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碳酸酐酶:钙质海绵生物矿化中的古老工具。

Carbonic Anhydrases: An Ancient Tool in Calcareous Sponge Biomineralization.

作者信息

Voigt Oliver, Fradusco Benedetta, Gut Carolin, Kevrekidis Charalampos, Vargas Sergio, Wörheide Gert

机构信息

Department of Earth and Environmental Sciences, Palaeontology and Geobiology, Ludwig-Maximilians-Universität München, Munich, Germany.

GeoBio-Center, Ludwig-Maximilians-Universität München, Munich, Germany.

出版信息

Front Genet. 2021 Apr 7;12:624533. doi: 10.3389/fgene.2021.624533. eCollection 2021.

Abstract

Enzymes of the α-carbonic anhydrase gene family (CAs) are essential for the deposition of calcium carbonate biominerals. In calcareous sponges (phylum Porifera, class Calcarea), specific CAs are involved in the formation of calcite spicules, a unique trait and synapomorphy of this class. However, detailed studies on the CA repertoire of calcareous sponges exist for only two species of one of the two Calcarea subclasses, the Calcaronea. The CA repertoire of the second subclass, the Calcinea, has not been investigated so far, leaving a considerable gap in our knowledge about this gene family in Calcarea. Here, using transcriptomic analysis, phylogenetics, and hybridization, we study the CA repertoire of four additional species of calcareous sponges, including three from the previously unsampled subclass Calcinea. Our data indicate that the last common ancestor of Calcarea had four ancestral CAs with defined subcellular localizations and functions (mitochondrial/cytosolic, membrane-bound, and secreted non-catalytic). The evolution of membrane-bound and secreted CAs involved gene duplications and losses, whereas mitochondrial/cytosolic and non-catalytic CAs are evidently orthologous genes. Mitochondrial/cytosolic CAs are biomineralization-specific genes recruited for biomineralization in the last common ancestor of calcareous sponges. The spatial-temporal expression of these CAs differs between species, which may reflect differences between subclasses or be related to the secondary thickening of spicules during biomineralization that does not occur in all species. With this study, we extend the understanding of the role and the evolution of a key biomineralization gene in calcareous sponges.

摘要

α-碳酸酐酶基因家族(CAs)的酶对于碳酸钙生物矿物的沉积至关重要。在钙质海绵(多孔动物门,钙质海绵纲)中,特定的CAs参与方解石骨针的形成,这是该纲的一个独特特征和共有衍征。然而,关于钙质海绵CAs库的详细研究仅存在于钙质海绵纲两个亚纲之一的钙质海绵亚纲中的两个物种。另一个亚纲,石灰海绵亚纲的CAs库迄今尚未得到研究,这使得我们对钙质海绵纲中这个基因家族的了解存在相当大的空白。在这里,我们使用转录组分析、系统发育分析和杂交技术,研究了另外四种钙质海绵的CAs库,其中包括来自之前未采样的石灰海绵亚纲的三个物种。我们的数据表明,钙质海绵纲的最后一个共同祖先有四个具有明确亚细胞定位和功能的祖先CAs(线粒体/胞质、膜结合和分泌型非催化)。膜结合和分泌型CAs的进化涉及基因重复和丢失,而线粒体/胞质和非催化CAs显然是直系同源基因。线粒体/胞质CAs是在钙质海绵的最后一个共同祖先中被招募用于生物矿化的生物矿化特异性基因。这些CAs的时空表达在不同物种之间存在差异,这可能反映了亚纲之间的差异,或者与并非所有物种都发生的生物矿化过程中骨针的二次增厚有关。通过这项研究,我们扩展了对钙质海绵中关键生物矿化基因的作用和进化的理解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/08bb/8058475/a530ac9c20c3/fgene-12-624533-g001.jpg

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