Keating Joseph N, Marquart Chloe L, Donoghue Philip C J
School of Earth Sciences, University of Bristol, Life Science Building, 24 Tyndall Avenue, Bristol, BS8 1TQ, UK.
J Morphol. 2015 Jun;276(6):657-80. doi: 10.1002/jmor.20370. Epub 2015 Mar 30.
Living vertebrates are divided into those that possess a fully formed and fully mineralised skeleton (gnathostomes) versus those that possess only unmineralised cartilaginous rudiments (cyclostomes). As such, extinct phylogenetic intermediates of these living lineages afford unique insights into the evolutionary assembly of the vertebrate mineralised skeleton and its canonical tissue types. Extinct jawless and jawed fishes assigned to the gnathostome stem evidence the piecemeal assembly of skeletal systems, revealing that the dermal skeleton is the earliest manifestation of a homologous mineralised skeleton. Yet the nature of the primitive dermal skeleton, itself, is poorly understood. This is principally because previous histological studies of early vertebrates lacked a phylogenetic framework required to derive evolutionary hypotheses. Nowhere is this more apparent than within Heterostraci, a diverse clade of primitive jawless vertebrates. To this end, we surveyed the dermal skeletal histology of heterostracans, inferred the plesiomorphic heterostracan skeleton and, through histological comparison to other skeletonising vertebrate clades, deduced the ancestral nature of the vertebrate dermal skeleton. Heterostracans primitively possess a four-layered skeleton, comprising a superficial layer of odontodes composed of dentine and enameloid; a compact layer of acellular parallel-fibred bone containing a network of vascular canals that supply the pulp canals (L1); a trabecular layer consisting of intersecting radial walls composed of acellular parallel-fibred bone, showing osteon-like development (L2); and a basal layer of isopedin (L3). A three layered skeleton, equivalent to the superficial layer L2 and L3 and composed of enameloid, dentine and acellular bone, is possessed by the ancestor of heterostracans + jawed vertebrates. We conclude that an osteogenic component is plesiomorphic with respect to the vertebrate dermal skeleton. Consequently, we interpret the dermal skeleton of denticles in chondrichthyans and jawless thelodonts as independently and secondarily simplified. J. Morphol. 276:657-680, 2015. © 2015 The Authors Journal of Morphology Published by Wiley Periodicals, Inc.
一类拥有完全形成且完全矿化的骨骼(有颌类),另一类仅拥有未矿化的软骨雏形(圆口类)。因此,这些现存谱系的已灭绝系统发育中间类型为脊椎动物矿化骨骼及其典型组织类型的进化组装提供了独特的见解。归入有颌类干群的已灭绝无颌和有颌鱼类证明了骨骼系统的逐步组装,揭示出真皮骨骼是同源矿化骨骼的最早表现形式。然而,原始真皮骨骼本身的性质却知之甚少。这主要是因为先前对早期脊椎动物的组织学研究缺乏推导进化假说所需的系统发育框架。这一点在多鳍鱼纲(一个多样化的原始无颌脊椎动物类群)中最为明显。为此,我们研究了多鳍鱼纲的真皮骨骼组织学,推断出原始多鳍鱼纲骨骼,并通过与其他形成骨骼的脊椎动物类群进行组织学比较,推导出脊椎动物真皮骨骼的祖先性质。多鳍鱼纲最初拥有四层骨骼,包括由牙本质和釉质组成的浅层齿质小体;一层致密的无细胞平行纤维骨,含有为髓管供血的血管网络(L1);一层小梁层,由相交的放射状壁组成,壁由无细胞平行纤维骨构成,显示出类似骨单位的发育(L2);以及一层异质素基层(L3)。多鳍鱼纲 + 有颌脊椎动物的祖先拥有三层骨骼,等同于浅层的L2和L3,由釉质、牙本质和无细胞骨组成。我们得出结论,成骨成分对于脊椎动物真皮骨骼而言是原始的。因此,我们将软骨鱼类和无颌盾皮鱼的小齿真皮骨骼解释为独立且次生简化的。《形态学杂志》276:657 - 680,2015年。© 2015作者 形态学杂志 由威利期刊公司出版