Articles | Volume 11, issue 6
Clim. Past, 11, 931–938, 2015
https://doi.org/10.5194/cp-11-931-2015
Clim. Past, 11, 931–938, 2015
https://doi.org/10.5194/cp-11-931-2015

Research article 23 Jun 2015

Research article | 23 Jun 2015

A tropical speleothem record of glacial inception, the South American Summer Monsoon from 125 to 115 ka

S. J. Burns1, L. C. Kanner1,*, H. Cheng2,3, and R. Lawrence Edwards3 S. J. Burns et al.
  • 1Department of Geosciences, University of Massachusetts, Amherst, Massachusetts 01002, USA
  • 2Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710049, China
  • 3Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA
  • *present address: 2nd Nature LLC, 500 Seabright Ave, Santa Cruz, CA 95062, USA

Abstract. Relatively few marine or terrestrial paleoclimate studies have focused on glacial inception, the transition from an interglacial to a glacial climate state. As a result, neither the timing and structure of glacial inception nor the spatial pattern of glacial inception in different parts of the world is well known. Here we present results of a study of a speleothem from the Peruvian Andes that records changes in the intensity of South American Summer Monsoon (SASM) rainfall over the period from 125 to 115 ka. The results show that late in the last interglacial period, at 123 ka, SASM rainfall decreased, perhaps in response to a decrease in temperature and ice cover in the high northern latitudes and associated changes in atmospheric circulation. Then at 120.8 ka, a rapid increase in SASM rainfall marks the end of the last interglacial. After a more gradual increase between 120 and 117 ka, a second abrupt increase occurs at 117 ka. This pattern of change is mirrored to a remarkable degree by changes in the East Asian Monsoon. It is interpreted to reflect both a long-term gradual response of the monsoons to orbitally driven insolation changes and to rapid changes in Northern Hemisphere ice volume and temperature. Both monsoon systems are close to their full glacial conditions by 117 ka, before any significant decrease in atmospheric CO2.