Paper No. 9
Presentation Time: 10:15 AM
Upwelling and Freshwater Runoff Events Recorded in the Brazilian Bivalve Semele Casali
HUNTLEY, John Warren, Geological Sciences, University of Missouri, 101 Geological Sciences Building, Columbia, MO 65211, KRAUSE Jr, Richard A., Museum fuer Naturkunde, Universitaet zu Berlin, Invalidenstrasse 43, Berlin, D-10115, Germany, ROMANEK, Christopher S., Savannah River Ecology Laboratory, Department of Geology, Univ of Georgia, Savannah River Ecology Laboratory, Draver E, Aiken, SC 29802, KAUFMAN, Darrell, Department of Geology, Northern Arizona University, Flagstaff, AZ 86011-4099, KOWALEWSKI, Michal, Department of Geosciences, Virginia Polytechnic Institute and State University, Blacksburg, VA 24061, BARBOUR WOOD, Susan, Geosciences & Natural Resources, Western Carolina University, 331 Stillwell Bldg, Cullowhee, NC 28723 and SIMOES, Marcello, Instituto de Biociencias, Universidade Estadual Paulista, Distrito de Rubiao Junior, CP. 510, 18.610-000, Botucatu, Brazil, huntleyj@missouri.edu
This project documents the long-term variability of freshwater runoff and upwelling events in coastal waters and the South Brazil Current of the Brazilian Bight over the last 1,000 yrs. Our methodology integrates amino acid racemization dating with trace element and stable isotope analyses to obtain high resolution time series of environmental proxies from numerous individually dated bivalves. Specimens of the aragonitic infaunal tellinid bivalve Semele casali were collected from two locations (10m and 30m depth) in Ubatuba Bay. Shell material grown in these water masses (background conditions) should display minimal variation in Mn/Ca and Ba/Ca and have δ
18O values from -1.3 to +2.2, and δ
13C values from +1 to +2. Shell material grown during upwelling events will be exposed to the colder nutrient-rich South Atlantic Central Water and should exhibit an increase in Ba/Ca, a larger range of δ
18O values, and a notable decline in δ
13C values. Shell deposited during freshwater runoff events should display concurrent increases in Mn/Ca and Ba/Ca and major concurrent decreases in δ
18O and δ
13C values.
Trace element profiles from 19 valves (0-944 years BP) suggest most bivalves (16) grew during background conditions, two grew during upwelling conditions, and one grew during freshwater runoff conditions. Stable isotope values for the background valves overlap with, though range slightly lower than, expected equilibrium values (δ18O: -2.1 to +0.6 and δ13C: -0.2 to +1.4). Stable isotope values for a valve that grew during runoff conditions were higher than expected (δ18O: -1.0 to +1.1 and δ13C: +0.7 to +2.1). The stable isotope results suggest that the bivalves grew primarily in standard marine background conditions but were occasionally exposed to other water masses.
These initial results suggest that past freshwater runoff and upwelling-induced productivity events can be detected and reconstructed in Holocene shell deposits.
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