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现存单板纲动物(=三槽类:软体动物)中的珍珠层和假珍珠层(叶状文石)。

Nacre and false nacre (foliated aragonite) in extant monoplacophorans (=Tryblidiida: Mollusca).

作者信息

Checa Antonio G, Ramírez-Rico Joaquín, González-Segura Alicia, Sánchez-Navas Antonio

机构信息

Departamento de Estratigrafía y Paleontología, Facultad de Ciencias, Universidad de Granada, Avenida Fuentenueva s/n, 18071, Granada, Spain.

出版信息

Naturwissenschaften. 2009 Jan;96(1):111-22. doi: 10.1007/s00114-008-0461-1. Epub 2008 Oct 9.

Abstract

Extant monoplacophorans (Tryblidiida, Mollusca) have traditionally been reported as having an internal nacreous layer, thus representing the ancestral molluscan condition. The examination of this layer in three species of Neopilinidae (Rokopella euglypta, Veleropilina zografi, and Micropilina arntzi) reveals that only V. zografi secretes an internal layer of true nacre, which occupies only part of the internal shell surface. The rest of the internal surface of V. zografi and the whole internal surfaces of the other two species examined are covered by a material consisting of lath-like, instead of brick-like, crystals, which are arranged into lamellae. In all cases examined, the crystallographic c-axis in this lamellar material is perpendicular to the surface of laths and the a-axis is parallel to their long dimension. The differences between taxa relate to the frequency of twins, which is much higher in Micropilina. In general, the material is well ordered, particularly towards the margin, where lamellae pile up at a small step size, which is most likely due to processes of crystal competition. Given its morphological resemblance to the foliated calcite of bivalves, we propose the name foliated aragonite for this previously undescribed biomaterial secreted by monoplacophorans. We conclude that the foliated aragonite probably lacks preformed interlamellar membranes and is therefore not a variant of nacre. A review of the existing literature reveals that previous reports of nacre in the group were instead of the aragonitic foliated layer and that our report of nacre in V. zografi is the first undisputed evidence of nacre in monoplacophorans. From the evolutionary viewpoint, the foliated aragonite could easily have been derived from nacre. Assuming that nacre represents the ancestral condition, as in other molluscan classes, it has been replaced by foliated aragonite along the tryblidiidan lineage, although the fossil record does not presently provide evidence as to when this replacement took place.

摘要

传统观点认为,现存的单板类动物(软体动物门,笠形腹足目)具有内部珍珠层,因此代表了软体动物的原始状态。对三种新蝶贝科动物(优美罗氏蝶贝、佐氏帆足贝和阿氏微蝶贝)的这一层进行检查后发现,只有佐氏帆足贝会分泌真正的内部珍珠层,且该珍珠层仅占据内壳表面的一部分。佐氏帆足贝内表面的其余部分以及另外两种被检查物种的整个内表面都覆盖着一种由板条状而非砖状晶体组成的物质,这些晶体排列成薄片。在所有被检查的情况下,这种层状物质中的晶体学c轴垂直于板条表面,a轴平行于其长轴方向。不同分类单元之间的差异与孪晶的频率有关,微蝶贝中的孪晶频率要高得多。总体而言,这种物质排列有序,尤其是在边缘处,薄片以很小的步长堆积,这很可能是晶体竞争过程导致的。鉴于其形态与双壳类动物的叶状方解石相似,我们为这种单板类动物分泌的前所未有的生物材料提议了“叶状文石”这一名称。我们得出结论,叶状文石可能缺乏预先形成的层间膜,因此不是珍珠层的变体。对现有文献的回顾表明,该类群中先前关于珍珠层的报道实际上是叶状文石层,而我们关于佐氏帆足贝中珍珠层的报道是单板类动物中珍珠层的首个无可争议的证据。从进化的角度来看,叶状文石很可能是由珍珠层演变而来的。假设珍珠层代表原始状态,就像其他软体动物类群一样,沿着笠形腹足目谱系,它已被叶状文石所取代,尽管目前化石记录并未提供这种取代发生时间的证据。

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