Preprints
https://doi.org/10.5194/egusphere-2024-217
https://doi.org/10.5194/egusphere-2024-217
01 Feb 2024
 | 01 Feb 2024

Reply to Comment on Franz et al. (2023): A reinterpretation of the 1.5 billion year old Volyn ‘biota’ of Ukraine, and discussion of the evolution of the eukaryotes, by Head et al. (2023)

Gerhard Franz, Vladimir Khomenko, Peter Lyckberg, Vsevolod Chornousenko, and Ulrich Struck

Abstract. Head et al. (2023) emphasize the importance of the Volyn biota for the evolution, especially in the so-called ‘boring billion’, in a detailed outline about the biological and geological context. However, they question that the Volyn biota represent Precambrian fossils and instead argue that they are young contaminants of ‘museum dust’. In addition, they postulate that they are of abiotic origin. We present here a detailed discussion of their points of concern based on presented data, including some additional information. Their points of concern were:

  • One object, shown by Franz et al. (2023) is similar to a pollen grain, another object is similar to trichomes; we show indications for fossilization and summarize our arguments against ‘museum dust’.
  • They question the fossil character of the biota and argue for a biomineralization; we show that the biomineralization in trichomes is distinct from the mineralization of the biota.
  • They missed information about the internal structure; we repeat the presented information about the internal structure in more detail, which is also indicative of fossil material and inconsistent with trichomes.
  • They argue that we did not compare via infrared spectroscopy the biota with recent fungi; since the biota experienced temperatures near 300 °C, we think that a comparison with thermally degraded chitosan is more appropriate.
  • They question the use of strongly negative δ13C as an argument for biotic origin, but we show that in combination with positive δ15N values and the geological situation, a biotic origin is more likely than abiotic synthesis.

In addition, Popov (2023) questioned the age of the Volyn biota, which we postulated as between approximately 1.5 and 1.7 Ga. He argues that the fossils could be Phanerozoic. We will also outline our arguments for the minimum age of 1.5 Ga.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Gerhard Franz, Vladimir Khomenko, Peter Lyckberg, Vsevolod Chornousenko, and Ulrich Struck

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-217', Anonymous Referee #1, 14 Mar 2024
  • RC2: 'Comment on egusphere-2024-217', Anonymous Referee #2, 03 Jun 2024
Gerhard Franz, Vladimir Khomenko, Peter Lyckberg, Vsevolod Chornousenko, and Ulrich Struck
Gerhard Franz, Vladimir Khomenko, Peter Lyckberg, Vsevolod Chornousenko, and Ulrich Struck

Viewed

Total article views: 294 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
235 45 14 294 7 7
  • HTML: 235
  • PDF: 45
  • XML: 14
  • Total: 294
  • BibTeX: 7
  • EndNote: 7
Views and downloads (calculated since 01 Feb 2024)
Cumulative views and downloads (calculated since 01 Feb 2024)

Viewed (geographical distribution)

Total article views: 300 (including HTML, PDF, and XML) Thereof 300 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 15 Jun 2024
Short summary
The Volyn biota (Ukraine), previously assumed to be an extreme case of natural, abiotic synthesis of organic matter, is more likely a diverse assemblage of fossils from the deep biosphere. Although contamination by modern organisms cannot completely be ruled out, it is unlikely, considering all aspects, i. e. their mode of occurrence in the deep biosphere, their fossilization and mature state of organic matter, their isotope signature, and their large morphological diversity.