Iron-stimulated changes in C-13 fractionation and export by equatorial Pacific phytoplankton: Toward a paleogrowth rate proxy

We present delta(13)C values for phytol, an algal biomarker, which document up to 7 per mil isotopic enrichment during the IronEx II iron fertilizatio n experiment. We evaluate these data using a laboratory-derived C-13 fracti onation model and show this variability is largely the result of elevated g rowth rates. Isotopic enrichment and stimulation of growth rate were accomp anied by a sevenfold increase in the export of particulate organic carbon a s estimated from Th-234 activities. This is the first direct evidence that enhanced productivity following iron enrichment can lead to both increased export of organic matter and an associated isotopic signal in an algal biom arker. On the basis of these results, we propose biomarker isotopic data be used in conjunction with paleo-CO2 records to reconstruct paleogrowth rate s. This approach provides a means to test for iron-stimulated changes in al gal growth in sedimentary records.