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XRD study of the Permian fossil bone tissue

Published online by Cambridge University Press:  15 March 2019

A. D. Ryanskaya
Affiliation:
Institute of Geology and Geochemistry, Ural Branch of Russian Academy of Sciences, Ekaterinburg, Russian Federation
D. V. Kiseleva*
Affiliation:
Institute of Geology and Geochemistry, Ural Branch of Russian Academy of Sciences, Ekaterinburg, Russian Federation
O. P. Shilovsky
Affiliation:
Kazan Federal University, Kazan, Russian Federation Natural History Museum of Tatarstan, Kazan, Russian Federation
E. S. Shagalov
Affiliation:
Institute of Geology and Geochemistry, Ural Branch of Russian Academy of Sciences, Ekaterinburg, Russian Federation
*
a)Author to whom correspondence should be addressed. Electronic mail: podarenka@mail.ru

Abstract

This paper is devoted to the X-ray diffraction study of bone fragments of Permian parareptile Deltavjatia vjatkensis obtained from the Kotelnich vertebrate fossil site, one of the richest of the Permian period, which is characterized by the excellent preservation of fossil remains because of their burial in a silty anaerobic environment similar to modern bogs. The bone is well-preserved and consists of fluorapatite, calcite, quartz, and dolomite. The refined apatite unit-cell parameters of a and b-axis (9.3526 ± 0.0001 and 9.3587 ± 0.0001) Å and c-axis (6.8930 ± 0.0001 and 6.8968 ± 0.0001) Å correspond to F-apatite. Crystallinity index determined as the full width at half maximum of the 002 reflection in degrees 2θ is 0.266–0.250, which is typical for Mesozoic vertebrate bones. Apatite crystallite size (length 70.3–74.9 nm, width 30.7–30.3 nm) in fossil pareiasaur bone is larger than in subfossil and recent mammal bone and is in a good agreement with the values for seismosaurus bone. Both crystallite size and aspect ratio (2.3–2.5) are independent of the fossil pareiasaur bone length.

Type
Technical Articles
Copyright
Copyright © International Centre for Diffraction Data 2019 

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References

Chipera, S. J. and Bish, D. L. (1990). “Applications of X-ray diffraction crystallite size/strain analysis to Seismosaurus dinosaur bone,” Adv. X-Ray Anal. 34, 473482.Google Scholar
Dumont, M., Kostka, A., Sander, P. M., Borbely, A., and Kaysser-Pyzalla, A. (2011). “Size and size distribution of apatite crystals in sauropod fossil bones,” Palaeogeogr. Palaeoclimatol. Palaeoecol. 310, 108116.Google Scholar
Elorza, J., Astibia, H., Murelaga, X., and Pereda-Suberbiola, X. (1999). “Francolite as a diagenetic mineral in dinosaur and other Upper Cretaceous reptile bones (Lano, Iberian Peninsula): microstructural, petrological and geochemical features,” Cretaceous Res. 20, 169187.Google Scholar
Gillette, D. D. (1991). “Seismosaurus halli, gen. et sp. nov., a new sauropod dinosaur from the Morrison formation (Upper Jurassic/Lower Cretaceuos) of New Mexico, USA,” J. Vert. Paleontol., 11 (4), 417433.Google Scholar
ICDD (2008). PDF-2+ 2008 (Database), International Centre for Diffraction Data, Newtown Square, PA, USA.Google Scholar
Ivakhnenko, M. F. (2001). “Tetrapody Vostochno-Evropeyskogo plakkata – pozdnepaleozoyskogo territorialno-prirodnogo kompleksa,” Paleontol. inst. RAN, Moskva. [Ivakhnenko, M.F. (2001). “Tetrapods of the East European plakkat – the late Paleozoic territorial-natural complex,” Paleontol. inst. RAS, Moscow. (in Russ.)].Google Scholar
Kowal-Linka, M., Jochum, K. P., and Surmik, D. (2014). “LA-ICP-MS analysis of rare earth elements in marine reptile bones from the Middle Triassic bonebed (Upper Silesia, S Poland): impact of long-lasting diagenesis, and factors controlling the uptake,” Chem. Geol. 363, 213228.Google Scholar
Landis, W. J. (1995). “The strength of a calcified tissue depends in part on the molecular structure and organization of its constituents mineral crystals in their organic matrix,” Bone 16, 533544.Google Scholar
Majid, C. A. and Hussain, M. A. (1996). “Refinement of structure of polycrystalline fluorapatite,” Proc. Pak. Acad. Sci. 33(1–2), 1117.Google Scholar
Piga, G., Santos-Cubedo, A., Brunetti, A., Piccinini, M., Malgosa, A., Napolitano, E., and Enzo, S. (2011). “A multi-technique approach by XRD, XRF, FT-IR to characterize the diagenesis of dinosaur bones from Spain,” Palaeogeogr. Palaeoclimatol. Palaeoecol. 310, 92107.Google Scholar
Plet, C., Grice, K., Pagès, A., Verrall, M., Coolen, M. J. L., Ruebsam, W., Rickard, W. D. A, and Schwark, L. (2017). “Palaeobiology of red and white blood cell-like structures, collagen and cholesterol in an ichthyosaur bone,” Nat. Sci. Rep. 7, 13776.Google Scholar
Rietveld, H. M. (1967). “Line profiles of neutron powder-diffraction peaks for structure refinement,” Acta Crystallogr. 22, 151152.Google Scholar
Silaev, V. I., Ponomarev, D. V., Kiseleva, D. V., Smoleva, I. V., Simakova, Yu, S., Martirosyan, O. V., Vasil'ev, E. A., Khazov, A. F., and Tropnikov, E. M. (2017). “Mineralogical–geochemical characteristics of the bone detritus of Pleistocene mammals as a source of paleontological information,” Paleontol. J. 51, 13951421.Google Scholar
Stathopoulou, E. T., Psycharis, V., Chryssikos, G. D., Gionis, V., and Theodorou, G. (2008). “Bone diagenesis: new data from infrared spectroscopy and X-ray diffraction,” Palaeogeogr. Palaeoclimatol. Palaeoecol. 266, 168174.Google Scholar
Taylor, J. C. (2004). Rietveld Made Easy: A Practical Guide to the Understanding of the Method and Successful Phase Quantifications (Sietronics Pty Limited, Canberra).Google Scholar
Trueman, C. N. G., Behrensmeyer, A. K., Tuross, N., and Weiner, S. (2004). “Mineralogical and compositional changes in bones exposed on soil surfaces in Amboseli National Park, Kenya: diagenetic mechanisms and the role of sediment pore fluids,” J. Archaeol. Sci. 31, 721739.Google Scholar