Skip to main content
Log in

Combined Raman spectroscopic and Rietveld analyses as a useful and nondestructive approach to studying flint raw materials at prehistoric archaeological sites

  • Original Paper
  • Published:
Archaeological and Anthropological Sciences Aims and scope Submit manuscript

Abstract

A set of six lithic tools, unearthed along 2011 in two karst sites of the Guadalteba County (Málaga, Spain), has been nondestructively investigated by Raman spectroscopy and laboratory x-ray diffraction. From a chemist’s point of view, our goal is to develop a systematic screening protocol for a quick, easy, low cost and nondestructive characterization of archaeological flints based on Raman spectroscopy, x-ray diffraction and Rietveld refinement. In this paper, we firstly made use of Raman spectroscopy to determine, in a semiquantitative way, but with the generic advantage of a faster data acquisition than x-ray diffraction, the surface content of moganite of each lithic tool, from the ratio between the relative intensities of the two Raman-active symmetric stretching vibrations (A1 modes) of α-quartz (465 cm−1) and moganite (501 cm−1). The precise bulk quartz/moganite weight content was then accurately quantified by means of high-quality x-ray diffraction, followed by Rietveld refinement. We found a general good correlation between Raman and x-ray data. Nonetheless, as recently reported in the scientific literature by other authors, the vibrational spectroscopic quantification of moganite in silica rocks like flint and chert have to be performed very cautiously, to avoid undesired interferences from other Raman features due to the eventual presence of silanol (SiOH) groups, which could finally lead to an overestimation of the surface moganite concentration. As reported in such a recent article, a useful treatment to reduce the interference from silanol-bands is to heat the samples prior to their Raman analysis at a minimum of 600 ºC (but better at 700 or 800 ºC) for silanol “dehydration”. This, in our opinion, may be for sure a satisfactory procedure when studying flint or chert samples of a “geological origin”. But not of practical use when studying lithic tools which were manufactured by men thousands and thousands of years ago.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7

Similar content being viewed by others

References

  • Bustillo MA (2001) Aparición y significado de la moganita en las rocas de la sílice: una revisión. J Sediment Res 71:436–443

    Article  Google Scholar 

  • Bustillo MA, Pérez-Jiménez JL, Fort R (2007) Deterioro de Sílex en Canteras Históricas y Muestras Líticas. MACLA 7:18

    Google Scholar 

  • Bustillo MA, Pérez-Jiménez JL, Alonso-Zarza AM, Furio M (2012) Moganite in the Chalcedony varieties of continental cherts (Miocene, Madrid Basin, Spain). Spectrosc Lett 45:109–113

    Article  Google Scholar 

  • Carbonell E, Márquez B, Mosquera M, Olí A, Rodríguez XP, Sala R, Vergés JM (1999) “El Modo 2 en Galería. Análisis de la industria lítica y sus procesos técnicos” in Atapuerca: ocupaciones humanas y paleoecología del yacimiento de Galería, ed. Junta de Castilla y León, Consejería de Educación y Cultura, Valladolid, 1st edn., 390

  • Clark G (1998) World prehistory: in new perspective, 3rd edn. Cambridge University Press, New York, ISBN: 052129178X

    Google Scholar 

  • Flörke OW, Jones JB, Schmincke HU (1976) A new microcrystalline silica from Gran Canaria. Z Kristallogr 143:156–165

    Google Scholar 

  • Frondel C (1962) The system of mineralogy, vol. III: silica minerals. Wiley, New York

    Google Scholar 

  • Gliozzo E, Grassi N, Bonanni P, Meneghini C, Tomei MA (2011) Gemstones from Vigna Barberini at the Palatine Hill (Rome, Italy). Archaeometry 53:469–489

    Article  Google Scholar 

  • Götze J, Nasdala L, Kleeberg R, Wenzel RM (1998) Occurrence and distribution of “moganite” in agate/chalcedony: a combined micro-Raman, Rietveld and cathodoluminescence study. Contrib Mineral Petrol 133:96–105

    Article  Google Scholar 

  • Graetsch HA, Grünberg JM (2012) Microstructure of flint and other chert raw materials. Archaeometry 54:18–36

    Article  Google Scholar 

  • Gutiérrez Mas JM, Martín Algarra A, Domínguez-Bella S, Moral JP (1991), Introducción a la Geología de la provincia de Cádiz, Ed. University of Cádiz, ISBN: 978-84-7786-050-1

  • Heaney PJ (1995) Moganite as an indicator for vanished evaporites: a testament reborn? J Sediment Res A65:633–638

    Google Scholar 

  • Heaney PJ, Post JE (1992) The widespread distribution of a novel silica polymorph in microcrystalline quartz varieties. Science 255:441–443

    Article  Google Scholar 

  • Heaney PJ, Post JE (2001) Evidence for an I2/a to Imab phase transition in the silica polymorph moganite at 570 K. Am Mineral 86:1358–1366

    Google Scholar 

  • Hernández V, Jorge-Villar SE, Capel Ferrón C, Medianero FJ, Ramos J, Weniger GC, Domínguez-Bella S, Linstaedter J, Cantalejo P, Espejo M, Durán Valsero JJ (2012) Raman spectroscopy analysis of Palaeolithic industry from Guadalteba terrace river, Campillos (Guadalteba county Southern of Iberian Peninsula. J Raman Spec 43:1651–1657

