石是古老时期的石
Joseph Moysiuk1, Martin R Smith2,3, Jean-Bernard Caron1,4
1Departments of Ecology and Evolutionary Biology and Earth Sciences, University of Toronto, 25 Willcocks Street, Toronto, Ontario M5S 3B2, Canada.
Nature
|January 13, 2017
概括
这项研究重建了坎布里亚海洛弗伦蒂斯岩石, 这些特征表明石与酸盐有关,澄清了它们的进化意义.
科学领域:
- 古生物学
- 进化生物学
- 坎布里亚化石
背景情况:
- 石是丰富的,分布在全球的坎布里亚化石,其生态和进化重要性尚未得到解决.
- 它们的软体解剖学和独特的结质导致了各种分类学分类,通常是 incertae sedis 或与软体动物相关.
研究的目的:
- 为了重建软体解剖学和生态作用的坎布里亚中期的岩石Haplophrentis.
- 为了澄清石在动物王国中的遗传位置.
主要方法:
- 对来自伯吉斯页岩和斯宾斯页岩仓库的1500多个样本进行了检查.
- 软组织的重建,包括食和消化器官,基于特别保存的标本.
主要成果:
- 哈普洛弗伦蒂斯被重新构建成一个半性,表性悬浮料.
- 非常完善的软组织显示出一个Lophophore和一个U形的消化道与一个背侧门.
- 这些特征表明与类动物 (类动物,类动物,类动物) 的亲缘关系.
结论:
- 这些发现确立了石和酸盐之间的明显关系.
- 这显著增加了已知的石形态差异.
- 这项研究解决了长期以来围绕着这一突出的化石群体的分类学不确定性.
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