首页> 外文期刊>Geografiska Annaler, Series A. Physical Geography >LICHENOMETRIC DATING (LICHENOMETRY) AND THE BIOLOGY OF THE LICHEN GENUS RHIZOCARPON: CHALLENGES AND FUTURE DIRECTIONS
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LICHENOMETRIC DATING (LICHENOMETRY) AND THE BIOLOGY OF THE LICHEN GENUS RHIZOCARPON: CHALLENGES AND FUTURE DIRECTIONS

机译:测化学定年法(选育术)和立香根瘤菌属的生物学:挑战和未来方向

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Lichenometric dating (lichenometry) involves the use of lichen measurements to estimate the age of exposure of various substrata. Because of low radial growth rates and considerable longevity, species of the crustose lichen genus Rhizocarpon have been the most useful in lichenometry. The primary assumption of lichenometry is that colonization, growth and mortality of Rhizocarpon are similar on surfaces of known and unknown age so that the largest thalli present on the respective faces are of comparable age. This review describes the current state of knowledge regarding the biology of Rhizocarpon and considers two main questions: (1) to what extent does existing knowledge support this assumption; and (2) what further biological observations would be useful both to test its validity and to improve the accuracy of lichenometric dates? A review of the Rhizocarpon literature identified gaps in knowledge regarding early development, the growth rate/size curve, mortality, regeneration, competitive effects, colonization, and succession on rock surfaces. The data suggest that these processes may not be comparable on different rock surfaces, especially in regions where growth rates and thallus turnover are high. In addition, several variables could differ between rock surfaces and influence maximum thallus size, including rate and timing of colonization, radial growth rates, environmental differences, thallus fusion, allelopathy, thallus mortality, colonization and competition. Comparative measurements of these variables on surfaces of known and unknown age may help to determine whether the basic assumptions of lichenometry are valid. Ultimately, it may be possible to take these differences into account when interpreting estimated dates.
机译:地衣测年法(lichenometry)涉及使用地衣测量来估计各种基质暴露的年龄。由于低的径向生长速率和相当长的寿命,地壳类地衣根茎植物的种类在地衣测量中是最有用的。地衣计量学的主要假设是,在已知和未知年龄的表面上,根茎植物的定殖,生长和死亡率都相似,因此在各个面部上存在的最大藻体的年龄相近。这篇综述描述了关于根皮果生物学的当前知识状态,并考虑了两个主要问题:(1)现有知识在多大程度上支持这一假设; (2)进一步的生物学观察将对检验其有效性并提高地衣测量日期的准确性有用吗?根皮植物的文献综述确定了关于早期发育,生长速度/大小曲线,死亡率,更新,竞争效应,定植和在岩石表面上的继承方面的知识差距。数据表明,这些过程在不同的岩石表面上可能不具有可比性,尤其是在生长速率和and流周转率较高的地区。此外,岩石表面之间的几个变量可能会有所不同,并影响最大th体的大小,包括定植的速率和时间,径向生长速率,环境差异,th体融合,化感作用,th体死亡率,定植和竞争。在已知和未知年龄的表面上对这些变量进行比较测量可能有助于确定地衣测定的基本假设是否有效。最终,在解释估计日期时可能会考虑这些差异。

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