Fourier transform infrared characterization of the Middle Devonian non‐vascular plant Spongiophyton

59 3 May 365 386 10.1111/pala.12230

MATSUMURA, W.M.K., BALZARETTI, N.M., IANNUZZI, R. 2016. Fourier transform infrared characterization of the Middle Devonian non‐vascular plant Spongiophyton. Palaeontology, 59, 3, 365-386. DOI: 10.1111/pala.12230

Willian M. K. Matsumura, Naira M. Balzaretti, and Roberto Iannuzzi
  • Willian M. K. Matsumura - Universidade Federal do Rio Grande do Sul Instituto de Geociências Porto Alegre RS Brazil (Email: williammatsumura@gmail.com)
  • Naira M. Balzaretti - Universidade Federal do Rio Grande do Sul Instituto de Física Porto Alegre RS Brazil (Email: naira@if.ufrgs.br)
  • Roberto Iannuzzi - Universidade Federal do Rio Grande do Sul Instituto de Geociências Porto Alegre RS Brazil (Email: roberto.iannuzzi@ufrgs.br)
  • Issue published online: 19 April 2016
  • Article first published online: 01 January 1970
  • Manuscript Accepted: 18 December 2015
  • Manuscript Received: 25 April 2015
National Council of Technological and Scientific Development. Grant Numbers: 141979/2011‐9, PQ 300801/2012‐2, PQ 309211/2013‐1, 401796/2010‐8, 479774/2011‐0

Spectroscopy information (functional groups and semiquantitative data) by Fourier transform infrared (FTIR) spectroscopy of Spongiophyton Kräusel emend. Chaloner et al. is reported for the first time, in an attempt to identify spectroscopic patterns that would differentiate species of these taxa. A total of 33 specimens identified as S. lenticularis, S. nanum and S. minutissimum and preserved as compressions were analysed. They come from the same fossiliferous horizon of one outcrop situated in the uppermost Middle Devonian São Domingos Formation of the Paraná Basin in southern Brazil. The results reveal that functional groups in the 3000–2800 and 1800–700 cm−1 wavenumber regions are present in all specimens. Infrared‐derived ratios (CH2/CH3, Al/Ox, Ox1/Ox2, C=O cont., C=C cont., Al2 and Ar/Al) and types of kerogen led to a comparison of the morphological characteristics of the studied material and indicate that compressions of S. lenticularis, S. nanum and S. minutissimum contain different organic compounds. S. nanum and S. minutissimum show higher oxidation and lower aromaticity of its organic matter than S. lenticularis. Additionally, S. lenticularis shows low A‐factor values, suggesting a composition similar to type III kerogen, while S. nanum and S. minutissimum showed intermediate to high A‐factor values, suggesting a composition similar to type II kerogen. In conclusion, the chemical‐analytical techniques and statistical analysis (using PCA technique) reveal a closer taxonomic relationship between S. nanum and S. minutissimum than either has with S. lenticularis, supporting their taxonomic separation, previously proposed in the literature on the basis of morphological features. Lastly, the chemical signatures support the hypothesis that links these enigmatic fossils to a type of lichen or other early inland plant.

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