Evidence of Early Holocene Glacial Advances in Southern South America from Cosmogenic Surface Exposure Dating

D. C. Douglass¹

B. S. Singer¹

M. R. Kaplan^1,2

R. P. Ackert³

D. M. Mickelson¹

M. W. Caffee⁴

¹Department of Geology and Geophysics, University of Wisconsin – Madison, Madison, WI 53706, USA.

²School of GeoSciences, University of Edinburgh, Edinburgh EH8 9 XP, Scotland, UK.

³Department of Earth and Planetary Science, Harvard University, Cambridge MA, 02138, USA.

⁴PRIME Lab, Purdue University, West Lafayette, IN, 47907, USA.

             ¹⁰Be and ³⁶Cl cosmogenic nuclide surface exposure dating of erratic boulders reveal two glacier advances in southern South America (46̊S) during the Early Holocene. Seven of ten and five of six boulders from two different moraines yield weighted mean ages of 8.5+0.7 and 6.2+0.8 ka (2s uncertainties), respectively. The four outliers are anomalously old (interpreted to contain inherited cosmogenic isotopes from prior exposure) and are identified on the basis of Chi-Squared statistics and bi-modal probability distribution curves. These glacial advances are likely the result of a northward migration of the southern westerlies causing an increase in precipitation and/or a decrease in temperature at this latitude. Reconstructions of equilibrium line altitudes (ELA) at the times of moraine deposition based on Accumulation Area Rations (AARs) are about 300 m lower than modern. This ELA depression is not particularly sensitive to the AAR used, and corresponds to conditions 2.4̊C cooler (if no change in precipitation), or 1000 mm/a wetter (if no change in temperature) than the modern climate. The older advance precedes the currently accepted initiation of Holocene glacial activity in southern South America by about 3000 years, and appears to be temporally synchronous with the “8.2 ka event” recorded in Greenland and many other parts of the world. The younger advance is slightly older than, but indistinguishable from, documented neoglacial advances and climate changes in southern South America and four other continents. If there are causal links between these temporally synchronous, globally distributed events, then rapid climate changes appear to be either externally forced (e.g. solar variability), or are rapidly propagated around the globe (e.g. atmospheric processes).