Oceanographic controls on the carbon isotopic compositions of sinking particles from the Cariaco Basin |
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| Authors: | Mark Woodworth Miguel Goi Eric Tappa Kathy Tedesco Robert Thunell Yrene Astor Ramon Varela Jose Rafael Diaz-Ramos Frank Müller-Karger |
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| Institution: | aDepartment of Geological Sciences, Earth & Water Sciences Building 617, University of South Carolina, Columbia, SC 29208, USA;bEstacion de Investigaciones Marinas de Margarita, Fundacion La Salle de Ciencias Naturales, Aptdo. 144, Porlamar 6301, Venezuela;cDepartamento de Biologia Marina, Instituto Oceanografico de Venezuela, Apdo. 245, Cumana 6101A, Venezuela;dDepartment of Marine Science, University of South Florida, St. Petersburg, FL 33701, USA |
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| Abstract: | This study examined the relationship between carbon isotopic composition of sinking organic matter (OM) and the biological, physical and chemical properties of the surface ocean in the Cariaco Basin. The 13C/12C ratio of OM (δ13Corg) in sinking particles was determined on sediment trap samples from four depths collected from 1996 to 1999 as part of the CArbon Retention In A Colored Ocean time series. Water column properties, including temperature, productivity, chlorophyll and concentration of dissolved CO2, were concurrently measured on monthly cruises. The δ13Corg varied from a high of –17.7‰ to a low of –22.6‰ during the study period. The variation of the δ13Corg throughout seasonal cycles was directly proportional to the strength of upwelling and was negatively correlated with temperature (r2=0.64). During the 1996–1997 upwelling event, the strongest during the study period, the δ13Corg increased by  4.4‰ whereas during the 1998–1999 upwelling event, the weakest during the study period, the δ13Corg only increased by 3.3‰. Contrary to most previous studies, we observed a negative relationship (r2=0.53) between CO2 aq] and the estimated isotopic fractionation factor (εp). However, there was no correlation between εp and the calculated growth rates indicating that there was non-diffusive uptake of carbon into phytoplankton cells. It thus appears that CO2 aq] does not control the δ13Corg in the water column of the study site. The best explanation for the isotopic enrichment observed is a carbon concentrating mechanism (CCM) in phytoplankton. The existence of a CCM in phytoplankton has major implications for the interpretation of the δ13Corg in the Cariaco Basin. |
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