首页> 外文期刊>Zoomorphology >Formation and morphology of epidermal sclerites from a deep-sea hydrothermal vent solenogaster (Helicoradomenia sp., Solenogastres, Mollusca)
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Formation and morphology of epidermal sclerites from a deep-sea hydrothermal vent solenogaster (Helicoradomenia sp., Solenogastres, Mollusca)

机译:深海热液喷口狼蛛(Helicoradomenia sp。,Solenogastres,Mollusca)的表皮巩膜的形成和形态

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摘要

The deep-sea hydrothermal vent solenogaster Helicoradomenia is covered with calcium carbonate sclerites. Light and electron microscopy reveal varying morphologies of these sclerites. Many sclerites have hollow tips and/or are pitted and etched. Bacteria are found on and in sclerites. Initial sclerite formation occurs in an extracellular crystalline chamber formed by the invagination of a cuboidal basal cell of the columnar microvillus mantle epithelium. As the sclerite grows, it fills the crystalline chamber resulting in direct contact with the microvilli of both the basal cell and neighboring secondary sclerite-forming cells. These cells shape a collar around the base of the growing sclerite. As growth continues, the sclerite-forming cells stretch around the sclerite forming a sheath in which the base of the sclerite resides. Mature sclerites grow through the cuticle into the external environment. The erosion pattern of sclerites reveals a less stable inner medullary region and a harder outer cortical region. This points to a secondary character state, where foremost hollow acicular sclerites develop into solid sclerites. This is in agreement with the systematic position of the genus Helicoradomenia within Simrothiellidae, a taxon typically with hollow sclerites.
机译:深海热液喷口千层金龟膜覆盖有碳酸钙硬钙石。光镜和电子显微镜揭示了这些硬锰矿的不同形态。许多巩膜石具有空心尖端和/或有凹坑并被蚀刻。在巩膜石上和之中发现细菌。最初的硬核形成发生在由柱状微绒毛膜幔上皮的立方基底细胞的内陷形成的细胞外晶体腔中。随着硬核的生长,它充满了晶体腔,导致与基底细胞和邻近的次级硬核形成细胞的微绒毛直接接触。这些细胞在生长的硬核基部周围形成领口。随着生长的继续,形成硬核的细胞围绕着硬核伸展,形成了鞘,硬核的基部位于其中。成熟的巩膜通过表皮生长到外部环境中。硬脂岩的侵蚀模式显示出较不稳定的内部髓质区域和较硬的外部皮质区域。这指向次要特征状态,在该状态下,最先的空心针状硬质岩发展成固态硬质岩。这与螺旋藻属在Simrothiellidae中的系统位置一致,Simrothiellidae是典型的具有空心巩膜的分类群。

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