Ichnofossils

Palaeosabella Clarke, 1921

Taxon description

Buatois et al., 2017

Palaeosabella Clarke, 1921 is an elongated cylindrical boring with a swollen distal end formed in carbonate substrates. It is similar to Trypanites except for the clavate expansion at its termination. Palaeosabella has a complicated ichnotaxonomic history. It was considered nomen dubium by Teichert (1945), resurrected by Plewes (1996), Bromley (2004) and Wilson (2007), and erroneously considered a junior synonym of the later established Clionoides Fenton and Fenton, 1932 by Furlong and McRoberts (2014). We are here considering Palaeosabella a valid ichnotaxon because it does not branch like Clionoides.

Buatois et al., 2017

2.66. Clavate-shaped borings

Knaust, 2012a

Unbranched, cylindrical.

Wyse Jackson & Key, 2007

Palaeosabella is a clavate boring with length-to-width ratio of < 10:1, and although morphologically different from Trypanites, the two ichnogenera have often been confused.

Taylor & Wilson, 2003

Remark: Unbranched, cylindro-clavate borings.

Selection of related publications
Vinn, O., Wilson, M. A. 2010. Occurrence of Giant Borings of Osprioneides kampto in the Lower Silurian (Sheinwoodian) Stromatoporoids of Saaremaa, Estonia. Ichnos 17, 3, 166-171. DOI:10.1080/10420940.2010.502478
References based on distribution