概括
在智利的普世晚期花粉分析显示,冰河时代的间隔更冷,更湿. 南方西风可能对这个亚热带气候的影响比太平洋反气旋更大.
科学领域:
- 古气候学 古气候学
- 帕利诺学 (Palynology) 是一个临床学科.
- 四分学科学 四分学科学
背景情况:
- 亚热带度的晚期普莱斯托时代气候受大气循环模式的影响.
- 了解过去的气候动态对于预测未来的气候变化至关重要.
- 在全新纪的植被和动物变化为环境变化提供了背景.
研究的目的:
- 用化石花粉重建智利塔瓜湖的冰河时代气候.
- 为了研究大气循环对普莱斯托纪晚期亚热带气候的影响.
- 为了将古老环境变化与动物和人类的存在联系起来.
主要方法:
- 从拉古纳德塔古亚塔古亚的沉积物核心进行花粉分析.
- 南方 (Nothofagaceae) 和 (Podocarpaceae) 花粉的识别和量化.
- 在冰川 - 冰川间周期和大气动态背景下解释花粉数据.
主要成果:
- 花粉聚合表明,在普莱斯托纪晚期,气候更加凉爽和湿.
- 有证据表明,南方西风的影响增加,太平洋反气旋减弱.
- 全新生代植被变迁与古印度人的到来和巨型动物灭绝有关.
结论:
- 在这个亚热带度的晚期普莱斯托时代气候的特点是明显的凉爽,潮湿的间隔.
- 大气循环的变化,特别是较强的西风,在调节区域气候方面发挥了关键作用.
- 全新纪的环境变化是由气候变化和人为因素推动的.
相关概念视频
Global Climate Change
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Speciation Rates
Speciation can proceed at markedly different rates, and evolutionary biologists commonly describe these differences through the models of gradualism and punctuated equilibrium. Both patterns explain how new species arise, but they differ in the tempo and continuity of evolutionary change. In both cases, evolutionary change arises from heritable variation within populations, with natural selection often shaping traits that improve survival and reproduction under specific environmental conditions.


