Chapligin B., Leng M. J., Webb E., Alexandre A., Dodd J. P., Ijiri A., Lucke A., Shemesh A., Abelmann A., Herzschuh U., Longstaffe F. J., Meyer H., Moschen R., Okazaki Y., Rees N. H., Sharp Z. D., Sloane H. J., Sonzogni C., Swann G. E. A., Sylvestre Florence, Tyler J. J., Yam R. (2011). Inter-laboratory comparison of oxygen isotope compositions from biogenic silica. Geochimica et Cosmochimica Acta, 75 (22), p. 7242-7256. ISSN 0016-7037.
Titre du document
Inter-laboratory comparison of oxygen isotope compositions from biogenic silica
Année de publication
2011
Auteurs
Chapligin B., Leng M. J., Webb E., Alexandre A., Dodd J. P., Ijiri A., Lucke A., Shemesh A., Abelmann A., Herzschuh U., Longstaffe F. J., Meyer H., Moschen R., Okazaki Y., Rees N. H., Sharp Z. D., Sloane H. J., Sonzogni C., Swann G. E. A., Sylvestre Florence, Tyler J. J., Yam R.
Source
Geochimica et Cosmochimica Acta, 2011,
75 (22), p. 7242-7256 ISSN 0016-7037
Several techniques have been introduced in the last decades for the dehydration and release of O-2 from biogenic silica (opal-A) for oxygen-isotope analysis. However, only one silica standard is universally available: a quartz standard (NBS28) distributed by the IAEA, Vienna. Hence, there is a need for biogenic silica working standards. This paper compares the existing methods of oxygen-isotope analyses of opal-A and aims to characterize additional possible working standards to calibrate the delta O-18 values of biogenic silica. For this purpose, an inter-laboratory comparison was organized. Six potential working standard materials were analysed repeatedly against NBS28 by eight participating laboratories using their specific analytical methods. The materials cover a wide range of delta O-18 values (+23 to +43 parts per thousand) and include diatoms (marine, lacustrine), phytoliths and synthetically-produced hydrous silica. To characterize the proposed standards, chemical analyses and imaging by scanning electron microscopy (SEM) were also performed. Despite procedural differences at each laboratory, all methods are in reasonable agreement with a standard deviation (SD) for delta O-18 values between 0.3 parts per thousand and 0.9 parts per thousand (1 sigma). Based on the results, we propose four additional biogenic silica working standards (PS1772-8: 42.8 parts per thousand; BFC: 29.0 parts per thousand; MSG60: 37.0 parts per thousand; G95-25-CL leaves: 36.6 parts per thousand) for delta O-18 analyses, available on request through the relevant laboratories.
Plan de classement
Géologie et formations superficielles [064]
Localisation
Fonds IRD [F B010054158]
Identifiant IRD
fdi:010054158
