Aulacoseira chockii sp. nov., an early freshwater centric diatom from the Eocene bearing a unique morphology

Abstract

Aulacoseira is a freshwater diatom genus found today in numerous lakes, ponds and rivers worldwide, and inhabiting a wide range of environmental conditions. The genus is one of the oldest diatom lineages known to colonize freshwater environments, dating to the late Cretaceous and radiating over much of the Cenozoic. The purpose of this paper is to describe a new species, Aulacoseira chockii, from an early Eocene locality situated near the Arctic Circle in northern Canada. The exquisitely preserved specimens have allowed for a detailed examination of frustule morphology of this early Cenozoic taxon. Three characteristics clearly separate A. chockii from all other known fossil and modern species in the genus. First, the spines of A. chockii are formed by coalescence of extensions from three to five mantle costae and multiple ribs that originate on the valve face. This type of spine design has never been reported and represents a potentially ancient trait in the Aulacoseiraceae lineage. Second, the valve has multiple sessile rimoportulae that are each connected to the end of a tube or canal that runs parallel to, and inside, the mantle wall. Rimoportulae with this structure are rare, and found primarily on extinct species of Aulacoseira. Third, the mantle striae are sinistrorse, and represent another rarely observed character within the genus. Because frustules of A. chockii possessed only separation spines, existed largely as single cells and not in long filaments, and were found in associated with remains of numerous heliozoans as well as testate euglyphids and sponges, it is believed this species grew in the littoral zone of a shallow waterbody.

Keywords:

• Aulacoseira
• Cenozoic
• Eocene
• Eoseira
• freshwater fossil diatoms
• Giraffe Pipe locality
• rimoportulae
• sinistrorse

Acknowledgements

I thank Anne Marie Lizzaralde for help with sample preparation, and Xuanhao Sun from the Bioscience Electron Microscopy Laboratory (BEML) at the University of Connecticut for help with SEM facilities.

Disclosure statement

No potential conflict of interest was reported by the author(s).

Additional information

Funding

This project was funded, in part, with grants to PAS from the National Science Foundation (NSF) (EAR-1725265 and EAR-1940070).