Have looked at the link.
“This view from the Mast Camera on board Curiosity shows an example of cross-bedding from water passing over a loose bed of sediment. The cross-bedding – evident as layers at angles to each other – reflects formation and passage of waves of sand, one on top of the other. These are known as ripples, or dunes. The direction of migration of these small ripples and dunes was toward the southeast. That direction is toward Mount Sharp and away from the area where Curiosity found evidence of delta deposits where a stream entered a lake.”
Hmm, cross bedding is typically associated with water, so they could be right. It’s not normally a feature of lava flows, but it can also be created by wind-blown sediments. The flow direction seems to be towards Mt Sharp, which argues against a water-based origin. The crater itself is clearly the result of asteroid impact, erosive forces are nowhere near strong enough to have created the crater by erosion of lake sediments.
I’d be far happier with the lake picture if they could show that the bonding between sand grains was due to evaporites, salts that were left behind when the water evaporated. Curiosity has the spectroscopic tools to check this.