Indications for abrupt Holocene climatic change: late Holocene oxygen isotope stratigraphy of the Great Salt Lake, Utah

Abstract

Oxygen-isotope stratigraphy in sediment cores together with carbonate mineralogy and percent carbonate stratigraphies have been used to reconstruct salinity changes, that is lake-level changes of the Great Salt Lake,Utah. For the late Holocene (last 5500 years), the data suggest four main points. -from Authors