We developed a method to measure picogram quantities of vanadium in calcite and seawater by isotope dilution (ID) inductively coupled plasma mass spectrometry using electrothermal vaporization (ETV) to introduce the sample into the plasma. A 50 V isotope spike enriched to 44 atom % was equilibrated with samples, followed by chemical purification by cation exchange chromatography. Samples were introduced into the ETV unit with a Pd modifier and heated to 1000 °C. This quantitatively eliminates the ClO + isobaric interference with V at m/z 51 for solutions up to 0.5 N HCl. The procedural blank was 0.27 pg of V. Corrections for 50 Ti and 50 Cr, which interfere with the 50 V signal, were made by measurement of 49 Ti and 53 Cr. These isobaric interferences and variable ArC levels were the limiting sources of error in the ID measurement and diminished the detection limit to 6 pg of V. The detection limit for nonisotope dilution applications was 0.3 pg of V. Measurement precision on the same sample of dissolved calcite over the course of one run was (3% (1σ). Accuracy was confirmed by determination of V standards in CaCO 3 and by comparative measurement with ID thermal ionization mass spectrometry and graphite furnace atomic absorption spectroscopy.Calcitic shells of foraminifera, unicellular marine animals that grow in surface waters and in ocean sediments, have concentrations of certain elements that are determined by the seawater concentration of the water in which the shell was formed. The determination of trace elements such as Cd, Ba, and Li in foraminiferal calcite has proven to be a powerful tool to deduce the history of ocean circulation patterns, nutrient concentrations, and oceanic inputs. [1][2][3][4] The development of new foraminiferal tracers including B, F, U, Mg, and V is an active area of oceanographic research which has shed new light on paleoclimatology and variations in the global carbon cycle. [5][6][7][8]