“人新世”和大加速(1780—2021)  

The Anthropocene and the Great Acceleration, 1780-2021

作　　者：约翰·麦克尼尔 徐露(译) 李星皓(译) John R.McNeill

机构地区：[1]乔治敦大学校务委员会 [2]不详

出　　处：《国际社会科学杂志（中文版）》2022年第2期62-69,7,13,共10页International Social Science Journal（Chinese Edition）

摘　　要：“人新世”是环境史最新的前沿理论之一,是作为新纪元被列入地质年代表的一个新议题。20世纪中叶,地球上的水、能源和生物多样性方面发生了巨大变化,因此这一时段被视为“人新世”的起点。关于“人新世”的起源、确立、具体定义、政治性和潜在影响,学界存在争议,我在本文中对此进行了评述,展现了“人新世”概念的跨学科适应性和不同面向,勾画了全球环境史的时空尺度。The Anthropocene is one of the new conceptions in environmental history, and a new era included in the geological timescale,which is also an issue for further research. In the mid-20 th century, water, energy and bio-diversity on the planet experienced drastic changes, and the moment is seen as the beginning of the Anthropocene. There are disputes over origins, establishment, concrete definition, politics and potential implications of the era, on which I make comments in the lecture to demonstrate the applicability of the concept across disciplines and its different dimensions, and outline the time-space scales for global environmental history.

关 键 词：前沿理论 地质年代表 具体定义 时空尺度 生物多样性 20世纪中叶 跨学科 潜在影响 

分 类 号：X-09[环境科学与工程]