Abstract
Radiocarbon was measured in dissolved inorganic carbon (DIC) and living organisms collected off the west coast of Baja California in October 1980. Samples from three locations were examined. Δ 14 C of DIC at the southernmost station was higher than those further north, which reflects reduced upwelling in the southern region. Crabs and anchovies had Δ 14 C values significantly lower than surface DIC Δ 14 C, indicating the incorporation of ‘older', sediment-derived carbon sources from their diets. Comparisons are made between our DIC Δ 14 C measurements and those obtained during other cruises and at a coastal site, from 1959 through 1987. Two distinct time histories of DIC Δ 14 C are apparent for the post-bomb period: 1) a lower Δ 14 C curve for sites close to the coast influenced by enhanced coastal upwelling; and 2) a higher Δ 14 C curve for sites further offshore within the California Current.
Cite
CITATION STYLE
Druffel, E. R. M., & Williams, P. M. (1991). Radiocarbon in Seawater and Organisms from the Pacific Coast of Baja California. Radiocarbon, 33(3), 291–296. https://doi.org/10.1017/s0033822200040315
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