概括
浅水碳酸盐沙中的高酸石矿在深海中转化为低酸石矿. 这种再结晶过程还可以去除,而不会改变骨质感.
科学领域:
- 地质化学 地质化学
- 海洋地质 海洋地质学
- 古代海洋学 古代海洋学 古代海洋学
背景情况:
- 浅水碳酸盐富含高酸的高酸,在埋葬或运输时经历了代谢.
- 以前人们认为深海环境只能溶解高酸酸.
研究的目的:
- 为了研究深海运输后从浅水沙中高酸石的基因转化.
- 了解在深海碳酸盐再结晶过程中和的命运.
主要方法:
- 对从浅海到深海运输的碳酸盐沙子样本的分析.
- 氧同位素分析以追踪再结晶过程.
- 要素分析以确定和的损失.
主要成果:
- 在深海中,高酸转化为低酸.
- 从碳酸盐中发生了大量的出水.
- 由氧同位素证明的再结晶,并没有改变骨碎片的纹理.
结论:
- 深海再结晶是高酸石的重要代谢途径,而不仅仅是溶解.
- 在这种深海转化过程中,和被调动.
- 骨完整性在深海再结晶过程中得到保护.
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