Late Quaternary Changes In Lakes, Vegetation, And Climate In The Bonneville Basin Reconstructed From Sediment Cores From Great Salt Lake

Sediment cores from Great Salt Lake (GSL) provide the basis for reconstructing changes in lakes, vegetation, and climate for the last similar to 40 cal ka. Initially, the coring site was covered by a shallow saline lake and surrounded by Artemisia steppe or steppetundra under a cold and dry climate. As Lake Bonneville began to rise (from similar to 30 to 28 cal ka), Pinus and subalpine conifer pollen percentages increased and Artemisia declined, suggesting the onset of wetter conditions. Lake Bonneville oscillated near the Stansbury shoreline between similar to 26 and similar to 24 cal ka, rose to the Bonneville shoreline by similar to 18 cal ka, and then fell to the Provo shoreline, which it occupied until similar to 15 cal ka. Vegetation changed during this time span, albeit not always with the same direction or amplitude as the lake. The pollen percentages of Pinus and subalpine conifers were high from similar to 25 to 21.5 cal ka, indicating cool and moist conditions during the Stansbury oscillation and for much of the rise toward the Bonneville shoreline. Pinus percentages then decreased and Artemisia became codominant, suggesting drier and perhaps colder conditions from similar to 21 to similar to 15 cal ka, when Lake Bonneville was at or near its highest levels.Lake Bonneville declined to a low level by similar to 13 cal ka, while Pinus pollen percentages increased, indicating that conditions remained cooler and moister than today. During the Younger Dryas interval, the brief Gilbert episode rise in lake level was followed by a shallow lake with a stratified water column. This lake rise occurred as Pinus pollen percentages were declining and those of Artemisia were rising (reflecting increasingly dry conditions), after which Artemisia pollen was at very high levels (suggesting cold and dry conditions) for a brief period.Since similar to 10.6 cal ka lacustrine conditions have resembled those of present-day GSL. Pollen spectra for the period from similar to 10.6 to 7.2 cal ka have low levels of conifer pollen and high (for the Holocene) levels of desert and steppe taxa, suggesting generally dry conditions with maximum aridity occurring prior to the deposition of the Mazama tephra (similar to 7.6 cal ka). After similar to 10.6 cal ka, Juniperus pollen percentages began to increase and by similar to 7.2 cal ka juniper woodlands were well established on lower mountain slopes. From similar to 7 to 4 cal ka, pollen percentages fluctuated near their mean values for the entire Holocene. The neopluvial (similar to 4 to 2 cal ka) was the wettest part of the Holocene, with higher levels of Juniperus pollen and lower levels for steppe and desert taxa than in older Holocene sediments. Pollen percentages for the last similar to 2 cal ka are variable, but generally indicate a return to drier conditions.