Skovsted Christian B, Holmer Lars E, Larsson Cecilia M, Högström Anette E S, Brock Glenn A, Topper Timothy P, Balthasar Uwe, Stolk Sandra Petterson, Paterson John R
Department of Earth Sciences, Palaeobiology, Uppsala University, Villavägen 16, 752 36 Uppsala, Sweden.
Proc Biol Sci. 2009 May 7;276(1662):1651-6. doi: 10.1098/rspb.2008.1655. Epub 2009 Jan 20.
Early Cambrian tommotiids are problematic fossil metazoans with external organophosphatic sclerites that have been considered to be basal members of the lophophorate stem group. Tommotiids are almost exclusively known from isolated or rarely fused individual sclerites, which made previous reconstructions of the actual organism highly conjectural. However, the recent discovery of the first articulated specimens of the tommotiid Eccentrotheca revealed a tubular sclerite arrangement (scleritome) that limited the possible life habit to sessile filter feeding and thus further supported a lophophorate affinity. Here, we report the first articulated specimens of a second tommotiid taxon, Paterimitra from the Early Cambrian of the Arrowie Basin, South Australia. Articulated specimens of Paterimitra are composed of two bilaterally symmetrical sclerite types and an unresolved number of small, asymmetrical and irregular crescent-shaped sclerites that attached to the anterior margin of the symmetrical sclerites. Together, the sclerites form an open cone in which the symmetrical sclerites are joined together and form a small posterior opening near the base of the scleritome, while the irregular crescent-shaped sclerites defined a broad anterior opening. The coniform scleritome of Paterimitra is interpreted to have attached to hard substrates via a pedicle that emerged through the small posterior opening (sometimes forming a tube) and was probably a sessile filter feeder. The scleritome of Paterimitra can be derived from the tubular scleritome of Eccentrotheca by modification of basal sclerites and reduction in tube height, and probably represents a more derived member of the brachiopod stem group with the paired symmetrical sclerites possibly homologous to brachiopod valves.
早寒武世的托莫特动物是有问题的化石后生动物,它们具有外部有机磷酸盐化的骨片,曾被认为是触手冠动物干群的基部成员。托莫特动物几乎仅通过孤立的或很少融合的单个骨片为人所知,这使得之前对实际生物体的重建极具推测性。然而,最近发现的托莫特动物偏心鞘的首个连接标本揭示了一种管状骨片排列(骨片组合),这种排列将可能的生活习性限制为固着滤食,从而进一步支持了其与触手冠动物的亲缘关系。在此,我们报告了来自南澳大利亚阿罗伊盆地早寒武世的第二个托莫特动物分类群——父神帽贝的首个连接标本。父神帽贝的连接标本由两种左右对称的骨片类型以及数量未明的小的、不对称且不规则的新月形骨片组成,这些新月形骨片附着在对称骨片的前缘。这些骨片共同形成一个开放的锥体,其中对称骨片连接在一起,在骨片组合基部附近形成一个小的后开口,而不规则的新月形骨片界定了一个宽阔的前开口。父神帽贝的锥形骨片组合被解释为通过一个从后小开口穿出(有时形成一根管子)的柄附着在坚硬基质上,并且可能是一种固着滤食者。父神帽贝的骨片组合可以通过基部骨片的改造和管高的降低从偏心鞘的管状骨片组合演化而来,并且可能代表腕足动物干群中一个更进化的成员,其成对的对称骨片可能与腕足动物的壳瓣同源。