海水化学和早期碳酸盐生物矿物化
1Department of Earth Science, University of California at Santa Barbara, Santa Barbara, CA 93106, USA. porter@geol.ucsb.edu
概括
动物骨的矿物学,如阿拉贡石和石,是由海水化学决定的,当它们第一次进化时. 一旦建立,这些矿物质很少发生变化,即使海洋条件也发生了变化.
科学领域:
- 古生物学的古生物学
- 地质化学 地质化学
- 进化生物学 进化生物学
背景情况:
- 动物生物矿物化的进化是早期动物历史的一个关键事件.
- 了解影响骨矿物质选择的环境因素至关重要.
研究的目的:
- 研究海水化学与动物骨的初始矿物学之间的关系.
- 确定骨进化时的海水化学是否影响了长期的矿物学趋势.
主要方法:
- 对从埃迪亚卡朗晚期到奥尔多维纪时期的化石记录进行分析.
- 在18个动物群体中,阿拉贡石和石骨首次出现的相关性与相同间隔的已知海水化学数据.
主要成果:
- 在不同的动物群体中,阿拉戈尼特和石骨的初始沉与每个矿物质有利的海水化学成分的时期相吻合.
- 骨矿物学在最初的进化后,无论以后的海水化学波动,骨矿物学在克拉德内保持稳定.
结论:
- 骨起源时的海水化学是早期动物进化的骨矿物学的主要决定因素.
- 这种早期的环境影响建立了矿物学路径,这些路径在随后的地质变化中持续存在.
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