The Marine Radiocarbon Reservoir Effect and its correlation with the ocean dynamics
This study presents MRE data for the Brazilian coast, where the two main ocean currents display different features. The Brazil current carries warm subtropical waters while the Falklands current is composed by cold subantartic waters. They flow in opposite directions along the coast and their encounter, around 38S, creates a strong thermohaline front referred to as Brazil-Falklands Confluence (Roden, 1986; Gordon,1989).
Radiocarbon dating of marine species was performed for different regions on the Brazilian coast. The use of samples from both, archaeological sites and museum collections, can give a consistent time frame for changes in the MRE and, potentially, in the South Atlantic Ocean circulation patterns. Moreover, seasonally or annually resolved coral carbon concentration measurements constitute a convenient tool for assessing sea-water radiocarbon signatures (Druffel and Linick, 1978; Dunbar and Colle, 1999; Druffel et al., 2007). These measurements are being performed in an attempt of creating a coral-based database for radiocarbon variability in the South Atlantic Ocean through time.
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Druffel, E. R. M., S. Griffin, S. R. Beaupre, and R. B. Dunbar (2007), Oceanic climate and circulation changes during the past four centuries from radiocarbon in corals, Geophys. Res. Lett., 34, L09601.
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