Malakhov V V
Zh Obshch Biol. 2004 Sep-Oct;65(5):371-88.
The paper is an attempt to attack the old problem of the origin of Bilateria by the methods of evolutionary tetrad (i.e. combination of comparative anatomy, comparative embryology, paleontology, and molecular biology). Three groups of theories of classical comparative anatomy (planulod-turbellarian, archicoelomate, and metameric) are discussed. Comparative embryology brings out clearly that the ventral side of embryo comes from the blastoporal region in all groups of Bilateria (except Chordata, where the blastoporal region corresponds to the dorsal side that is come out of the upside-down morphology of chordates) and mouth and anus comes from the anterior and posterior ends of elongated blastopore. From the point of view of paleontology, some of vendian metazoans demonstrate transitional conditions between the Radiata and Bilateria. Vendian bilaterians are metameric organisms with normal or asymmetric position of segments and could be pictured as "bilateral coelenterates" creeping on the oral surface. In Cnidaria, the expression of homologues of "Brachyury", "goosecoid", and "fork head" genes are revealed in the circular region around the mouth. In Bilateria, these genes are expressed along the elongated blastopore and around the mouth and anus. These results support the old conception on the amphistomic origin of mouth and anus as well as the homology between the oral disc of cnidarians and ventral side of Bilateria. The combination of four mentioned approaches enables us to propose the conception of the origin of Bilateria from vendian bilateral coelenterates with numerous metameric pouches of gastral cavity. Bilaterian ancestors crawled on the oral disc (= ventral side). These ancestors gave rise to both phanerosoic cnidarians and triploblastic bilaterians. Cnidarian ancestors attached to bottom by the aboral pole with the resulting degradation of aboral nerve ganglion. Bilateral symmetry of anthozoans is considered to be primitive feature for cnidarians. In case of triploblastic Bilateria, the elongated blastopore closed in the middle and subdivided into mouth and anus (amphistomy) and gastral pouches separated from the central part of gastral cavity and transformed to metameric coelomic chambers. The primary bilaterians are supposed to be complicated organisms having coelom and segmentation. The complexity of primary Bilateria provides an explanation for the abundance of highly organized organisms (arthropods, mollusks etc.) in Cambrian time. It is postulated that Ctenophora is the only group recent eumetazoans with primary axial symmetry.
本文试图通过进化四分法(即比较解剖学、比较胚胎学、古生物学和分子生物学的结合)来探讨两侧对称动物起源这一古老问题。文中讨论了经典比较解剖学的三组理论(扁平涡虫理论、原肠腔理论和分节理论)。比较胚胎学清楚地表明,在所有两侧对称动物类群中(除脊索动物外,脊索动物的胚孔区域对应于因脊索动物形态倒置而形成的背侧),胚胎的腹侧都来自胚孔区域,口和肛门则分别来自拉长胚孔的前端和后端。从古生物学的角度来看,一些文德纪后生动物展示了辐射对称动物和两侧对称动物之间的过渡状态。文德纪两侧对称动物是具有正常或不对称体节位置的分节生物,可以被想象为在口面爬行的“双侧腔肠动物”。在刺胞动物门中,“短尾型”“鹅膏蕈氨酸”和“叉头”基因的同源物在口周围的环形区域表达。在两侧对称动物中,这些基因沿着拉长的胚孔以及口和肛门周围表达。这些结果支持了关于口和肛门两端起源的古老概念,以及刺胞动物口盘与两侧对称动物腹侧之间的同源性。上述四种方法的结合使我们能够提出两侧对称动物起源于具有众多胃腔分节囊的文德纪双侧腔肠动物的概念。两侧对称动物的祖先在口盘(即腹侧)上爬行。这些祖先产生了显生宙的刺胞动物和三胚层两侧对称动物。刺胞动物的祖先通过反口极附着在底部,导致反口神经节退化。珊瑚纲动物的两侧对称被认为是刺胞动物的原始特征。对于三胚层两侧对称动物来说,拉长的胚孔在中间闭合并分成口和肛门(两端开口),胃囊与胃腔的中央部分分离并转化为分节的体腔室。原始两侧对称动物被认为是具有体腔和分节的复杂生物。原始两侧对称动物的复杂性为寒武纪时期高度组织化生物(节肢动物、软体动物等)的丰富性提供了解释。据推测,栉水母动物门是现存唯一具有原始轴向对称的真后生动物类群。