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人类时代在功能上和地层学上与全新时代不同
Colin N Waters1, Jan Zalasiewicz2, Colin Summerhayes3
1British Geological Survey, Keyworth, Nottingham NG12 5GG, UK.
概括
人类活动正在留下独特的地质标记, 引发了关于识别新时代的辩论:人类世. 在地层记录中的证据显示了地球系统的重大,持久的变化.
科学领域:
- 地球科学
- 地质学
- 环境科学
背景情况:
- 人类活动对地球系统的影响越来越普遍.
- 关于正式指定一个新的地质时间单位 - - 人类世,以反映这些影响的争论仍在继续.
研究的目的:
- 审查层级记录中的人类标志物.
- 评估人类活动造成的地球系统的功能变化.
- 确定这些标志物是否支持人类世与全新世的分层学区别.
主要方法:
- 对人为标记物的层级记录的审查.
- 在沉积物中分析制造材料 (如,塑料,混凝土).
- 对化石燃料燃烧产生的放射性核素和颗粒物的全球峰值进行检查.
- 对碳,和循环的改变进行评估.
- 评估海平面上升和气候系统的干扰.
- 生物变化的记录,包括物种入侵和灭绝率.
主要成果:
- 制造材料,放射性核素和燃烧颗粒在沉积物中广泛存在.
- 全球元素循环 (碳,,) 呈现实质性的变化.
- 海平面上升和气候变化的速度超过了晚期全新纪.
- 在全球范围内,物种的入侵和灭绝正在加速.
结论:
- 综合的人类信号提供了独特的层级学标志.
- 这些信号区分了人类世与全新世和早期的地质时代.
- 证据支持人类纪作为一个独特的地质时间单位.
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