Author:

Keywords:

k-p boundary, texas, brazos, sequence stratigraphy, sea-level, chicxulub impact, ejecta, clay mineral distribution, single shocked zircons, sea-level fluctuations, gulf-of-mexico, tertiary boundary, t boundary, calcareous nannoplankton, mass extinction, foraminiferal biostratigraphy, planktonic-foraminifera, Science & Technology, Physical Sciences, Geology, K-P boundary, Texas, Brazos, Chicxulub impact, CLAY MINERAL DISTRIBUTION, SINGLE SHOCKED ZIRCONS, SEA-LEVEL FLUCTUATIONS, TERTIARY BOUNDARY, T BOUNDARY, CALCAREOUS NANNOPLANKTON, BLAKE-NOSE, FORAMINIFERAL BIOSTRATIGRAPHY, PLANKTONIC-FORAMINIFERA, MASS EXTINCTION, 0403 Geology, 3705 Geology

Abstract:

Two cores from Brazos, Texas, spanning the Cretaceous-Palcogene (K-P) boundary, are investigated by a multidisciplinary approach aiming at unraveling environmental changes and sequence stratigraphic setting. In addition, the sedimentology of the K- event deposit and its correlation with the K-P boundary is studied. Foraminifera and nannofossil stratigraphy indicates that both cores include a latest Maastrichtian (Zone CF1-CF2) and earliest Danian (P0, P alpha and P1a) shale sequence with a sandy and Chicxulub ejecta-bearing event deposit at the K-P boundary; a hiatus of unknown duration may be present by the unconformable base of the event deposit. Planktic foraminifera as well as calcareous nannofossil abundance and diversity both decline abruptly above the event deposit (K-P mass extinction), whereas benthic foraminifera show a pronounced faunal change but no mass extinction.