Reynolds Patrick D
Biology Department, Hamilton College, Clinton, NY 13323, USA.
Adv Mar Biol. 2002;42:137-236. doi: 10.1016/s0065-2881(02)42014-7.
The Scaphopoda are marine infaunal carnivores that feed on foraminiferans and other microorganisms selected and manipulated by their unique feeding tentacles or captacula. Their tusk-like shell is open at both ends; the burrowing foot and captacula protrude anteriorly, while respiratory currents pass through the posterior opening. Although the scaphopods comprise one of the smallest molluskan classes in terms of species diversity, they have a worldwide distribution ranging from intertidal to depths in excess of 6000 m. Despite detailed monographic work from the late nineteenth and early twentieth centuries, however, the biology of scaphopods is today among the least understood of mollusks. To some extent, this is related to a significant departure from more typical molluscan organization inferred from studies of the larger classes. For example, the mantle cavity is elongate and restricted in space, and several associated organs are lost, including the osphradium and ctenidia; the latter is associated with the loss of auricles from the scaphopod heart. There is also little record of ontogeny in the adult shell, as the older portion is periodically decollated to maintain the posterior aperture for passage of inhalant and exhalant currents. This and other constraints on scaphopod diversification are reflected in the range limits of shell shape within the class. In contrast, the "Dentalium" egg has been a model system for experimental embryology, particularly in studies of cell lineage and early morphogenesis. Later larval development and most organogenesis is nonetheless poorly known, although recent studies have considerably enhanced our knowledge in this area. Global biogeographic patterns of scaphopod diversity have been studied only preliminarily. A general decrease in diversity with depth is broken by small diversity peaks at bathyal depths. There is also evidence for a marked latitudinal diversity gradient in the world's oceans, near equatorial in the Pacific but at approximately 20 degrees N in the Atlantic. Scaphopods have a wide diversity of ecto- and endo-symbiotic associations with other organisms, including commensal bacteria and ciliates, mutualistic anemones and corals, and parasitic algae and platyhelminths. Other documented associations include predation by naticid gastropods and ratfish, and the inhabitation of empty scaphopod shells by a variety of sipunculans and hermit crabs. Phylogeny within the class is still unresolved, although significant progress has been made recently in documenting morphological variation among families, genera, and species for application in a cladistic context. The evolutionary relationships of Scaphopoda within Mollusca are farther from resolution, with every conchiferan class a proposed sister group among modern analyses. Molecular avenues should provide significant progress in scaphopod phylogenetics, as indicated by recent comparative sequence analysis and gene expression patterns. Scaphopods comprise the most recent class of mollusks to appear in the fossil record, dating at least from the Mississippian Carboniferous (362.5 My). They appear from first-order occurrence data to have a substantially documented fossil record, with several sharp extinction and radiation events evident during their comparatively short geologic history. The unresolved position of the Scaphopoda within molluscan phylogeny, and their relatively limited range of morphological disparity but substantial derivation from other conchiferans, renders the scaphopods an enigmatic group. They represent a significant evolutionary avenue within the Mollusca, but one that is poorly examined. Nonetheless, comprehensive phylogenetic analysis and documentation of diversity within this small, monophyletic, class-level taxon, well-preserved in the fossil record, is imminently tractable, and presents a singular opportunity in the study of molluscan evolution.
掘足纲动物是海洋底栖肉食性动物,以有孔虫和其他微生物为食,这些食物是由它们独特的捕食触手或触腕选择和操控的。它们的象牙状贝壳两端开口;穴居足和触腕向前突出,而呼吸水流则通过后端开口。尽管就物种多样性而言,掘足纲是最小的软体动物类群之一,但它们在全球范围内均有分布,从潮间带到超过6000米的深度都有。然而,尽管在19世纪末和20世纪初有详细的专题研究,但如今掘足纲动物的生物学仍是软体动物中了解最少的。在某种程度上,这与从对较大类群的研究推断出的更典型的软体动物组织有显著差异有关。例如,外套腔细长且空间受限,一些相关器官消失了,包括嗅检器和鳃;后者与掘足纲动物心脏耳状部的丧失有关。成年贝壳的个体发育记录也很少,因为较老的部分会周期性脱落,以保持后端开口用于吸入和呼出水流的通过。这种以及其他对掘足纲动物多样化的限制反映在该类群贝壳形状的范围界限上。相比之下,“角贝”卵一直是实验胚胎学的模型系统,特别是在细胞谱系和早期形态发生的研究中。然而,后期幼虫发育和大多数器官发生仍知之甚少,尽管最近的研究在这一领域大大增加了我们的知识。掘足纲动物多样性的全球生物地理模式仅得到初步研究。随着深度增加多样性总体下降的趋势被深海深度处的小多样性峰值打破。也有证据表明世界海洋中存在明显的纬度多样性梯度,在太平洋靠近赤道,但在大西洋约北纬20度处。掘足纲动物与其他生物有广泛的外共生和内共生关系,包括共生细菌和纤毛虫、互利共生的海葵和珊瑚,以及寄生藻类和扁形虫。其他有记录的关系包括玉螺腹足类动物和银鲛的捕食,以及各种星虫和寄居蟹对空掘足纲动物贝壳的栖息。该纲内的系统发育仍未解决,尽管最近在记录科、属和种之间的形态变异以应用于分支系统学方面取得了重大进展。掘足纲动物在软体动物门中的进化关系距离解决更远,在现代分析中每个有壳类群都被提议为姐妹群。正如最近的比较序列分析和基因表达模式所示分子途径应该会在掘足纲动物系统发育研究中取得重大进展。掘足纲是化石记录中出现的最新的软体动物类群,至少可以追溯到密西西比纪石炭纪(3.625亿年前)。从一级出现数据来看,它们似乎有大量记录的化石记录,在其相对较短的地质历史中明显有几次急剧的灭绝和辐射事件。掘足纲动物在软体动物系统发育中的未解决位置,以及它们相对有限的形态差异范围但从其他有壳类动物大量衍生,使得掘足纲动物成为一个神秘的类群。它们代表了软体动物门内一条重要的进化途径,但却是一个研究较少的途径。尽管如此,对这个小的、单系的、纲级分类单元内的多样性进行全面的系统发育分析和记录,其在化石记录中保存完好,即将变得易于处理,并为软体动物进化研究提供了一个独特的机会。