What is often a consequence of reduced flow in ephemeral streams?

Reduced flow in ephemeral streams can significantly affect the way sediments are deposited in the streambed and surrounding areas. When water flow decreases, the energy available to transport sediments diminishes. This can lead to altered sediment deposition patterns, as lighter particles may settle out more easily, while heavier materials could remain suspended or be deposited in different locations than they would be during periods of higher flow.

Additionally, as the hydrology of the stream changes, the areas where water is present for shorter durations might not have the same capacity to carry sediments downstream, leading to a build-up in certain zones. These modifications can impact the stream ecosystem, affecting the habitats and organisms that depend on specific sediment conditions.

The other options, while relevant to changes that can occur in ecosystems, are less directly linked to the immediate effects of reduced flow on sediment deposition. For instance, while higher water temperatures can occur due to decreased flow and increased sun exposure, it does not directly pertain to sediment patterns. Similarly, biodiversity and invasive species may be influenced by a range of environmental factors, but they are not guaranteed consequences of changes in stream flow specifically concerning sediment deposition.