[Palaeontology, Vol. 52, Part 3, 2009, pp. 561–567] AN ORDOVICIAN LOBOPODIAN FROM THE SOOM SHALE LAGERSTA¨ TTE, SOUTH AFRICA by ROWAN J. WHITTLE*,à, SARAH E. GABBOTT*, RICHARD J. ALDRIDGE* and JOHANNES THERON *Department of Geology, University of Leicester, Leicester LE1 7RH, UK; e-mails:
[email protected];
[email protected] Department of Geology, University of Stellenbosch, Private Bag XI, Stellenbosch 7602, South Africa; e-mail:
[email protected] àPresent address: British Antarctic Survey, Madingley Road, Cambridge, CB3 0ET, UK; e-mail:
[email protected] Typescript received 18 July 2008; accepted in revised form 27 January 2009 Abstract: The first lobopodian known from the Ordovician and Carboniferous. The new fossil preserves an annulated is described from the Soom Shale Lagersta¨tte, South Africa. trunk, lobopods with clear annulations, and curved claws. It The organism shows features homologous to Palaeozoic mar- represents a rare record of a benthic organism from the ine lobopodians described from the Middle Cambrian Bur- Soom Shale, and demonstrates intermittent water oxygena- gess Shale, the Lower Cambrian Chengjiang biota, the Lower tion during the deposition of the unit. Cambrian Sirius Passet Lagersta¨tte and the Lower Cambrian of the Baltic. The discovery provides a link between marine Key words: Lagersta¨tte, lobopodian, Ordovician, Soom Cambrian lobopodians and younger forms from the Silurian Shale. Cambrian lobopodians are a diverse group showing a in an intracratonic basin with water depths of approxi- great variety of body shape, size and ornamentation. mately 100 m (Gabbott 1999). Dominantly quiet water However, they share a segmented onychophoran-like conditions are indicated by a lack of flow-induced sedi- body, paired soft-skinned annulated lobopods, and in mentary structures and the taphonomy of the fossils.