Controls on the carbon isotopic composition of Southern Ocean phytoplankton

• Published in: Global biogeochemical cycles 1999-12, Vol.13 (4), p.827-843
• Main Authors: Popp, B.N, Trull, T, Kenig, F, Wakeham, S.G, Rust, T.M, Tilbrook, B, Griffiths, F.B, Wright, S.W, Marchant, H.J, Bidigare, R.R
• Format: Article
• Language: English
• Subjects: biogeochemical cycles; chemical composition; Earth sciences; Earth, ocean, space; Exact sciences and technology; External geophysics; Geochemistry; isotopes; Marine; Mineralogy; Physical and chemical properties of sea water; Physics of the oceans; phytoplankton; Silicates; Water geochemistry
• ISSN: 0886-6236; 1944-9224
• DOI: 10.1029/1999GB900041

Carbon isotopic compositions of suspended organic matter and biomarker compounds were determined for 59 samples filtered from Southern Ocean surface waters in January 1994 along two north‐south transects (WOCE SR3 from Tasmania to Antarctica, and across the Princess Elizabeth Trough (PET) east of Prydz Bay, Antarctica). Along the SR3 line, bulk organic matter show generally decreasing 13C contents southward, which are well correlated with increasing dissolved molecular carbon dioxide concentrations, CO2(aq). This relationship does not hold along the PET transect. Using concentrations and isotopic compositions of molecular compounds, we evaluate the relative roles of several factors affecting the δ13C of Southern Ocean suspended particulate organic matter. Along the WOCE SR3 transect, the concentration of CO2(aq) plays an important role. It is well described by a supply versus demand model for the extent of cellular CO2 utilization and its associated linear dependence of isotopic fractionation (EP) on the reciprocal of CO2(aq). An equally important factor appears to be changes in algal assemblages along the SR3 transect, with their contribution to isotopic fractionation also well described by the supply and demand model, when formulated to include the cell surface/volume control of supply. Changes in microalgal growth rates appear to have a minor effect on EP. Along the PET transect, algal assemblage changes and possibly changes in microalgal growth rates appear to strongly affect the carbon isotopic variations of suspended organic matter. These results can be used to improve the formulation of modern carbon cycle models that include phytoplankton carbon isotopic fractionation.