グランドキャニオンは初期動物進化の“ゴルディロックスゾーン”だった(Grand Canyon was a ‘Goldilocks zone’ for the evolution of early animals)

2025-07-23 ケンブリッジ大学

ケンブリッジ大学の研究チームが、米グランドキャニオンでカンブリア紀の軟体動物化石を初めて発見。従来は硬質化石が主だった同地で、泥岩から数千点の微小化石片を酸処理とふるい分けで回収。歯や摂食器官などの構造が確認され、進化初期の動物に高度な摂食機構が存在した可能性が示唆された。発見は「Science Advances」に掲載され、グランドキャニオンが初期生命進化に理想的な「ゴルディロックス・ゾーン」だったと結論づけた。

<関連情報>

グランドキャニオン(米国アリゾナ州)のカンブリア紀の生物相における進化のエスカレーション Evolutionary escalation in an exceptionally preserved Cambrian biota from the Grand Canyon (Arizona, USA)

Giovanni Mussini, James W. Hagadorn, Anne E. Miller, Karl E. Karlstrom, […] , and Nicholas J. Butterfield
Science Advances  Published:23 Jul 2025
DOI:https://doi.org/10.1126/sciadv.adv6383

グランドキャニオンは初期動物進化の“ゴルディロックスゾーン”だった(Grand Canyon was a ‘Goldilocks zone’ for the evolution of early animals)

Abstract

Exceptionally preserved fossil assemblages, or Konservat-Lagerstätten, open direct windows on non-biomineralized faunas that chronicle the Cambrian radiation of animal phyla. However, these assemblages do not typically capture the well-oxygenated, resource-rich environments sustaining most metazoan diversity in modern marine systems. We describe exceptionally preserved and articulated carbonaceous mesofossils from the middle Cambrian (~507 to 502 million years) Bright Angel Formation of the Grand Canyon (Arizona, USA). This biota preserves probable algal and cyanobacterial photosynthesizers together with a range of functionally sophisticated metazoan consumers: suspension-feeding crustaceans, substrate-scraping molluscs, and morphologically exotic priapulids with complex filament-bearing teeth, convergent on modern microphagous forms. The Grand Canyon’s extensive ichnofossil and sedimentological records show that these phylogenetically and functionally derived taxa occupied highly habitable shallow-marine environments, sustaining higher levels of benthic activity than broadly coeval macrofossil Konservat-Lagerstätten. These data suggest that evolutionary escalation in resource-rich Cambrian shelf settings was an important driver of the assembly of later Phanerozoic ecologies.

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