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北美花粉记录提供了关于人类新世纪宏观生态变化的证据
M Allison Stegner1, Trisha L Spanbauer2
1Department of Biology, Stanford University, Stanford, CA 94305.
概括
人类活动造成的生态变化与最后一个冰川 - 冰川间过渡时期相似. 对北美花粉记录的分析揭示了近期生物多样性的重大转变和社区重组.
科学领域:
- 古生物学的古生物学
- 生态生态学 生态生态学
- 气候科学 气候科学
背景情况:
- 人类活动正在推动全球生态变化,标志着人类世.
- 了解长期生态轨迹对于将当前的生物多样性丧失置于环境中至关重要.
研究的目的:
- 分析北美自浮世纪晚期以来的生物多样性和社区组成变化.
- 为了比较最近的人为影响与过去的自然环境变化.
主要方法:
- 利用了来自Neotoma数据库的四年纪晚期花粉记录.
- 测量了分类学丰富性,损失/收益,第一次/最后一次出现 (FAD/LAD) 和社区的突然变化.
- 考虑到年龄模型的不确定性和样本大小的变化,以保守的估计.
主要成果:
- 在普莱斯托时代-全新时代过渡期间和过去200年观察到的高植被变化信号.
- 在普世到全新世过渡期间,突然变化和FADs的增加.
- 自200 cal YBP以来,检测到短期分类学损失的增加,FADs,LADs,以及社区的突然变化.
结论:
- 最近的人类影响引发了与冰川 - 间冰川过渡相似的景观变化.
- 生物多样性模式显示区域的变化,最近的变化是显著的.
- 这项研究强调了人类世时期发生的深刻生态重组.
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