Abstract
Modern and fossil populations of a Stephanodiscus Ehrenberg species from June Lake, California (USA) were analysed using light and scanning electron microscopy (SEM). Stephanodiscus valves were a major constituent of almost all analysed samples, often dominating fossil assemblages dating back several thousand years. The most commonly observed Stephanodiscus specimen in the samples bore a striking resemblance to the extinct Late Pliocene species Stephanodiscus klamathensis, particularly under light microscopy. The population size range, ultrastructure, and other defining characteristics closely matched published information on S. klamathensis. However, under SEM, internal views of the specimens from June Lake showed an important difference; specimens lacked valve face fultoportulae, whereas S. klamathensis is characterized by the presence of two valve face fultoportulae, each with three satellite pores near the centre of the valve. Additional differences in valve size range, absence of fultoportulae on the valve face, and the fact that S. klamathensis is an extinct species (observed in diatomites deposited from Late Pliocene to Pleistocene) with no closely related living relatives, necessitates describing this Stephanodiscus as a new species. To date, Stephanodiscus coruscus has been observed only in June Lake, California; most Stephanodiscus that share strong morphological similarities to this species have only been observed in ancient fossil diatomites. Thus, Stephanodiscus coruscus Jeff. R. Stone, Edlund & Streib sp. nov. is not only a new species but also provides a rare glimpse into the likely types of environments that S. klamathensis and other similar ancient Stephanodiscus may have inhabited in the late Pliocene. Character variations between S. coruscus and S. klamathensis reveal potential patterns of evolution in freshwater lineages, such as character loss, over time.
Acknowledgments
The authors would like to thank Helena Bierly for assistance with sample processing and slide preparation. The authors also thank Anna Nesterovich for assistance with translations and Matthew Julius (St. Cloud State University) for discussions on Stephanodiscus phylogeny. Research at June Lake was conducted under permits granted by the U.S. Department of Agriculture-Inyo National Forest (LVD 16026). Financial support for fieldwork was provided by the Overcash Field Research Fund and the Pioneer Endowment at the University of Kentucky (UK). The authors are grateful to Ed Woolery, Eva Lyon, Joseph Lucas, numerous UK students, and the staff of the June Lake Marina for assistance with sampling in the field. Cores were sampled and are archived at LacCore (National Lacustrine Core Facility), University of Minnesota-Twin Cities.
Disclosure statement
No potential conflict of interest was reported by the authors.