Runnegar B, Pojeta J
Science. 1974 Oct 25;186(4161):311-7. doi: 10.1126/science.186.4161.311.
Stasek (1) theorized that the extant mollusks are the progeny of three separate lineages that separated before the phylum was well established. He wrote that no known intermediate forms, fossil or living, bridge the "enormous gaps between any two of the three lineages," and therefore treated each as a separate subphylum. These subphyla are (i) the subphylum Aculifera Hatscheck 1891, containing only the class Aplacophora, derived from the most primitive ancestors of the Mollusca; (ii) the subphylum Placophora von Jhering 1876, containing only the class Polyplacophora, and emphasizing the pseudometamerism of its more advanced premollusk ancestor; and (iii) the subphylum Conchifera Gegenbaur 1878, containing the Monoplacophora and the other classes derived from it. We point out that the Polyplacophora may be derived from the Monoplacophora instead of a more primitive ancestral stock. We also suggest that the Conchifera can be separated into two major lineages, each worthy of the rank of subphylum. The fossil record indicates that the Monoplacophora gave rise to the Gastropoda, Cephalopoda, Rostroconchia, and possibly Polyplacophora, and that the Pelecypoda and Scaphopoda are derived from the Rostroconchia. These last three classes thus form a lineage that diverged from the Monoplacophora in the Early Cambrian. They emphasized a shell form that in all groups is primitively open at both ends, allowing the gut to remain relatively straight, with an anterior mouth and posterior anus. They became burrowing (infaunal) deposit or filter feeders. We coin the term Diasoma (through-body) for the subphylum containing these three classes (Rostroconchia, Pelecypoda, and Scaphopoda). The remaining three classes (Monoplacophora, Gastropoda, and Cephalopoda) emphasize a conical univalved shell, usually twisted into a spiral. The relatively small single aperture forces the anus to lie close to the mouth, and the gut is bent into a "U." Most are surface-dwelling (epifaunal) grazers or carnivores. We coin the name Cyrtosoma (hunchback-body) for the subphylum containing these three classes. Strictly speaking, the cyrtosomes are the ancestors of the diasomes but, in fact, both subphyla appeared and began to diversify within a few million years in the Early Cambrian. Note added in proof: After proofs were corrected we were informed that the new genus Opikella (40) is preoccupied by (Opikella = Oepikella) Thorslund 1940, an Ordovican ostracod. We rename the mollusk genus Oepikila.
斯塔塞克(1)提出理论,认为现存的软体动物是三个独立谱系的后代,这些谱系在该门动物尚未完全确立之前就已分离。他写道,没有已知的中间形式,无论是化石还是现存的,能够填补这三个谱系中任意两个之间的“巨大差距”,因此将每个谱系都视为一个独立的亚门。这些亚门分别是:(i)1891年哈茨克命名的无板亚门,仅包含单板纲,源自软体动物最原始的祖先;(ii)1876年冯·耶林命名的多板亚门,仅包含多板纲,并强调其更高级的前软体动物祖先的拟分节现象;(iii)1878年格根鲍尔命名的有壳亚门,包含单板纲以及由此衍生出的其他纲。我们指出,多板纲可能源自单板纲,而非更原始的祖先种群。我们还建议,有壳亚门可分为两个主要谱系,每个谱系都有资格列为亚门。化石记录表明,单板纲演化出了腹足纲、头足纲、喙壳纲,可能还包括多板纲,而双壳纲和掘足纲则源自喙壳纲。因此,后三个纲形成了一个在寒武纪早期从单板纲分化出来的谱系。它们强调一种贝壳形态,在所有类群中,贝壳最初两端都是开口的,使肠道保持相对笔直,前端有口,后端有肛门。它们成为穴居(底内动物)的沉积物或滤食性动物。我们为包含这三个纲(喙壳纲、双壳纲和掘足纲)的亚门创造了“通体亚门”(Diasoma,意为贯穿身体)这个术语。其余三个纲(单板纲、腹足纲和头足纲)则强调一种圆锥形的单壳,通常扭曲成螺旋状。相对较小的单一开口迫使肛门靠近口部,肠道弯曲成“U”形。大多数是体表生活(表栖动物)的草食性或肉食性动物。我们为包含这三个纲的亚门创造了“驼背体亚门”(Cyrtosoma,意为驼背身体)这个名称。严格来说,驼背体亚门是通体亚门的祖先,但实际上,这两个亚门在寒武纪早期的几百万年内都出现并开始分化。校样后补注:校样校正后我们得知,新属奥皮凯拉(40)已被1940年的托尔斯特伦德(奥皮凯拉 = 厄皮凯拉)占用,厄皮凯拉是一种奥陶纪介形虫。我们将软体动物属奥皮基拉重新命名。