%]; P < .001). Conclusions and Relevance Among overweight adolescents with type 1 diabetes, the addition of metformin to insulin did not improve glycemic control after 6 months. Of multiple secondary end points, findings favored metformin only for insulin dose and measures of adiposity; conversely, use of metformin resulted in an increased risk for gastrointestinal adverse events. These results do not support prescribing metformin to overweight adolescents with type 1 diabetes to improve glycemic control
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