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有机磷酸腕足动物贝壳的表征:胶原蛋白基质和生物矿物成分的光谱评估

Characterization of organophosphatic brachiopod shells: spectroscopic assessment of collagen matrix and biomineral components.

作者信息

Agbaje Oluwatoosin B A, George Simon C, Zhang Zhifei, Brock Glenn A, Holmer Lars E

机构信息

Department of Earth Sciences, Palaeobiology, Uppsala University Uppsala Sweden

Department of Earth and Environmental Sciences and MQ Marine Research Centre, Macquarie University Sydney Australia.

出版信息

RSC Adv. 2020 Oct 20;10(63):38456-38467. doi: 10.1039/d0ra07523j. eCollection 2020 Oct 15.

Abstract

The shells of linguloid brachiopods such as and are inorganic-organic nanocomposites with a mineral phase of calcium phosphate (Ca-phosphate). Collagen, the main extracellular matrix in Ca-phosphatic vertebrate skeletons, has not previously been clearly resolved at the molecular level in organophosphatic brachiopods. Here, modern and recently-alive linguliform brachiopod shells of and have been studied by microRaman spectroscopy, Fourier transform infrared spectroscopy, field emission gun scanning electron microscopy, and thermal gravimetric analysis. For the first time, biomineralized collagen matrix and Ca-phosphate components were simultaneously identified, showing that the collagen matrix is an important moiety in organophosphatic brachiopod shells, in addition to prevalent chitin. Stabilized nanosized apatitic biominerals (up to ∼50 nm) permeate the framework of organic fibrils. There is a ∼2.5-fold higher wt% of carbonate (CO ) in shells. Both microRaman spectroscopy and infrared spectra show transient amorphous Ca-phosphate and octacalcium phosphate components. For the first time, trivalent moieties at ∼1660 cm and divalent moieties at ∼1690 cm in the amide I spectral region were identified. These are related to collagen cross-links that are abundant in mineralized tissues, and could be important features in the biostructural and mechanical properties of Ca-phosphate shell biominerals. This work provides a critical new understanding of organophosphatic brachiopod shells, which are some of the earliest examples of biomineralization in still-living animals that appeared in the Cambrian radiation.

摘要

舌形腕足动物如 和 的外壳是无机 - 有机纳米复合材料,其矿物相为磷酸钙(钙磷酸盐)。胶原蛋白是钙磷酸盐脊椎动物骨骼中的主要细胞外基质,此前在有机磷酸盐腕足动物中尚未在分子水平上得到清晰解析。在这里,通过显微拉曼光谱、傅里叶变换红外光谱、场发射枪扫描电子显微镜和热重分析对现代和近期存活的 和 的舌形腕足动物外壳进行了研究。首次同时鉴定出生物矿化的胶原蛋白基质和磷酸钙成分,表明除了普遍存在的几丁质外,胶原蛋白基质是有机磷酸盐腕足动物外壳中的重要组成部分。稳定的纳米级磷灰石生物矿物(最大约50纳米)渗透到有机纤维的框架中。 外壳中的碳酸盐(CO )重量百分比高约2.5倍。显微拉曼光谱和红外光谱均显示出瞬态无定形磷酸钙和八钙磷酸盐成分。首次在酰胺I光谱区域中鉴定出约1660厘米处的三价部分和约1690厘米处的二价部分。这些与矿化组织中丰富的胶原蛋白交联有关,并且可能是磷酸钙外壳生物矿物的生物结构和力学性能的重要特征。这项工作为有机磷酸盐腕足动物外壳提供了至关重要的新认识,这些外壳是寒武纪辐射中出现的现存动物中最早的生物矿化实例之一。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6470/9057340/7fe96e319096/d0ra07523j-f1.jpg

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