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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Biogeomorphological disturbance regimes: progress in linking ecological and geornorphological systems
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Biogeomorphological disturbance regimes: progress in linking ecological and geornorphological systems

机译:生物地貌扰动机制:将生态学与地貌学系统联系起来的进展

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Understanding the complex, non-linear ways in which linked ecological and geomorphological systems respond to disturbance is important to improving both theoretical understanding and practical environmental management. Some simple conceptual models have been proposed to describe biogeomorphological responses to disturbance within fluvial and aeolian environments, and are reviewed here. Recent research on the interactions between ecological and geomorphological processes in rock breakdown, aeolian, hillslope, fluvial and coastal wetland process regimes indicates a number of additional factors which need to be considered by such models in order to provide a more realistic representation. In particular, many empirical studies point to complex interactions between vegetation, microphytic crusts and animal action (bioturbation and grazing) in a wide range of sediment systems, which act as intrinsic feedback factors complicating the response of these systems to disturbances such as climate change and human action. Improved understanding of these interactions will help effective environmental management, as exemplified by salt marsh restoration schemes. Furthermore, better specification of biogeomorphological interactions can provide insights into large-scale, long-term Earth systems dynamics problems such as the long-term carbon cycle. Copyright (c) 2008 John Wiley & Sons, Ltd.
机译:了解相互联系的生态系统和地貌系统对干扰的复杂,非线性方式,对于提高理论理解和实际环境管理都很重要。已经提出了一些简单的概念模型来描述河流和风环境中对扰动的生物地貌响应,并在此进行了综述。对岩石破坏,风成,山坡,河流和沿海湿地过程机制中的生态和地貌过程之间相互作用的最新研究表明,此类模型需要考虑许多其他因素,以便提供更真实的表示。特别是,许多实证研究都指出,在广泛的沉积物系统中,植被,微植​​皮和动物活动(生物扰动和放牧)之间的复杂相互作用是内在的反馈因素,使这些系统对诸如气候变化和气候变化等干扰的响应变得复杂。人类的行动。更好地理解这些相互作用将有助于有效的环境管理,例如盐沼恢复计划。此外,更好地规范生物地貌相互作用可以提供对大规模,长期地球系统动力学问题(例如长期碳循环)的见解。版权所有(c)2008 John Wiley&Sons,Ltd.

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