To understand the molecular details of O -tolerant hydrogen cycling by a soluble NAD -reducing [NiFe] hydrogenase, we herein present the first bioinspired heterobimetallic S-oxygenated [NiFe] complex as a structural and vibrational spectroscopic model for the oxygen-inhibited [NiFe] active site. This compound and its non-S-oxygenated congener were fully characterized, and their electronic structures were elucidated in a combined experimental and theoretical study with emphasis on the bridging sulfenato moiety. Based on the vibrational spectroscopic properties of these complexes, we also propose novel strategies for exploring S-oxygenated intermediates in hydrogenases and similar enzymes.
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http://dx.doi.org/10.1002/anie.201611069 | DOI Listing |
J Inorg Biochem
March 2025
Department of Chemistry, The Johns Hopkins University, 3400 North Charles Street, Baltimore, MD 21218, United States. Electronic address:
The synthesis and characterization of a new ligand, 1-(bis(pyridin-2-ylmethyl) amino)-2-methylpropane-2-thiolate (BPAS) and its nonheme iron complex, Fe(BPAS)Br (1), is reported. Reaction of 1 with O at -20 °C generates a high-spin iron(III)-hydroxide complex, [Fe(OH)(BPAS)(Br)] (2), that was characterized by UV-vis, Fe Mössbauer, and electron paramagnetic resonance (EPR) spectroscopies, and electrospray ionization mass spectrometry (ESI-MS). Density functional theory (DFT) calculations were employed to support the spectroscopic assignments.
View Article and Find Full Text PDFJ Am Chem Soc
March 2024
Department of Chemistry, The Johns Hopkins University, 3400 North Charles Street, Baltimore, Maryland 21218, United States.
A new alkylthiolate-ligated nonheme iron complex, Fe(BNPAS)Br (), is reported. Reaction of with O at -40 °C, or reaction of the ferric form with O at -80 °C, gives a rare iron(III)-superoxide intermediate, [Fe(O)(BNPAS)] (), characterized by UV-vis, Fe Mössbauer, ATR-FTIR, EPR, and CSIMS. Metastable then converts to an S-oxygenated Fe(sulfinate) product via a sequential O atom transfer mechanism involving an iron-sulfenate intermediate.
View Article and Find Full Text PDFElife
June 2023
School of Oceanography, University of Washington, Seattle, United States.
Phytoplankton rely on diverse mechanisms to adapt to the decreased iron bioavailability and oxidative stress-inducing conditions of today's oxygenated oceans, including replacement of the iron-requiring ferredoxin electron shuttle protein with a less-efficient iron-free flavodoxin under iron-limiting conditions. Yet, diatoms transcribe flavodoxins in high-iron regions in contrast to other phytoplankton. Here, we show that the two clades of flavodoxins present within diatoms exhibit a functional divergence, with only clade II flavodoxins displaying the canonical role in acclimation to iron limitation.
View Article and Find Full Text PDFNat Commun
October 2022
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing, 10083, China.
Reconstructing historical atmospheric oxygen (O) levels at finer temporal resolution is a top priority for exploring the evolution of life on Earth. This goal, however, is challenged by gaps in traditionally employed sediment-hosted geochemical proxy data. Here, we propose an independent strategy-machine learning with global mafic igneous geochemistry big data to explore atmospheric oxygenation over the last 4.
View Article and Find Full Text PDFR Soc Open Sci
January 2022
National Center for Atmospheric Research, Boulder, CO 80301, USA.
The history of molecular oxygen (O) in Earth's atmosphere is still debated; however, geological evidence supports at least two major episodes where O increased by an order of magnitude or more: the Great Oxidation Event (GOE) and the Neoproterozoic Oxidation Event. O concentrations have likely fluctuated (between 10 and 1.5 times the present atmospheric level) since the GOE ∼2.
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