Abstract Details

SEDIMENT ACCUMULATIONS FROM THE BOCA PAILA CAVE SYSTEM LOCATED IN THE SIAN KA'AN BIOSPHERE OF THE YUCATAN PENINSULA PROVIDE EVIDENCE ON RECENT SEA-LEVEL RISE AND FORMATION OF THE CLASSIC MAYA CANAL SYSTEM

STEELE, Riley1, REINHARDT, Eduard1, ZHU, Juliet1, DEVOS, Frederic2 and MEACHAM, Samuel2, (1)School of Earth Environment and Society, McMaster University, 1280 Main St. W, Hamilton, ON L8S 4K1, Canada, (2)Centro Investigador del Sistema Acuifero de Quintana Roo A.C. (CINDAQ), Puerto Aventuras, QR xxxxxx, Mexico