最古の硬骨魚類化石が初期脊椎動物進化を解明(Oldest Known Bony Fish Fossils Uncover Early Vertebrate Evolution)

2026-03-05 中国科学院(CAS)

中国科学院(CAS)脊椎動物古生物学・古人類学研究所(IVPP)の研究チームは、シルル紀の地層から世界最古の硬骨魚類化石を発見し、脊椎動物進化の初期段階を明らかにした。重慶の約4億3600万年前の地層から発見されたEosteus chongqingensisは体長約3cmながら全身が保存された最古の完全な硬骨魚化石である。また雲南省曲靖の約4億2300万年前の地層から見つかったMegamastax amblyodusは当時最大級(1m超)の脊椎動物で、CT解析により頭骨や歯の構造が詳細に復元された。系統解析の結果、これらは条鰭類と肉鰭類が分岐する以前の「幹群硬骨魚類」に位置づけられ、顎や歯の進化過程を理解する重要な証拠となった。本研究は、魚類から四足動物、そして人類へと続く進化の空白を埋める成果であり、中国南部が初期顎口類進化の重要な起源地であることを示している。

最古の硬骨魚類化石が初期脊椎動物進化を解明(Oldest Known Bony Fish Fossils Uncover Early Vertebrate Evolution)
Fossil and high-resolution CT reconstruction of Megamastax amblyodus. (Image by IVPP)

<関連情報>

シルル紀初期の最古の関節式硬骨魚類 The oldest articulated bony fish from the early Silurian period

You-An Zhu,Yang Chen,Qiang Li,Wen-Jin Zhao,Zheng-Da Zhou,Lian-Tao Jia,Yi-Lun Yu,Han-Xin Yu,Guang-Biao Wei,Per E. Ahlberg,Jing Lu & Min Zhu
Nature  Published:04 March 2026
DOI:https://doi.org/10.1038/s41586-026-10125-2

Abstract

Osteichthyans, comprising sarcopterygians and actinopterygians, dominate modern vertebrate biodiversity1,2,3, yet their pre-Devonian fossil record remains scarce and fragmentary4,5. The oldest articulated sarcopterygian6 and stem osteichthyan7 date to the late Silurian, whereas undisputed actinopterygian fossils in articulation appear only in the Middle Devonian8. Here we report an articulated, near-complete osteichthyan from the early Silurian Chongqing Lagerstätte (approximately 436 million years ago)9,10,11, representing the oldest osteichthyan occurrence including microfossils. This tiny fish exhibits a fusiform, generalized osteichthyan body outline, with plesiomorphic osteichthyan characters, including the lack of lepidotrichia and the presence of serial median dorsal plates, pectoral and dorsal fin spines and an anal fin spine reported previously exclusively in stem chondrichthyans12 and one placoderm13. It also displays features, such as a single dorsal fin and caudal fulcra, seen commonly in actinopterygians. Bayesian inference and the 50% majority rule consensus of the maximum-parsimony analysis place the new fish on the osteichthyan stem, whereas the strict consensus leaves its position unresolved within osteichthyans. This discovery increases Silurian osteichthyan diversity and further populates the osteichthyan stem group. The morphological disparity among early osteichthyans implies a more extensive Silurian to Early Devonian radiation of bony fishes than previous lines of evidence suggested.

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