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A Silurian placoderm with osteichthyan-like marginal jaw bones
Min Zhu1, Xiaobo Yu, Per Erik Ahlberg
1Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China. zhumin@ivpp.ac.cn
A 419-million-year-old placoderm fish fossil reveals jawed vertebrates (gnathostomes) likely evolved dermal jaw bones before splitting into cartilaginous and bony fish lineages. This finding reshapes our understanding of early vertebrate evolution.
Area of Science:
- Paleontology
- Evolutionary Biology
- Vertebrate Zoology
Background:
- Gnathostomes (jawed vertebrates) consist of Chondrichthyes (cartilaginous fish) and Osteichthyes (bony fish and tetrapods).
- Key differences include the presence of large dermal bones in Osteichthyes, absent in Chondrichthyes.
- The evolutionary origin of these dermal bones and the ancestral gnathostome morphology are debated.
Purpose of the Study:
- To describe a newly discovered stem gnathostome fossil.
- To investigate the phylogenetic position of this fossil within gnathostome evolution.
- To infer the characteristics of the last common ancestor of crown gnathostomes.
Main Methods:
- Description of a 3D-preserved 419-million-year-old placoderm fish from the Silurian of China.
- Phylogenetic analysis incorporating morphological data.
Main Results:
- The fossil represents the first stem gnathostome with dermal marginal jaw bones (premaxilla, maxilla, dentary).
- Phylogenetic analysis places the new form high in the gnathostome stem group, near the divergence of major clades.
- Acanthodians are assigned to the chondrichthyan stem group.
Conclusions:
- The last common ancestor of Chondrichthyes and Osteichthyes likely possessed a macromeric dermal skeleton.
- This discovery provides a new framework for understanding the divergence of jawed vertebrates.
- It suggests dermal jaw bones evolved prior to the split between cartilaginous and bony fish lineages.
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