一个Silurian大层体照亮了下巴的进化
Min Zhu1,2, Per E Ahlberg3, Zhaohui Pan4,2
1Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, PO Box 643, Beijing 100044, China. zhumin@ivpp.ac.cn per.ahlberg@ebc.uu.se.
概括
一个新的Silurian placoderm发现澄清了大骨的演变. 大,前大和牙骨与牙板相同,显示出牙的共同起源.
科学领域:
- 古生物学
- 脊椎动物的进化
- 比较解剖学
背景情况:
- 在Silurian层中发现的Entelognathus呈现了大骨,前大骨和牙骨,挑战了以前的分类.
- 这些边缘骨与其他斑皮动物的牙板之间的同质性,传统上被认为是内部牙廊,仍然没有得到解决.
- 了解这种关系对于追踪脊椎动物下结构的进化起源至关重要.
研究的目的:
- 为了研究在一些石流时期的石流体中发现的牙板和边缘骨 (大,前,牙) 之间的进化联系.
- 澄清这些元素的同质性以及它们对早期牙科廊的贡献.
- 重建脊椎动物进化过程中下结构的转变过程.
主要方法:
- 一个新发现的Silurian大皮样本的分析.
- 不同体群和早期骨质动物之间的元素的比较形态分析.
- 基因组分类来推断同质性和进化关系.
主要成果:
- 新描述的皮表现出中间的特征,弥合了典型的皮板和上结构之间的差距.
- 证据表明,这些西卢里亚甲体的部,前部和牙与其他甲体的牙板相同.
- 这项研究表明,从骨板转变为骨同时发生在上下上.
结论:
- 大,前和牙被整合到牙上,这表明它们与牙板具有共同的进化起源.
- 这种大骨转变早于下骨的进化.
- 这些发现为脊椎动物的器的早期演变提供了关键的见解,特别是向骨类结构的过渡.
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