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Inverse solvent isotope effects arising from substrate triggering in the factor inhibiting hypoxia inducible factor.

ABSTRACT: Oxygen homeostasis plays a critical role in angiogenesis, erythropoiesis, and cell metabolism. Oxygen homeostasis is set by the hypoxia inducible factor-1? (HIF-1?) pathway, which is controlled by factor inhibiting HIF-1? (FIH). FIH is a non-heme Fe(II), ?-ketoglutarate (?KG)-dependent dioxygenase that inhibits HIF-1? by hydroxylating the C-terminal transactivation domain (CTAD) of HIF-1? at HIF-Asn(803). A tight coupling between CTAD binding and O2 activation is essential for hypoxia sensing, making changes in the coordination geometry of Fe(II) upon CTAD encounter a crucial feature of this enzyme. Although the consensus chemical mechanism for FIH proposes that CTAD binding triggers O2 activation by causing the Fe(II) cofactor to release an aquo ligand, experimental evidence of this has been absent. More broadly, this proposed coordination change at Fe(II) has not been observed during steady-state turnover in any ?KG oxygenase to date. In this work, solvent isotope effects (SIEs) were used as a direct mechanistic probe of substrate-triggered aquo release in FIH, as inverse SIEs (SIE < 1) are signatures for pre-equilibrium aquo release from metal ions. Our mechanistic studies of FIH have revealed inverse solvent isotope effects in the steady-state rate constants at limiting concentrations of CTAD or ?KG [(D2O)kcat/KM(CTAD) = 0.40 ± 0.07, and (D2O)kcat/KM(?KG) = 0.32 ± 0.08], providing direct evidence of aquo release during steady-state turnover. Furthermore, the SIE at saturating concentrations of CTAD and ?KG was inverse ((D2O)kcat = 0.51 ± 0.07), indicating that aquo release occurs after CTAD binds. The inverse kinetic SIEs observed in the steady state for FIH can be explained by a strong Fe-OH2 bond. The stable Fe-OH2 bond plays an important part in FIH's regulatory role over O2 homeostasis in humans and points toward a strategy for tightly coupling O2 activation with CTAD hydroxylation that relies on substrate triggering.

SUBMITTER: Hangasky JA

PROVIDER: S-EPMC4059518 | biostudies-literature | 2013 Mar

REPOSITORIES: biostudies-literature

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Inverse solvent isotope effects arising from substrate triggering in the factor inhibiting hypoxia inducible factor.

Hangasky John A JA Saban Evren E Knapp Michael J MJ

Biochemistry 20130218 9

Oxygen homeostasis plays a critical role in angiogenesis, erythropoiesis, and cell metabolism. Oxygen homeostasis is set by the hypoxia inducible factor-1α (HIF-1α) pathway, which is controlled by factor inhibiting HIF-1α (FIH). FIH is a non-heme Fe(II), α-ketoglutarate (αKG)-dependent dioxygenase that inhibits HIF-1α by hydroxylating the C-terminal transactivation domain (CTAD) of HIF-1α at HIF-Asn(803). A tight coupling between CTAD binding and O2 activation is essential for hypoxia sensing, m ...[more]

PMID: 23351038

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Project description:Prolyl hydroxylase domain 2 (PHD2) is deemed a primary oxygen sensor in humans, yet many details of its underlying mechanism are still not fully understood. (Fe(2+) + ?KG)PHD2 is 6-coordinate, with a 2His/1Asp facial triad occupying three coordination sites, a bidentate ?-ketoglutarate occupying two sites, and an aquo ligand in the final site. Turnover is thought to be initiated upon release of the aquo ligand, creating a site for O(2) to bind at the iron. Herein we show that steady-state turnover is faster under acidic conditions, with k(cat) exhibiting a kinetic pK(a) = 7.22. A variety of spectroscopic probes were employed to identify the active-site acid, through comparison of (Fe(2+) + ?KG)PHD2 at pH 6.50 with pH 8.50. The near-UV circular dichroism spectrum was virtually unchanged at elevated pH, indicating that the secondary structure did not change as a function of pH. UV-visible and Fe X-ray absorption spectroscopy indicated that the primary coordination sphere of Fe(2+) changed upon increasing the pH; extended X-ray absorption fine structure analysis found a short Fe-(O/N) bond length of 1.96 Å at pH 8.50, strongly suggesting that the aquo ligand was deprotonated at this pH. Solvent isotope effects were measured during steady-sate turnover over a wide pH-range, with an inverse solvent isotope effect (SIE) of k(cat) observed ((D(2)O)k(cat) = 0.91 ± 0.03) for the acid form; a similar SIE was observed for the basic form of the enzyme ((D(2)O)k(cat) = 0.9 ± 0.1), with an acid equilibrium offset of ?pK(a) = 0.67 ± 0.04. The inverse SIE indicated that aquo release from the active site Fe(2+) immediately precedes a rate-limiting step, suggesting that turnover in this enzyme may be partially limited by the rate of O(2) binding or activation, and suggesting that aquo release is relatively slow. The unusual kinetic pK(a) further suggested that PHD2 might function physiologically to sense both intracellular pO(2) as well as pH, which could provide for feedback between anaerobic metabolism and hypoxia sensing.

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Inverse solvent isotope effects arising from substrate triggering in the factor inhibiting hypoxia inducible factor.

Publications

Inverse solvent isotope effects arising from substrate triggering in the factor inhibiting hypoxia inducible factor.

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