南美洲伊纪高植物多样性:来自巴塔哥尼亚的证据
Peter Wilf1, N Rubén Cúneo, Kirk R Johnson
1Department of Geosciences, Pennsylvania State University, University Park, PA 16802, USA. pwilf@geosc.psu.edu
概括
南美洲的古代植物多样性很高,早于最近的地质时期. 来自巴塔哥尼亚的化石叶片记录揭示了丰富的伊欧纪植物群,挑战了热带植物多样性的先前时间表.
科学领域:
- 古植物学是古植物学.
- 古气候学 古气候学
- 南美地质学 南美地质
背景情况:
- 目前,南美是全球陆地植物多样性最高的地区.
- 在历史上,这种异常丰富的植物被归因于最近的地质发展,特别是新生代或世时期.
- 之前的研究在很大程度上忽视了这个地区古老的,高多样性植物的潜力.
研究的目的:
- 为了调查在阿根廷巴塔哥尼亚发现的化石植物的年龄和多样性.
- 为了确定南美洲高植物多样性是否有古老的起源.
- 为了重建中度的世气候和植被.
主要方法:
- 在巴塔哥尼亚拉古纳德尔亨科湖 (Laguna del Hunco) 的火山湖床上对102种叶子进行古植物学分析.
- 放射性同位素测年法用于确定化石沉积物的年龄.
- 古磁分析以确定古度和完善日期.
主要成果:
- 化石植物可以追溯到5200万年前,这与早期欧气候最佳时期相吻合.
- 植物群中包含102种不同的叶子物种,其丰富性超过其他已知的纪叶子植物群,当调整样本大小时.
- 有证据表明,温暖,平衡的气候延伸到中度,支持热带植物种类.
结论:
- 南美洲的高植物多样性比以前假设的历史要古老得多,可以追溯到纪.
- 这些发现支持南美洲温暖地区古老多样化的热带动植物的存在.
- 这项研究修订了南美洲非凡的植物生物多样性起源的时间表.
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