T121 Quantitative Reconstructions of the Large-Scale Cenozoic Terrestrial Climate Change

Monday, 28 October 2013
8:00 AM - 12:00 PM
Room 507


SEDIMENTOLOGICAL AND GEOCHRONOLOGICAL EVIDENCE FOR LARGE-MAGNITUDE PALEOFLOODS IN THE DESERT REGION OF BAJA CALFORNIA SUR, MEXICO

Paper number: T121-11
Program: Technical Sessions
Time: 10:30 AM – 10:45 AM


Authors


Abstract

Sedimentological analyses and optical dating results from extensive alluvial fan terraces in the desert region of Baja California Sur, Mexico, suggest that a very different climatic regime existed prior to the Holocene (~11.7 ka). Recently, researchers have discovered a more stable infrared-stimulated luminescence (IRSL) signal within K-feldspar, termed the 'post-IR IRSL' (Buylaert et al., 2009). This study measures the post-IR IRSL signal within individual grains of K-feldspar. The use of single grain measurements in luminescence dating allows for confident identification and circumvention of incomplete IRSL signal zeroing, a problem characteristic of dating alluvial fan sediments. By sampling in high density (typically four sediment samples per stratigraphic section) over a wide spatial extent (15 sites spread over 145 kilometers) we are able to assess the regularity of depositional events between and within terrace units. We demonstrate a regionally-consistent pattern of more recent, lower magnitude terrace deposits overlying pre-Holocene, larger magnitude deposits. Antidune bedforms and transported boulders found within these pre-Holocene units suggest paleoflood discharges up to ~13,000 m3/s. We interpret this change in depositional style to be reflective of a regional shift in climatic regime. The modern recurrence of these floods has important implications for local communities as well as, potentially, the southwest United States.

References:

Buylaert, J.P., Murray, A.S., Thomsen, K.J., Jain, M., 2009. Testing the potential of an elevated temperature IRSL signal from K-feldspar. Radiation Measurements 44, 560-565.