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Freezing in a warming climate: Marked declines of a subnivean hibernator after a snow drought

机译:在温暖的气候中冻结:在雪水干旱后亚因冬二二嵌体的下降

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摘要

Recent snow droughts associated with unusually warm winters are predicted to increase in frequency and affect species dependent upon snowpack for winter survival. Changes in populations of some cold‐adapted species have been attributed to heat stress or indirect effects on habitat from unusually warm summers, but little is known about the importance of winter weather to population dynamics and how responses to snow drought vary among sympatric species. We evaluated changes in abundance of hoary marmots (Marmota caligata) over a period that included a year of record‐low snowpack to identify mechanisms associated with weather and snowpack. To consider interspecies comparisons, our analysis used the same a priori model set as a concurrent study that evaluated responses of American pikas (Ochotona princeps) to weather and snowpack in the same study area of North Cascades National Park, Washington, USA. We hypothesized that marmot abundance reflected mechanisms related to heat stress, cold stress, cold exposure without an insulating snowpack, snowpack duration, atmospheric moisture, growing‐season precipitation, or select combinations of these mechanisms. Changes in marmot abundances included a 74% decline from 2007 to 2016 and were best explained by an interaction of chronic dryness with exposure to acute cold without snowpack in winter. Physiological stress during hibernation from exposure to cold, dry air appeared to be the most likely mechanism of change in marmot abundance. Alternative mechanisms associated with changes to winter weather, including early emergence from hibernation or altered vegetation dynamics, had less support. A post hoc assessment of vegetative phenology and productivity did not support vegetation dynamics as a primary driver of marmot abundance across years. Although marmot and pika abundances were explained by strikingly similar models over periods of many years, details of the mechanisms involved likely differ between species because pika abundances increased in areas where marmots declined. Such differences may lead to diverging geographic distributions of these species as global change continues.
机译:最近与异常温暖的冬季相关的雪水预计频率和影响物种依赖于冬季生存的频率。一些冷适应物种的群体的变化归因于对异常温暖的夏季的栖息地的热应激或间接影响,但对冬季天气对人口动态的重要性几乎是知名的以及如何在合并症中对雪干旱的反应变化。我们在一段时间内评估了包括一年记录低积雪的时期核心土拨鼠(Marmota Caligata)的变化,以确定与天气和积雪相关的机制。要考虑跨校比较,我们的分析将其与并发研究相同的模型,作为同时的研究,该研究评估了美国PIKAS(Ochotona Princeps)对北瀑布国家公园,美国华盛顿州北瀑布国家公园的同一研究区的天气和积雪的回应。我们假设Marmot丰富的反射机制有关的热应力,冷应力,冷曝光而无需绝缘的积雪,积雪持续时间,大气湿度,生长季节降水,或选择这些机制的组合。 Marmot丰富的变化包括2007年至2016年的74%下降,最好是通过在冬季没有积雪的情况下暴露于急性寒冷的慢性干燥的相互作用来解释。冬眠期间的生理压力从暴露于寒冷,干燥空气似乎是土拨鼠丰富的最有可能的变化机制。与冬季天气的变化相关的替代机制,包括从冬眠或改变植被动态的早期出现,都有较低的支持。 HOC营养素质和生产率的后HOC评估并不支持植被动态作为跨越多年土拨鼠的主要驱动因素。虽然Marmot和Pika丰富在多年的时间内通过惊人的类似模型解释,但涉及的机制的细节可能在物种之间存在差异,因为Pika丰富在土拨鼠拒绝的地区增加。随着全球变化的继续,这种差异可能导致这些物种的地理分布。

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