School of Biological Sciences, University of Bristol, Life Sciences, Building, 24 Tyndall Avenue, Bristol BS8 1TQ, UK.
School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol BS8 1RJ, UK.
Nature. 2017 Feb 23;542(7642):471-474. doi: 10.1038/nature21055. Epub 2017 Feb 6.
Exceptionally preserved fossils provide crucial insights into extinct body plans and organismal evolution. Molluscs, one of the most disparate animal phyla, radiated rapidly during the early Cambrian period (approximately 535-520 million years ago (Ma)). The problematic fossil taxa Halkieria and Orthrozanclus (grouped in Sachitida) have been assigned variously to stem-group annelids, brachiopods, stem-group molluscs or stem-group aculiferans (Polyplacophora and Aplacophora), but their affinities have remained controversial owing to a lack of preserved diagnostic characters. Here we describe a new early sachitid, Calvapilosa kroegeri gen. et sp. nov. from the Fezouata biota of Morocco (Early Ordovician epoch, around 478 Ma). The new taxon is characterized by the presence of a single large anterior shell plate and polystichous radula bearing a median tooth and several lateral and uncinal teeth in more than 125 rows. Its flattened body is covered by hollow spinose sclerites, and a smooth, ventral girdle flanks an extensive mantle cavity. Phylogenetic analyses resolve C. kroegeri as a stem-group aculiferan together with other single-plated forms such as Maikhanella (Siphogonuchites) and Orthrozanclus; Halkieria is recovered closer to the aculiferan crown. These genera document the stepwise evolution of the aculiferan body plan from forms with a single, almost conchiferan-like shell through two-plated taxa such as Halkieria, to the eight-plated crown-group aculiferans. C. kroegeri therefore provides key evidence concerning the long debate about the crown molluscan affinities of sachitids. This new discovery strongly suggests that the possession of only a single calcareous shell plate and the presence of unmineralised sclerites are plesiomorphic (an ancestral trait) for the molluscan crown.
保存异常完好的化石为已灭绝的身体形态和生物进化提供了重要的见解。软体动物是动物界最多样化的门之一,在寒武纪早期(约 5.35-5.20 亿年前)迅速辐射。有问题的化石分类群 Halkieria 和 Orthrozanclus(归入 Sachitida)被归入不同的环节动物、腕足动物、软体动物或原始刺胞动物(多板纲和无板纲)的干群,但由于缺乏保存完好的鉴别特征,它们的亲缘关系一直存在争议。本文描述了一种来自摩洛哥 Fezouata 生物群的新的早期 Sachitida 属 Calvapilosa kroegeri gen. et sp. nov.(早奥陶世,约 4.78 亿年前)。新的分类群的特征是具有单个大的前壳板和多列式的齿舌,带有一个中齿和多个侧齿和后齿,超过 125 排。其扁平的身体被中空的刺状骨板覆盖,一个光滑的腹带位于广泛的套膜腔旁边。系统发育分析将 C. kroegeri 解析为与其他单壳形式(如 Maikhanella(Siphogonuchites)和 Orthrozanclus)一起的原始刺胞动物干群;Halkieria 被恢复为更接近刺胞动物冠群的位置。这些属记录了刺胞动物身体形态从具有单个类似海螺壳的形式到具有两个壳板的形式(如 Halkieria)的逐步进化,到八壳板的冠群刺胞动物。因此,C. kroegeri 为关于 Sachitida 干群软体动物亲缘关系的长期争论提供了关键证据。这一新发现强烈表明,只有一个钙质壳板和未矿化的骨板的存在是软体动物冠群的原始特征(祖先特征)。