在整个法内罗纪时期记录了Foraminifera试验成分
Katherine Faulkner1,2, Christopher Lowery3, Rowan Clare Martindale1
1Earth and Planetary Sciences, University of Texas at Austin, Austin, TX, USA.
Proceedings. Biological sciences
|April 9, 2025
概括
海洋化物,就像化物一样,表现出对海洋化学的进化反应. 海洋碳酸盐化学的长期变化并不是它们在地质时间内的壁状多样性的主要驱动因素.
科学领域:
- 古生物学的古生物学
- 海洋生物学 海洋生物学
- 地质化学 地质化学
背景情况:
- 海洋化物产生贝和骨,使它们对海洋化学变化敏感.
- 海洋碳酸盐系统变化的长期进化影响尚不清楚.
研究的目的:
- 为了比较石灰质和非石灰质海洋生物对海洋化学变化的反应,在Phanerozoic Eon.
- 为了研究盆地菌壁类型的进化趋势.
主要方法:
- 对2282个盆地类动物属的比例壁型多样性,起源和灭绝率的分析.
- 检查跨越法内罗纪纪 (54.1亿年前到现在) 的数据.
主要成果:
- 石灰质藻的起源和灭绝率在古生代波动,但在中生代稳定下来.
- 石灰岩墙壁类型在整个代保持了大约77%的比例多样性.
- 石灰岩壁类型比例的显著下降仅发生在波斯末期和三叠纪末期的大规模灭绝期间.
结论:
- 罗纪的类动物壁类型进化主要受到当代环境条件的影响,而不是长期的海洋化学趋势.
- 海洋化学变化并不是在地质时间尺度上形成壁类型多样性的主要驱动因素.
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