Articles | Volume 12, issue 8
Biogeosciences, 12, 2301–2309, 2015
Biogeosciences, 12, 2301–2309, 2015

Research article 16 Apr 2015

Research article | 16 Apr 2015

Fossilized bioelectric wire – the trace fossil Trichichnus

M. Kędzierski1, A. Uchman1, Z. Sawlowicz1, and A. Briguglio2,3 M. Kędzierski et al.
  • 1Institute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063 Kraków, Poland
  • 2Institut für Paläontologie, Universität Wien, Geozentrum, Althanstrasse 14, 1090 Vienna, Austria
  • 3Faculty of Science, Department of Petroleum Geoscience, Universiti Brunei Darussalam, Jalan Tungku Link, Gadong BE1410, Brunei

Abstract. The trace fossil Trichichnus is proposed as an indicator of fossil bioelectric bacterial activity at the oxic–anoxic interface zone of marine sediments. This fulfils the idea that such processes, commonly found in the modern realm, should be also present in the geological past. Trichichnus is an exceptional trace fossil due to its very thin diameter (mostly less than 1 mm) and common pyritic filling. It is ubiquitous in some fine-grained sediments, where it has been interpreted as a burrow formed deeper than any other trace fossils, below the redox boundary. Trichichnus, formerly referred to as deeply burrowed invertebrates, has been found as remnant of a fossilized intrasediment bacterial mat that is pyritized. As visualized in 3-D by means of X-ray computed microtomography scanner, Trichichnus forms dense filamentous fabric, which reflects that it is produced by modern large, mat-forming, sulfide-oxidizing bacteria, belonging mostly to Thioploca-related taxa, which are able to house a complex bacterial consortium. Several stages of Trichichnus formation, including filamentous, bacterial mat and its pyritization, are proposed to explain an electron exchange between oxic and suboxic/anoxic layers in the sediment. Therefore, Trichichnus can be considered a fossilized "electric wire".

Final-revised paper