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石珊瑚骨骼从微米级到整体尺度的两步生长模式。

The two-step mode of growth in the scleractinian coral skeletons from the micrometre to the overall scale.

作者信息

Cuif Jean-Pierre, Dauphin Yannicke

机构信息

UMR 8148 IDES, Geology, bat. 504, Université Paris XI-Orsay, F-91405 Orsay cedex, France.

出版信息

J Struct Biol. 2005 Jun;150(3):319-31. doi: 10.1016/j.jsb.2005.03.004. Epub 2005 Mar 31.

Abstract

It has been known since the 19th century that coral skeletons are built of aragonite crystals with taxonomy-linked arrangements, but the way by which each coral species controls this crystallization process remains an unsolved question. The problem became still more intriguing when it was shown that isotopic compositions of coral aragonite were subject to taxonomy-linked influences (the "vital effect"). On the other hand, presence of an organic component in coral skeletons is also long known, but localization of these compounds is admittedly restricted to particular structures called "centres of calcifications." Fibres, the largely predominant part of the coral skeletons, are usually considered as purely mineral units. In this paper, it is shown that in both "centres of calcification" and fibres, organic compounds are associated with the mineral material at a deep structural level. A series of variously scaled observations and localized measurements allow recognition of the presence of an organic component at the nanometre scale. Far from being a freely operating process, crystallization of coral fibres is thus permanently controlled by the polyp basal ectoderm through a cyclic two-step process acting at the micrometre-scale. The biomineralization cycle begins by secretion of a proteoglycan matrix. As the composition of these sugars-proteins assemblages has been shown taxonomy dependent, the hypothesis can be made that multiple and long recognized specificities of coral skeletons are linked to this biochemically driven crystallization process. Additionally, this new concept of the biomineralization process in coral skeletons provides us with an access to the long term evolution of the Scleractinia. Remarkably, results of a skeleton-based approach using microstructural criteria (i.e., the spatial relationships of "centres of calcification" and the three-dimensional arrangements of fibres), are consistent with a molecular phylogenetic analysis carried out on the same species. Clearly, at the overall ontogenic level, the two-step growth mode of coral skeletons is also a valuable tool to reconstruct the evolutionary history of Scleractinia.

摘要

自19世纪以来,人们就知道珊瑚骨骼是由具有与分类学相关排列的文石晶体构成的,但每种珊瑚物种控制这种结晶过程的方式仍然是一个未解之谜。当研究表明珊瑚文石的同位素组成受到与分类学相关的影响(即“生命效应”)时,这个问题变得更加引人入胜。另一方面,珊瑚骨骼中有机成分的存在也早已为人所知,但这些化合物的定位仅限于特定结构,即所谓的“钙化中心”。纤维是珊瑚骨骼的主要组成部分,通常被认为是纯粹的矿物单元。本文表明,在“钙化中心”和纤维中,有机化合物在深层结构水平上与矿物质相关联。一系列不同尺度的观察和局部测量使得能够识别纳米尺度上有机成分的存在。因此,珊瑚纤维的结晶远非一个自由进行的过程,而是由珊瑚虫基部外胚层通过一个在微米尺度上起作用的循环两步过程永久控制。生物矿化循环始于蛋白聚糖基质的分泌。由于这些糖 - 蛋白组合的组成已被证明依赖于分类学,因此可以推测,珊瑚骨骼长期以来被认可的多种特异性与这种由生物化学驱动的结晶过程有关。此外,珊瑚骨骼生物矿化过程的这一新概念为我们了解石珊瑚目(Scleractinia)的长期进化提供了途径。值得注意的是,使用微观结构标准(即“钙化中心”的空间关系和纤维的三维排列)的基于骨骼的方法的结果与对同一物种进行的分子系统发育分析一致。显然,在整体个体发育水平上,珊瑚骨骼的两步生长模式也是重建石珊瑚目进化历史的一个有价值的工具。

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