最古のカンブリア紀微化石が環形動物を保存していることを発見(Earliest Cambrian Microfossils Preserve Ringed Worms)

2026-014-21 中国科学院(CAS)

約5億3500万年前のカンブリア紀初期の微化石から、環形動物(ゴカイ類など)の最古の確実な化石証拠が発見された。研究は中国科学院南京地質古生物研究所などの国際チームにより行われ、PNASに掲載された。中国の寛川鋪層から見つかったリン酸塩化した微小化石は、体節構造と二叉状付属肢を持ち、多毛類に特徴的な形態を示す。新属新種2種が記載され、底生型と遊泳型という異なる生態も確認された。これにより、環形動物は初期から多様化し、多毛類的形態が祖先的であった可能性が支持される。また、遊泳性環形動物の起源は従来より古いことが示された。

最古のカンブリア紀微化石が環形動物を保存していることを発見(Earliest Cambrian Microfossils Preserve Ringed Worms)
Cambrian Fortunian annelids. A–C, Kuanchuanpivermis brevicruris, holotype; B–D, Zhangjiagoivermis longicruris, holotype. (Image by ZHANG Huaqiao)

<関連情報>

カンブリア紀初期の多毛類環形動物 Polychaete annelids from the earliest Cambrian Period

Xiaofeng Xian, Huaqiao Zhang, Shuhai Xiao, +2 , and Baichuan Duan
Proceedings of the National Academy of Sciences  Published:April 20, 2026
DOI:https://doi.org/10.1073/pnas.2538071123

Significance

Annelids (ringed worms) possess an epidermis which secretes a collagenous cuticle prone to decay. Therefore, they have relatively low fossilization potential and have left very few articulated body fossils. Previously reported annelid body fossils in the Cambrian Period come exclusively from Burgess Shale-type fossil localities (<521 Myr old), with compressed two-dimensional preservation. In this study, we report three-dimensionally preserved body fossils of annelids from an early Fortunian Orsten-type fossil locality (ca. 535 Myr old). These represent the oldest known body fossils of annelids in the Phanerozoic and suggest that the earliest Cambrian annelids may have differentiated into polychaete morphologies and that annelids may have had an evolutionary history prior to the Cambrian explosion.

Abstract

Unambiguous body fossils of annelids (ringed worms) first appear in the Cambrian Period but are so far known exclusively as flattened specimens preserved in Burgess Shale-type Lagerstätten. Here, we report phosphatized microfossils, interpreted as polychaete annelids, from a distinct taphonomic window (i.e., three-dimensional Orsten-type preservation) in the earliest Cambrian (early Fortunian Age, ca. 535 Ma) Zhangjiagou Lagerstätte of South China. The fossils are millimetric in length and preserved as three-dimensional endocasts of the body. They exhibit clear trunk segmentation, with each segment bearing a pair of lateral or ventrolateral outgrowths. Two species, Kuanchuanpivermis brevicruris gen. et sp. nov. and Zhangjiagoivermis longicruris gen. et sp. nov., are distinguished based on the relative length of these outgrowths. The lateral outgrowths terminate in a bifurcation into two lobes of equal, subequal, or unequal size, closely resembling the notopodium and neuropodium of annelid parapodia. Both species are interpreted as members of the total-group Annelida. Kuanchuanpivermis brevicruris has relatively short appendages and may have been a benthic annelid similar to modern nereids. Zhangjiagoivermis longicruris closely resembles fossil and extant polychaetes (e.g., Eotomopteris and Tomopteris) in their relatively long appendages, suggesting a swimming lifestyle and representing the earliest known semi-pelagic annelid. These findings indicate that annelids had already acquired a polychaete-like body plan in the Fortunian and that early members of the clade had diverged from their living sister group and differentiated into forms with both short and elongate parapodia by the Fortunian Age.

1703地質
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