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海洋冷却是否引发了奥尔多维纪生物多样化? 来自体温度测量的证据
Julie A Trotter1, Ian S Williams, Christopher R Barnes
1Research School of Earth Sciences, Australian National University, Mills Road, Canberra ACT 0200, Australia. julie.trotter@anu.edu.au
概括
奥尔多维纪时期不是温室状态,而是稳步冷却,支持现代海洋化学. 这种稳定的气候促进了重要的生命辐射,生物多样性在这个时代增加.
科学领域:
- 古气候学 古气候学
- 古生物学的古生物学
- 地质化学 地质化学
背景情况:
- 奥尔多维纪时期以显著的生命辐射而闻名,但以前被认为是一个超级温室状态.
- 高温估计 (高达70°C) 导致人们对海水氧同位素组成的演变进行猜测.
- 以前的气候模型缺乏对奥尔多维纪全球温度及其对生命的影响的全面了解.
研究的目的:
- 为了重建全球气候记录的早期奥尔多维克到Silurian时期.
- 研究气候在奥尔多维纪前所未有的生物多样性增长中的作用.
- 为了测试奥尔多维纪海水氧同位素组成与现代值有显著差异的假设.
主要方法:
- 氧同位素分析从早期奥尔多维纪到纪的孔 (化石牙).
- 利用离子微探针技术进行精确的同位素测量.
- 基于这些地化学代理,开发了一个新的全球气候记录.
主要成果:
- 一个稳定的冷却趋势通过早期奥尔多维纪被确定.
- 现代赤道温度在整个中期和晚期奥尔多维纪被达到并维持.
- 发现奥尔多维纪海水的氧同位素成分与现代值相似.
结论:
- 奥尔多维纪时期经历了冷却趋势,而不是超级温室状态.
- 稳定,有利的气候条件,类似于现代气候条件,在整个中期和晚期奥尔多维纪盛行.
- 气候在促进这一时期观察到的显著生物多样性扩张方面发挥了关键作用.
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