Dinuclear [(V<sup>V</sup>O(putrebactin))<sub>2</sub>(μ-OCH<sub>3</sub>)<sub>2</sub>] Formed in Solution as Established from LC-MS Measurements
Using <sup>50</sup>V‑Enriched V<sub>2</sub>O<sub>5</sub>
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Abstract
Analysis of 1:1 solutions of V(V)
and the macrocyclic dihydroxamic
acid siderophore putrebactin (pbH<sub>2</sub>) in 1:1 H<sub>2</sub>O/CH<sub>3</sub>OH using triple quadrupole liquid chromatography–mass
spectrometry (LC-MS-QQQ) (pH ≈ 4) showed two well-resolved
peaks (<i>t</i><sub>R</sub>(1) 10.85 min; <i>t</i><sub>R</sub>(2) 14.27 min) using simultaneous detection modes (absorbance,
450 nm; selective ion monitoring, <i>m</i>/<i>z</i> 437) characteristic of the previously identified oxidoV(V) complex
[V<sup>V</sup>O(pb)]<sup>+</sup> ([M]<sup>+</sup>, <i>m</i>/<i>z</i><sub>calc</sub> 437.1). Peak 1 gave mass spectrometry
(MS) signals consistent with [V<sup>V</sup>O(pb)]<sup>+</sup>, together
with [V<sup>V</sup>O(pb)(OH)] and the dinuclear complexes [(V<sup>V</sup>O(pb))<sub>2</sub>(μ-OH)]<sup>+</sup> and [(V<sup>V</sup>O(pb))<sub>2</sub>(μ-OH)<sub>2</sub>]. Peak 2 gave MS signals
consistent with [V<sup>V</sup>O(pb)]<sup>+</sup>, together with [V<sup>V</sup>O(pb)(OCH<sub>3</sub>)] and the dinuclear complexes
[(V<sup>V</sup>O(pb))<sub>2</sub>(μ-OCH<sub>3</sub>)]<sup>+</sup> and [(V<sup>V</sup>O(pb))<sub>2</sub>(μ-OCH<sub>3</sub>)<sub>2</sub>]. This analysis showed that two groups of V(V)/pbH<sub>2</sub> complexes with water- or methanol-derived ancillary ligands were
resolved by liquid chromatography (LC). The detection of [V<sup>V</sup>O(pb)]<sup>+</sup> in both peaks could be accounted for by its production
from dissociation (peak 1: [(V<sup>V</sup>O(pb))<sub>2</sub>(μ-OH)]<sup>+</sup> → [V<sup>V</sup>O(pb)]<sup>+</sup> + [V<sup>V</sup>O(pb)(OH)]; peak 2: [(V<sup>V</sup>O(pb))<sub>2</sub>(μ-OCH<sub>3</sub>)]<sup>+</sup> → [V<sup>V</sup>O(pb)]<sup>+</sup> +
[V<sup>V</sup>O(pb)(OCH<sub>3</sub>)]). The assignment of the
signal at <i>m</i>/<i>z</i><sub>obs</sub> 959.2
(100%) as the dinuclear complex [(V<sup>V</sup>O(pb))<sub>2</sub>(μ-OCH<sub>3</sub>)<sub>2</sub>] ([M + Na<sup>+</sup>]<sup>+</sup>, <i>m</i>/<i>z</i><sub>calc</sub> 959.3) and not an ion
cluster of mononuclear [V<sup>V</sup>O(pb)(OCH<sub>3</sub>)]
({2[M] + Na<sup>+</sup>}<sup>+</sup>, <i>m</i>/<i>z</i><sub>calc</sub> 959.3) was made unequivocal by the use of <sup>50</sup>V-enriched V<sub>2</sub>O<sub>5</sub>, which gave a signal with an
isotope pattern comprising the sum of the patterns of the three constituent <sup>51</sup>V–<sup>51</sup>V, <sup>51</sup>V–<sup>50</sup>V, and <sup>50</sup>V–<sup>50</sup>V species. Coordination
of methoxide was confirmed upon the replacement of CH<sub>3</sub>OH
with CD<sub>3</sub>OD, which generated [(V<sup>V</sup>O(pb))<sub>2</sub>(μ-OCD<sub>3</sub>)<sub>2</sub>] ([M + Na<sup>+</sup>]<sup>+</sup>, <i>m</i>/<i>z</i><sub>calc</sub> 965.3, <i>m</i>/<i>z</i><sub>obs</sub> 965.3). Analysis of 1:1
solutions of Mo(VI) and pbH<sub>2</sub> showed a single peak in the
LC (<i>t</i><sub>R</sub> 16.04 min), which gave MS signals
that were characterized as mononuclear [Mo<sup>VI</sup>(O)<sub>2</sub>(pb)] ([M + Na<sup>+</sup>]<sup>+</sup>, <i>m</i>/<i>z</i><sub>calc</sub> 523.1, <i>m</i>/<i>z</i><sub>obs</sub> 523.1) and dinuclear [(Mo<sup>VI</sup>O(pb))<sub>2</sub>(μ-O)<sub>2</sub>] ([M + Na<sup>+</sup>]<sup>+</sup>, <i>m</i>/<i>z</i><sub>calc</sub> 1019.1, <i>m</i>/<i>z</i><sub>obs</sub> 1019.2). The steric and electronic
effects of the <i>cis</i>-dioxido group(s) in [Mo<sup>VI</sup>(O)<sub>2</sub>(pb)] mitigated coordination of solvent-derived ancillary
ligands. The work highlights the value of using isotopically enriched
metal ion sources and deuterated solvents to deconvolute metal/siderophore
solution speciation. The results have relevance for an improved understanding
of the coordination chemistry of pbH<sub>2</sub> and other marine
siderophores in V(V)- and Mo(VI)-rich surface ocean waters