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dc.contributor.authorAgbaje, O. B. A.en
dc.contributor.authorBrock, G. A.en
dc.contributor.authorZhang, Z.en
dc.contributor.authorDuru, K. C.en
dc.contributor.authorLiang, Y.en
dc.contributor.authorGeorge, S. C.en
dc.contributor.authorHolmer, L. E.en
dc.date.accessioned2022-05-12T08:16:14Z-
dc.date.available2022-05-12T08:16:14Z-
dc.date.issued2021-
dc.identifier.citationBiomacromolecules in Recent Phosphate-Shelled Brachiopods: Identification and Characterization of Chitin Matrix / O. B. A. Agbaje, G. A. Brock, Z. Zhang et al. — DOI 10.21538/0134-4889-2020-26-4-290-299 // Journal of Materials Science. — 2021. — Vol. 56. — Iss. 36. — P. 19884-19898.en
dc.identifier.issn0022-2461-
dc.identifier.otherAll Open Access, Hybrid Gold, Green3
dc.identifier.urihttp://elar.urfu.ru/handle/10995/111324-
dc.description.abstractAbstract: Phosphate-shelled brachiopods differ in filter-feeding lifestyle, with Lingula anatina an active infaunal burrower, and Discinisca tenuis a shallow marine epibenthic animal. The shells of these animals are built of organophosphatic constituents, the organic fibres/sheets reinforced with calcium phosphate to provide a sophisticated ultrastructural robustness. This investigation examined the nature of the organic fibres in order to improve understanding of how living organisms produce hierarchically structured biomaterials. Unlike powdered samples commonly used in previous studies, organic fibres were isolated for the first time and the shell fractions were purified, in order to study the content and nature of the biopolymer fibres. Biochemical methods including Calcofluor staining revealed a chitin matrix. Ultrastructural analysis, thermal gravimetric analysis, and spectroscopic analyses show that the core polysaccharide framework is composed of layers of β-chitin sheets and/or fibrils that are coated with a fibrous organic matrix. There is more chitin matrix in the L. anatina shells (26.6 wt.%) compared to the D. tenuis shells (12.9 wt.%). Taken together, the data show that the chitin matrix contributes to increased skeletal strength, making L. anatina highly adapted for life as an active burrower. In comparison, D. tenuis contains less chitin and lives as attached epibenthos in a shallow marine environment. Graphical abstract: [Figure not available: see fulltext.] First spectroscopic evidence of β-chitin sheets in recent organophosphatic brachiopods. © 2021, The Author(s).en
dc.description.sponsorshipOBAA is grateful to Uppsala University for support through the VR Project number 2018-03390. The research for this paper was supported by the Swedish Research Council (VR Project no. 2018-03390 to LEH, GAB and SCG), by the National Natural Science Foundation of China (41720104002, 41621003 and 41890844 to NWU members), and by a Zhongjian Yang Scholarship to LEH from the Department of Geology, Northwest University, Xi’an. GAB’s research is also funded by a 1000 Talent Shaanxi Province Fellowship at Northwest University, Xi’an.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherSpringeren1
dc.publisherSpringer Science and Business Media LLCen
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceJ Mater Sci2
dc.sourceJournal of Materials Scienceen
dc.subjectANIMALSen
dc.subjectBIOPOLYMERSen
dc.subjectCALCIUM PHOSPHATEen
dc.subjectFIBERSen
dc.subjectGRAVIMETRIC ANALYSISen
dc.subjectSHELLS (STRUCTURES)en
dc.subjectSPECTROSCOPIC ANALYSISen
dc.subjectTHERMOGRAVIMETRIC ANALYSISen
dc.subjectBIOCHEMICAL METHODSen
dc.subjectBIOMACROMOLECULESen
dc.subjectFILTER-FEEDINGen
dc.subjectLIVING ORGANISMSen
dc.subjectPOWDERED SAMPLESen
dc.subjectSPECTROSCOPIC EVIDENCEen
dc.subjectTHERMAL GRAVIMETRIC ANALYSISen
dc.subjectULTRASTRUCTURAL ANALYSISen
dc.subjectCHITINen
dc.titleBiomacromolecules in Recent Phosphate-Shelled Brachiopods: Identification and Characterization of Chitin Matrixen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.rsi47064725-
dc.identifier.doi10.21538/0134-4889-2020-26-4-290-299-
dc.identifier.scopus85114853099-
local.contributor.employeeAgbaje, O.B.A., Department of Earth Sciences, Palaeobiology, Uppsala University, Uppsala, Sweden, Department of Earth and Environmental Sciences, Macquarie University, Sydney, Australia, Department of Biological Sciences, Macquarie University, Sydney, Australia, Globe Institute, Section for GeoGenetics, Faculty of Health and Medical Sciences, Copenhagen University, København, Denmark; Brock, G.A., Department of Biological Sciences, Macquarie University, Sydney, Australia, State Key Laboratory of Continental Dynamics, Shaanxi Key Laboratory of Early Life and Environments, Department of Geology, Northwest University, Xi’an, 710069, China; Zhang, Z., State Key Laboratory of Continental Dynamics, Shaanxi Key Laboratory of Early Life and Environments, Department of Geology, Northwest University, Xi’an, 710069, China; Duru, K.C., Department of Technology for Organic Synthesis, Ural Federal University, Yekaterinburg, Russian Federation, Department of Biomedical Sciences, Macquarie University, Sydney, Australia; Liang, Y., State Key Laboratory of Continental Dynamics, Shaanxi Key Laboratory of Early Life and Environments, Department of Geology, Northwest University, Xi’an, 710069, China; George, S.C., Department of Earth and Environmental Sciences, Macquarie University, Sydney, Australia; Holmer, L.E., Department of Earth Sciences, Palaeobiology, Uppsala University, Uppsala, Sweden, State Key Laboratory of Continental Dynamics, Shaanxi Key Laboratory of Early Life and Environments, Department of Geology, Northwest University, Xi’an, 710069, Chinaen
local.description.firstpage19884-
local.description.lastpage19898-
local.issue36-
local.volume56-
dc.identifier.wos000695792900003-
local.contributor.departmentDepartment of Earth Sciences, Palaeobiology, Uppsala University, Uppsala, Sweden; Department of Earth and Environmental Sciences, Macquarie University, Sydney, Australia; Department of Biological Sciences, Macquarie University, Sydney, Australia; State Key Laboratory of Continental Dynamics, Shaanxi Key Laboratory of Early Life and Environments, Department of Geology, Northwest University, Xi’an, 710069, China; Department of Technology for Organic Synthesis, Ural Federal University, Yekaterinburg, Russian Federation; Department of Biomedical Sciences, Macquarie University, Sydney, Australia; Globe Institute, Section for GeoGenetics, Faculty of Health and Medical Sciences, Copenhagen University, København, Denmarken
local.identifier.pure29070303-
local.identifier.eid2-s2.0-85114853099-
local.identifier.wosWOS:000695792900003-
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