Several species of marine tunicates store oxygen-sensitive VIII in blood cells. A sensitive colorimetric VIII assay was used to survey the leading candidates for the native reducing agent of vanadate in tunicates (i.e., An-type tunichromes, glutathione, NADPH, and H2S) in reactions with VV or VIV ions under anaerobic, aqueous conditions at acidic or neutral pH. Except for the case of An-1 and VV ions in pH 7 buffer, the assay results for the biogenic reducing agents clearly showed that appreciable quantities of VIII products were not generated under the conditions tested. Therefore, the assay results place new limits on hypothetical mechanisms of VIII formation in vivo. For reactions between An-1 and VV ions in pH 7 buffer, low levels of VIII products could not be ruled out because of an interfering peak in the colorimetric assays. For similar reactions between VV ions and An-1, or an An-1,2 mixture, in mildly to moderately basic media, the product mixtures precipitated as greenish black solids. Analyses of the precipitated V/An mixtures using vanadium K-edge X-ray absorption spectroscopy (XAS) showed that the major products were tris(catecholate)-type VIV complexes (65 +/- 6%) and bis(catecholate)-type VIVO complexes (20 +/- 4%). XAS analysis of the V/An-1 product mixture also provided evidence of a minor VIII component (9 +/- 5% of total V), notable for possible relevance to tunicate biochemistry. The combined results of XAS studies, spectrophotometric studies [Ryan, D. E., et al. (1996) Biochemistry 35, 8640-8650], and EPR studies [Grant, K. B., et al. (1996) J. Inorg. Biochem. (manuscript in preparation)] consistently establish that reactions between tunichromes (Mm-1 or An-1) and VV ions generate predominantly VIV-tunichrome complexes in neutral to moderately basic aqueous media.