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石海绵纲骨针硅质沉积的某些方面。

Some aspects of silica deposition in lithistid demosponge desmas.

作者信息

Pisera Andrzej

机构信息

Instytut Paleobiologii, Polska Akademia Nauk, 00-818 Warszawa, Poland.

出版信息

Microsc Res Tech. 2003 Nov 1;62(4):312-26. doi: 10.1002/jemt.10398.

Abstract

Transmitted light microscope and SEM observations of various growth stages, including very young forms, of lithistid demosponge spicules called desmas provided a wealth of new observations on silica deposition in desmas of most lithistid demosponge groups. In typical (pachastrellid) demosponges a basic feature of silica deposition in young spicules is the formation of silica granules (100-160 nm in diameter) deposited in more or less regular concentric layers. Further growth stages in typical demosponges are similar, only silica granules are smaller and more densely packed. The shape of the spicule is controlled by an organic axial filament, while features of the outer spicule surface are also determined by silicalemma. In lithistid desmas the early stage of silica deposition is controlled by an organic axial filament or, in some cases, dispersed organic molecules only. The next step, after early arrest of axial filament growth and its total encasing by silica, is the deposition of various silica granules (40-300 nm in diameter), spheres, and/or cylinders (1,300-3,330 nm), which are either the result of precipitation or the effect of templating by organic molecules (proteins and polysaccharides), without direct control by the silicalemma. The later stages of desma growth are under direct control of the silicalemma, which molds secondary branches and/or elements of sculpture of the desmas. The tips of desmas, which articulate with older desmas, are also controlled by local spatial relationships. Differentiation of morphological forms of silica in desmas, which is at least genus-specific, clearly supports the polyphyletic nature of lithistid sponges.

摘要

对称为骨针的石海绵类(lithistid)海绵骨针不同生长阶段(包括非常幼嫩的形态)进行透射光显微镜和扫描电子显微镜观察,为大多数石海绵类群骨针中二氧化硅沉积提供了大量新观察结果。在典型的(帕氏海绵科)海绵中,幼嫩骨针中二氧化硅沉积的一个基本特征是形成直径为100 - 160纳米的二氧化硅颗粒,这些颗粒以或多或少规则的同心层状沉积。典型海绵的进一步生长阶段类似,只是二氧化硅颗粒更小且堆积更密集。骨针的形状由有机轴向丝控制,而骨针外表面特征也由硅质膜决定。在石海绵类骨针中,二氧化硅沉积的早期阶段由有机轴向丝控制,或者在某些情况下仅由分散的有机分子控制。在轴向丝生长早期停止且其完全被二氧化硅包裹之后的下一步,是沉积各种直径为40 - 300纳米的二氧化硅颗粒、球体和/或圆柱体(1300 - 3330纳米),这些要么是沉淀的结果,要么是由有机分子(蛋白质和多糖)模板化作用的结果,不受硅质膜直接控制。骨针生长的后期阶段由硅质膜直接控制,硅质膜塑造骨针的次生分支和/或雕刻元素。与较老骨针相连的骨针尖端也受局部空间关系控制。骨针中二氧化硅形态形式的分化至少具有属特异性,这清楚地支持了石海绵类海绵的多系性质。

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