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The Anthropocene: Is there a geomorphological case?

机译:人类世:是否存在地貌学案例?

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摘要

The 'Anthropocene', as used to describe the interval of recent Earth history during which humans have had an 'overwhelming' effect on the Earth system, is now being formally considered as a possible new geological Epoch. Such a new geological time interval (possibly equivalent to the Pleistocene Epoch) requires both theoretical justification as well as empirical evidence preserved within the geological record. Since the geological record is driven by geomorphological processes that produce terrestrial and near-shore stratigraphy, geomorphology has to be an integral part of this consideration. For this reason, the British Society for Geomorphology (BSG) has inaugurated a Fixed Term Working Group to consider this issue and advise the Society on how geomorphologists can engage with debates over the Anthropocene. This ESEX Commentary sets out the initial case for the formalisation of the Anthropocene and a priori considerations in the hope that it will stimulate debate amongst, and involvement by, the geomorphological community in what is a crucial issue for the discipline. The Working Group is now considering the practical aspects of such a formalization including the relative magnitude problem, the boundary problem and the spatial diachrony of 'anthropogenic geomorphology'.
机译:用来描述人类最近对地球系统造成“压倒性”影响的最近人类历史间隔的“人类世”现在被正式认为是可能的新地质时代。这种新的地质时间间隔(可能等同于更新世),既需要理论依据,也需要在地质记录中保存的经验证据。由于地质记录是由产生陆地和近岸地层的地貌过程驱动的,因此地貌学必须成为这一考虑的组成部分。因此,英国地貌学会(BSG)成立了一个固定期限工作组,以考虑该问题,并就该地貌学家如何参与人类世的辩论向该学会提供建议。该《 ESEX评论》列出了人类世正式化的初步案例和先验考虑,希望它能激发地貌学界之间的辩论,并促使地貌学界对该学科的关键问题进行探讨。工作组现在正在考虑这种形式化的实际方面,包括相对幅度问题,边界问题和“人为地貌”的空间历时。

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