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http://eprints.org/relation/isVersionOf https://researchdata.gla.ac.uk/id/document/519 http://eprints.org/relation/isVolatileVersionOf https://researchdata.gla.ac.uk/id/document/519 http://eprints.org/relation/isIndexCodesVersionOf https://researchdata.gla.ac.uk/id/document/519 525 1 3170 document 525 indexcodes.txt text/plain a87d12e447b513851fc1249e9606feca MD5 759 2016-01-22 14:17:31 https://researchdata.gla.ac.uk/259/10/indexcodes.txt 259 10 10 text/plain other Generate index codes conversion from Text to indexcodes en public

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http://eprints.org/relation/isVersionOf https://researchdata.gla.ac.uk/id/document/520 http://eprints.org/relation/isVolatileVersionOf https://researchdata.gla.ac.uk/id/document/520 http://eprints.org/relation/isIndexCodesVersionOf https://researchdata.gla.ac.uk/id/document/520 archive 5 disk0/00/00/02/59 2016-01-22 14:17:56 2026-01-12 09:14:54 2016-03-30 09:04:13 data_collection show Fitzer S.C. 16961 Chung Peter 10526 Maccherozzi Francesco Diamond Light Source Dhesi Sarnjeet S. Diamond Light Source Kamenos Nicholas 9996 0000-0003-3434-0807 Phoenix V.R. 12780 Cusack M 10363 glaresearchdata:2016-02-15-259 pub 30400000 The text files provide data for the XAS spectra in Figure 2 of the article 'Biomineral shell formation under ocean acidification: a shift from order to chaos' Scientific Reports | 6:21076 | DOI: 10.1038/srep21076. Figure 2: The XAS spectra across the Ca L2,3-edge of Mytilus edulis shell grown under present day conditions for (a) the outer calcite, (b) the interface calcite, (c) the interface aragonite and (d) inner aragonite area. The colour of the present day (380 μ atm pCO2) solid line corresponds to the area with the same colour circle in Fig. 1. The spectra for each region of the shell grown under OA (1000 μ atm pCO2) conditions are shown as the solid black line in each panel. The spectra have been overlaid to highlight the increased ACC presence in shells grown under OA in the areas determined to be calcite and aragonite by XPEEM and EBSD. The six features in the XAS spectra are labelled 1–6. The solid vertical line in (a) indicates the position of the lower energy shoulder indicative of ACC. The dashed vertical line in (a) indicates the position of the peak that increases intensity from the outer calcite to the inner aragonite layer. 2016-02-15 published University of Glasgow 10.5525/gla.researchdata.259 Text 45247 1 Understanding polymorph production and control in calcite/aragonite biominerals Andrew Freer Biotechnology and Biological Sciences Research Council (BBSRC) BB/E025110/1 CHEM - CHEMISTRY 56357 1 Biomineralisation - protein and mineral response to ocean acidification. Maggie Cusack Leverhulme Trust (LEVERHULME) RPG-042 SCHOOL OF GEOGRAPHICAL & EARTH SCIENCES FALSE Data was collected at the Diamond light source in May 2014. English http://dx.doi.org/10.1038/srep21076 article 2036-01-22 R 2026-01-12 AA Original retention date 2026-01-22. Extended to 10 years from date of last access. FALSE FALSE http://eprints.gla.ac.uk/id/eprint/115013