The dominant effect of the late Pleistocene sea level change was shoreline advance around the globe.

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The dominant effect of the late Pleistocene sea level change was actually shoreline retreat, as global sea levels fell around 120 meters during this time period due to the growth of glaciers and ice sheets. As a result, coastlines would have been exposed and inland. It wasn't until the Holocene, around 11,000 years ago, that sea levels began to rise again and shorelines advanced.

The Dominant Effect of the Late Pleistocene Sea Level Change