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首页> 外文期刊>Geografiska Annaler, Series A. Physical Geography >Growth Rate Of A Very Large Crustose Lichen (Rhizocarpon Subgenus) And Its Implications For Lichenometry
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Growth Rate Of A Very Large Crustose Lichen (Rhizocarpon Subgenus) And Its Implications For Lichenometry

机译:很大的地壳地衣(根茎亚属)的生长速率及其对地衣测定的意义

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摘要

The growth rate of an individual thallus of the Rhizocarpon subgenus with a current maximum diameter of 465mm was measured directly over a 26-year period at ca 5-year intervals along 10 radii. Mean annual diametral growth rate was 0.48mmyr-1 (the range between individual radii and time intervals was 0.02-1.54mmyr-1). The southeasterly aspect of the lichen may have led to a higher growth rate in years that were relatively cool and dry. Combined with the growth rate of 18 smaller lichens at the site near the Haugabreen glacier in southern Norway, the data support a parabolic growth-rate model. The corresponding growth curve, which is sigmoidal, indicates an age of about 1000 years for the very large lichen. Results also suggest that it may be possible to extend the temporal range of traditional (largest lichen) lichenometric dating in southern Norway. However, despite having been pointed out by R.E. Beschel in the 1950s, there is still an urgent need for further direct lichenometric data, for the monitoring of relatively large lichens and for a better understanding of the factors causing variability in growth rates.
机译:在长达26年的时间内,以大约5年的间隔,沿着10半径,直接测量了当前最大直径为465mm的根茎亚种的单个th的生长速率。年平均直径增长率为0.48mmyr-1(各个半径和时间间隔之间的范围为0.02-1.54mmyr-1)。在相对凉爽和干燥的年份中,地衣的东南方可能导致较高的增长率。结合挪威南部Haugabreen冰川附近站点的18个较小的地衣的增长率,该数据支持抛物线增长率模型。相应的S形生长曲线表明,非常大的地衣的年龄约为1000年。结果还表明,有可能扩大挪威南部传统(最大的地衣)地衣测量的时间范围。然而,尽管R.E.指出。在贝舍尔(Beschel),1950年代,仍然迫切需要进一步的直接地衣测量数据,以监测相对较大的地衣,并更好地理解导致增长率变化的因素。

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