State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, China.
School of Natural Sciences, Macquarie University, Macquarie Park, Australia.
Elife. 2024 Apr 10;12:RP88855. doi: 10.7554/eLife.88855.
Biologically-controlled mineralization producing organic-inorganic composites (hard skeletons) by metazoan biomineralizers has been an evolutionary innovation since the earliest Cambrian. Among them, linguliform brachiopods are one of the key invertebrates that secrete calcium phosphate minerals to build their shells. One of the most distinct shell structures is the organo-phosphatic cylindrical column exclusive to phosphatic-shelled brachiopods, including both crown and stem groups. However, the complexity, diversity, and biomineralization processes of these microscopic columns are far from clear in brachiopod ancestors. Here, exquisitely well-preserved columnar shell ultrastructures are reported for the first time in the earliest eoobolids gen. et sp. nov. and sp. nov. from the Cambrian Series 2 Shuijingtuo Formation of South China. The hierarchical shell architectures, epithelial cell moulds, and the shape and size of cylindrical columns are scrutinised in these new species. Their calcium phosphate-based biomineralized shells are mainly composed of stacked sandwich columnar units. The secretion and construction of the stacked sandwich model of columnar architecture, which played a significant role in the evolution of linguliforms, is highly biologically controlled and organic-matrix mediated. Furthermore, a continuous transformation of anatomic features resulting from the growth of diverse columnar shells is revealed between Eoobolidae, Lingulellotretidae, and Acrotretida, shedding new light on the evolutionary growth and adaptive innovation of biomineralized columnar architecture among early phosphatic-shelled brachiopods during the Cambrian explosion.
后生动物生物矿化作用产生的有机-无机复合材料(硬骨骼)自最早的寒武纪以来一直是进化创新。其中,舌形贝是分泌磷酸钙矿物构建贝壳的关键无脊椎动物之一。最独特的贝壳结构之一是磷酸盐壳腕足动物特有的有机磷质圆柱状柱,包括冠群和干群。然而,这些微观柱的复杂性、多样性和生物矿化过程在腕足动物的祖先中还远不清楚。在这里,首次报道了华南寒武纪第 2 统静水沱组最早的 eoobolids 属。及其种和种具有保存精美的柱状壳超微结构。在这些新物种中,对分层壳结构、上皮细胞模具以及圆柱状柱的形状和大小进行了详细研究。它们的磷酸钙基生物矿化贝壳主要由堆叠的三明治柱状单元组成。堆叠三明治模型的分泌和构建在舌形贝的进化中起重要作用,高度受生物控制和有机基质介导。此外,揭示了 Eoobolidae、Lingulellotretidae 和 Acrotretida 之间不同柱状贝壳生长导致的解剖特征的连续变化,为寒武纪大爆发期间早期磷酸盐壳腕足动物生物矿化柱状结构的进化生长和适应性创新提供了新的认识。