首页> 外文期刊>Journal of Vegetation Science >South Patagonian ombrotrophic bog vegetation reflects biogeochemical gradients at the landscape level.
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South Patagonian ombrotrophic bog vegetation reflects biogeochemical gradients at the landscape level.

机译:巴塔哥尼亚南部的营养缺陷型沼泽植被在景观水平上反映了生物地球化学梯度。

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Question: Which environmental variables affect the floristic composition of south Patagonian bog vegetation along a gradient of climate and biogeochemical changes with increasing distance from the Pacific ocean? Location: Trans-Andean transect (53 degrees S), southern Patagonia Material and Methods: Floristic composition, peat characteristics (water level, decomposition, pH, total nitrogen, total carbon, ash content and plant available P, K, Na, Ca, Mg, Fe, Mn, Zn, and Al) and climatic constraints of ombrotrophic peatlands were measured at 82 plots along a gradient of increasing distance from the Pacific Ocean. Results: Climatic constraints and biogeochemical peat characteristics significantly change with increasing distance from the Pacific. Peatland vegetation shifted from hyperoceanic blanket bogs dominated by cushion forming vascular plants to the west to Sphagnum bogs to the east. Climatic and biogeochemical variables explained a large proportion of the floristic variation along the first DCA axis. The second axis represented a water level gradient. When 'distance to the Pacific' was defined as a covariable in partial CCA, the proportion of variance explained declined for most other variables, especially in the case of annual precipitation and exchangeable base cations and related traits. The differences in biogeochemical characteristics related to peat were mainly attributed to the input of sea-borne cations. Conclusions: While variation in vegetation composition along a longitudinal gradient crossing the southern Andes was attributed to climatic constraints as expected, vegetation composition was also strongly affected by the biogeochemical characteristics of peat. Sea spray was of high ecological importance to peat chemistry and, consequently, to floristic composition. Presumably, south Patagonian peat bogs represent a glimpse of pre-industrial environments, so that these peat bogs may act as reference systems with respect to atmospheric inputs in mire ecology research.
机译:问题:随着距太平洋的距离增加,哪些环境变量会沿气候和生物地球化学变化的梯度影响巴塔哥尼亚南部沼泽植被的植物区系?地点:巴塔哥尼亚南部安第斯山脉横断面(53度)材料和方法:植物区系,泥炭特征(水位,分解,pH,总氮,总碳,灰分和植物有效磷,钾,钠,钙, Mg,Fe,Mn,Zn和Al)和营养约束性泥炭地的气候约束条件是在距太平洋越来越远的梯度的82个样地上进行的。结果:气候限制和生物地球化学泥炭特征随距太平洋的距离增加而显着变化。泥炭地植被从以洋洋垫层为主的垫层沼泽植物转移到西部的泥炭藓沼泽地带,再到东部的泥炭藓沼泽地。气候和生物地球化学变量解释了沿第一DCA轴的大部分植物区系变化。第二轴代表水位梯度。当“到太平洋的距离”被定义为部分CCA中的协变量时,对于大多数其他变量,解释的方差比例下降了,特别是在年降水量和可交换的碱性阳离子及相关性状的情况下。与泥炭有关的生物地球化学特征的差异主要归因于海洋阳离子的输入。结论:尽管沿途穿过安第斯山脉南部的纵向梯度的植被组成变化是由于预期的气候限制,但植被组成也受到泥炭生物地球化学特征的强烈影响。海水喷雾对泥炭化学具有重要的生态意义,因此对植物组成也很重要。据推测,巴塔哥尼亚南部的泥炭沼泽代表了工业前环境的一瞥,因此这些泥炭沼泽可以作为泥潭生态研究中大气输入的参考系统。

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