    Article  Google Scholar 

  • Jambor JL, Burke EAJ, Grew ES, Puziewicz J (1993) New mineral names. Am Mineral 78:672–678

    Google Scholar 

  • Kingma KJ, Hemley RJ (1994) Raman spectroscopic study of microcrystalline silica. Am Mineral 79:269–273

    Google Scholar 

  • Laplace G (1975) La typologie analytique et structurale: Base rationnelle d’étude des industries lithiques et osseuses. Colloques Nationaux du Centre National de la Reserche Scientifique, Ed. CNRS, Marseille, 932: 91-141

  • Larson AC, Von Dreele RB (2000) General Structure Analysis System (GSAS), Los Alamos National Laboratory Report LAUR

  • Maslen EN, Streltsov VA, Streltsova NR, Ishizawa N (1995) Electron density and optical anisotropy in rhombohedral carbonates. III. Synchrotron X-ray studies of CaCO3, MgCO3 and MnCO3. Acta Cryst B51:929–939

    Article  Google Scholar 

  • Medianero FJ, Ramos J, Palmqvist P, Weniger GC, JRiquelme JA, Espejo M, Cantalejo P, Aranda A, Pérez-Claros JA, Figueirido B, Espigares P, Ros-Montoya S, Torregrosa V, Linstädter L, Cabello L, Becerra S, Ledesma P, Mevdev I, Castro A, Romero M, Martínez-Navarro B (2011) The karst site of Las Palomas (Guadalteba County, Málaga, Spain): a preliminary study of its Middle–Late Pleistocene archaeopaleontological record. Quatern Int 243:127–136

    Article  Google Scholar 

  • Olivares M, Tarriño A, Murelaga X, Baceta JI, Castro K, Etxebarria N (2009) Non-destructive spectrometry methods to study the distribution of archaeological and geological chert samples. Spectrochim Acta A 73:492–497

    Article  Google Scholar 

  • Pretola JP (2001) A feasibility study using silica polymorph ratios for sourcing chert and chalcedony lithic materials. J Archaeol Sci 28:721–739

    Article  Google Scholar 

  • Schmidt P, Bellot-Gurlet L, Slodczyk A, Fröhlich F (2012) A hitherto unrecognised band in the Raman spectra of silica rocks: influence of hydroxylated Si–O bonds (silanole) on the Raman moganite band in chalcedony and flint (SiO2). Phys Chem Minerals 39:455–464

    Article  Google Scholar 

  • Schmidt P, Bellot-Gurlet L, Léa V, Sciau P (2013) Moganite detection in silica rocks using Raman and infrared spectrocopy. Eur J Mineral 25(5):797–805

    Article  Google Scholar 

  • Tarriño A, Olivares M, Etxebarria N, Baceta JI, Larrasoaña JC, Yusta I, Pizarro JL, Cava A, Barandiarán I, Murelaga X (2007) El sílex de tipo “Urbasa” Caracterización petrológica y geoquímica de un marcador litológico en yacimientos arqueológicos del Suroeste europeo durante el Pleistoceno superior y Holoceno inicial. Geogaceta 43:127–130

    Google Scholar 

  • Thompson P, Cox DE, Hastings JB (1987) Rietveld refinement of Debye-Scherrer synchrotron X-ray data from Al2O3. J Appl Cryst 20:79–83

    Article  Google Scholar 

  • Vallespí E (1986), El Paleolítico inferior y medio en Andalucía in Homenaje a Luis Siret (1934–1984). Ed. Junta de Andalucía, Consejería de Cultura, pp. 59-66. ISBN: 84-505-3511-5

  • Vallespí E (1986), Cultura de las graveras y comienzos del Achelense Ibérico in Estudios en homenaje al Dr. Antonio Beltrán Martínez, Ed. University of Zaragoza, Zaragoza, pp. 147–157. ISBN: 84-600-4366-5

  • Vallespí E (1992) Las industrias Achelenses de Andalucía: Ordenación y Comentarios. SPAL 1:61–78

    Article  Google Scholar 

  • Will G, Bellotto M, Parrish W, Hart M (1988) Crystal structures of quartz and magnesium germanate by profile analysis of synchrotron-radiation high-resolution powder data. J Appl Cryst 21:182–191

    Article  Google Scholar 

Download references

Acknowledgments

Research at the Universities of Málaga and Cádiz was supported by Junta de Andalucía, through funding the FQM-159, FQM-113 and HUM-440 scientific groups. We also acknowledge the help by part of the students of the “Escuela Taller de Peñarrubia”, sponsored by the “Guadalteba County Consortium”, both in regards to the on-site works and the subsequent classification of the findings in the archaeology workroom. Financial and technical support from the Stiftung Neanderthal Museum is also acknowledged. We finally thank José Bello for providing us with moganite-rich samples from Mogán (Canary Islands, Spain).

Author information

Authors and Affiliations

Authors

Corresponding authors

Correspondence to S. Jorge-Villar or V. Hernández.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Capel Ferrón, C., León-Reina, L., Jorge-Villar, S. et al. Combined Raman spectroscopic and Rietveld analyses as a useful and nondestructive approach to studying flint raw materials at prehistoric archaeological sites. Archaeol Anthropol Sci 7, 235–243 (2015). https://doi.org/10.1007/s12520-014-0189-0

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s12520-014-0189-0

Keywords

Navigation