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A climatic threshold triggers the die-off of peat mosses during an extreme heat wave

机译:在极端热浪中,气候阈值触发泥炭藓的死亡

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摘要

Heat waves, which are projected to be more frequent and intense in a warmer climate, could become a serious threat to plants that rely on water surplus availability, such as bryophytes. Here, I take the advantage of the European summer 2003 climate anomaly to assess the impact of an extreme heat wave on peat mosses of the genus Sphagnum, a group of bryophytes forming the bulk of living and dead biomass in peatlands. With this aim, 20 selected bogs in the Italian Alps were checked for Sphagnum survival in the years following the heat wave. Over the study area, the period May-September 2003 was characterized by higher mean monthly air temperature (13.5 degree C) and lower mean monthly precipitation (87mm) compared with normal climatic conditions (11.5 degree C and 117mm, respectively) so that the heat wave coincided with a drought spell. As a consequence of the unusual water stress, I documented an increased mortality of peat mosses forming high hummocks. In particular, at habitat scale, the distribution of desiccated peat mosses was restricted to the hummock face receiving the greatest amount of solar irradiation. However, at regional scale, the present study identified a climatic threshold, simply defined by the ratio of precipitation to temperature (P:T), which triggered an irreversible desiccation of peat mosses when mean monthly P:T dropped below 6.5(mm: degree C) during May-September 2003. The absence of any sign of recovery after 4 years since the drought must be seen as a harbinger of the deleterious effects of extreme heat waves on organisms not adapted to cope with abrupt climate anomaly.
机译:预计在温暖的气候下,热浪会更加频繁和强烈,可能会对依赖苔藓植物等依靠水余量的植物构成严重威胁。在这里,我利用2003年欧洲夏季气候异常来评估极端热浪对泥炭藓(Sphagnum)的泥炭藓的影响,泥炭藓是一组苔藓植物,在泥炭地中构成了大量的活生物和死生物质。为此目的,在热浪之后的几年中,检查了意大利阿尔卑斯山中20个选定的沼泽的泥炭藓生存情况。在研究区域内,与正常气候条件(分别为11.5摄氏度和117毫米)相比,2003年5月至9月的平均每月气温较高(13.5摄氏度),平均每月降水量较低(87毫米)。波正巧与干旱符咒。由于异常的水分胁迫,我记录了形成高高的草丛的泥炭苔藓的死亡率增加。特别是在栖息地范围内,干燥泥炭苔藓的分布仅限于接受最大量太阳光照射的山岗面。然而,在区域范围内,本研究确定了一个气候阈值,该阈值仅由降水与温度的比值(P:T)定义,当平均每月P:T降至6.5(mm:度)以下时,这触发了泥炭藓的不可逆转的干燥。 C)在2003年5月至9月期间。自干旱以来四年没有任何恢复迹象,这必须视为极端热浪对不适合应对突然的气候异常的生物的有害影响的预兆。

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