Towards understanding desert shorelines - coastal landforms and dynamics around ephemeral Lake Eyre North, South Australia

ABSTRACT

While shorelines around playa lakes have traditionally played a key role for reconstructing late Quaternary megalakes in drylands, little attention has been given to recent shorelines associated with episodic filling events of modern ephemeral playa lakes such as Kati Thanda-Lake Eyre in central Australia. We here present results from geomorphic mapping around the playa margin of Lake Eyre North and interpret these data regarding timescales and drivers of shoreline processes. The diversity and distribution of landforms point to lithology and variations in wave energies as major controls on large-scale shoreline geomorphology. Our results suggest that the presence or absence of shoreline features is an incomplete and inaccurate indicator of past lake levels. Instead, wave-built landforms in ephemeral playa lake settings need to be considered threshold-related phenomena, with differences in frequency, magnitude and rate of water level change leading to vertically differing potential for wave-driven geomorphic activity and thus topographic differences between landforms. While mainland barriers probably best represent rare peak lake levels, barrier spits or islands dominantly form at lower and intermediate levels through lower energy longshore drift, thus providing a more complete record of playa flood events. Additionally, the lowest magnitude events offer potential for frequent wetting and drying along playa margins that effectively drives salt-related production and aeolian sediment deflation. Therefore, in contrast to marine or perennial lake shorelines, the complete range of wind-driven sedimentary processes needs to be coupled with an accurate understanding of lake-specific flooding frequency and magnitude towards a comprehensive model of shoreline evolution around playa lakes.

KEYWORDS:

• Drylands
• ephemeral playa lakes
• shoreline dynamics
• Kati Thanda - Lake Eyre
• mapping
• Holocene

Acknowledgments

The authors would like to thank Matthew and Chantelle Williams from Anna Creek Station for granting access to their property around south-western Belt Bay. The Lake Eyre Flood Data was kindly provided courtesy of Bob Backway, Lake Eyre Yacht Club (www.LakeEyreYC.com). Fruitful discussions with Bob Backway, Sarah Mc Sweeney and Teresa Konlechner are gratefully acknowledged and have helped to initiate this paper. Comments and suggestions by Martin Williams and an anonymous reviewer have helped to improve the quality of this paper. Trevor Worthy is thanked for all efforts in editing and correcting the original manuscript.

Disclosure statement

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