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dc.contributor.authorSzabo, Reka
dc.contributor.authorCalder, Angus
dc.contributor.authorFerrier, David Ellard Keith
dc.date.accessioned2015-09-13T23:10:48Z
dc.date.available2015-09-13T23:10:48Z
dc.date.issued2014-11
dc.identifier.citationSzabo , R , Calder , A & Ferrier , D E K 2014 , ' Biomineralisation during operculum regeneration in the polychaete Spirobranchus lamarcki ' , Marine Biology , vol. 161 , no. 11 , pp. 2621-2629 . https://doi.org/10.1007/s00227-014-2534-3en
dc.identifier.issn0025-3162
dc.identifier.otherPURE: 154023912
dc.identifier.otherPURE UUID: 2cc2158d-4984-4947-b019-df95521a1216
dc.identifier.otherScopus: 84919683935
dc.identifier.otherORCID: /0000-0003-3247-6233/work/36423818
dc.identifier.otherWOS: 000343919800014
dc.identifier.urihttp://hdl.handle.net/10023/7455
dc.descriptionRS was supported by a Carnegie Scholarship.en
dc.description.abstractFormation of calcified biominerals is widespread in marine animals and is often associated with important elements of their biology, such as support and protection. Serpulid polychaetes are relatively understudied examples of biomineralisation despite their prominence in many marine ecosystems. An investigation of calcification in the regenerating opercular plate of the serpulid polychaete Spirobranchus (formerly Pomatoceros) lamarcki was performed using optical microscopy, calcein labelling and powder diffraction analysis. Worms were collected between January 2012 and June 2013 from East Sands beach, St Andrews, Scotland (56.33° N, 2.78° W). The earliest visible signs of calcification were birefringent grains. Later-stage regenerates displayed a complex mixture of calcified structures including grains, round, smooth tiles, and larger tiles with a rugged appearance. The plate matures by the growth and eventual merging of tiles into a contiguous crust. Calcein pulse-chase experiments showed the progression of calcification from the centre towards the edge of the plate, and powder diffraction analysis of three regenerative stages revealed a major shift in mineralogy from a predominantly calcitic to a predominantly aragonitic composition. The mechanisms underlying the shift are currently unknown. These are the first mineralogical data comparing different developmental stages in a serpulid operculum, and contribute to the understanding of biomineralisation in this group.
dc.format.extent9
dc.language.isoeng
dc.relation.ispartofMarine Biologyen
dc.rights© 2014. Springer International Publishing AG, Part of Springer Science+Business Media. The final publication is available at Springer via http://dx.doi.org/10.1007/s00227-014-2534-3en
dc.subjectCalcificationen
dc.subjectSerpuliden
dc.subjectMagnesium calciteen
dc.subjectAragoniteen
dc.subjectX-ray diffractometryen
dc.subjectQH301 Biologyen
dc.subject.lccQH301en
dc.titleBiomineralisation during operculum regeneration in the polychaete Spirobranchus lamarckien
dc.typeJournal articleen
dc.description.versionPostprinten
dc.contributor.institutionUniversity of St Andrews.School of Biologyen
dc.contributor.institutionUniversity of St Andrews.Marine Alliance for Science & Technology Scotlanden
dc.contributor.institutionUniversity of St Andrews.Scottish Oceans Instituteen
dc.identifier.doihttps://doi.org/10.1007/s00227-014-2534-3
dc.description.statusPeer revieweden
dc.date.embargoedUntil2015-09-14


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