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Instruments / Technical Area	Publication Details	Published
	Structure of photosystem II and substrate binding at room temperature Iris D. Young , Mohamed Ibrahim , Ruchira Chatterjee , Sheraz Gul , Franklin D. Fuller , Sergey Koroidov , Aaron S. Brewster , Rosalie Tran , Roberto Alonso-Mori , Thomas Kroll , Tara Michels-Clark , Hartawan Laksmono , Raymond G. Sierra , Claudiu A. Stan , Rana Hussein , Miao Zhang , Lacey Douthit , Markus Kubin , Casper De Lichtenberg , Long Vo Pham , Håkan Nilsson , Mun Hon Cheah , Dmitriy Shevela , Claudio Saracini , Mackenzie A. Bean , Ina Seuffert , Dimosthenis Sokaras , Tsu-Chien Weng , Ernest Pastor , Clemens Weninger , Thomas Fransson , Louise Lassalle , Philipp Bräuer , Pierre Aller , Peter T. Docker , Babak Andi , Allen M. Orville , James M. Glownia , Silke Nelson , Marcin Sikorski , Diling Zhu , Mark S. Hunter , Thomas J. Lane , Andy Aquila , Jason E. Koglin , Joseph Robinson , Mengning Liang , Sébastien Boutet , Artem Y. Lyubimov , Monarin Uervirojnangkoorn , Nigel W. Moriarty , Dorothee Liebschner , Pavel V. Afonine , David G. Waterman , Gwyndaf Evans , Philippe Wernet , Holger Dobbek , William I. Weis , Axel T. Brunger , Petrus H. Zwart , Paul D. Adams , Athina Zouni , Johannes Messinger , Uwe Bergmann , Nicholas K. Sauter , Jan Kern , Vittal K. Yachandra , Junko Yano Nature DOI: 10.1038/nature20161 Show Abstract ▼ Abstract: Light-induced oxidation of water by photosystem II (PS II) in plants, algae and cyanobacteria has generated most of the dioxygen in the atmosphere. PS II, a membrane-bound multi-subunit pigment protein complex, couples the one-electron photochemistry at the reaction centre with the four-electron redox chemistry of water oxidation at the Mn4CaO5 cluster in the oxygen-evolving complex (OEC). Under illumination, the OEC cycles through five intermediate S-states (S0 to S4)1, in which S1 is the dark-stable state and S3 is the last semi-stable state before O–O bond formation and O2 evolution2, 3. A detailed understanding of the O–O bond formation mechanism remains a challenge, and will require elucidation of both the structures of the OEC in the different S-states and the binding of the two substrate waters to the catalytic site4, 5, 6. Here we report the use of femtosecond pulses from an X-ray free electron laser (XFEL) to obtain damage-free, room temperature structures of dark-adapted (S1), two-flash illuminated (2F; S3-enriched), and ammonia-bound two-flash illuminated (2F-NH3; S3-enriched) PS II. Although the recent 1.95 Å resolution structure of PS II at cryogenic temperature using an XFEL7 provided a damage-free view of the S1 state, measurements at room temperature are required to study the structural landscape of proteins under functional conditions8, 9, and also for in situ advancement of the S-states. To investigate the water-binding site(s), ammonia, a water analogue, has been used as a marker, as it binds to the Mn4CaO5 cluster in the S2 and S3 states10. Since the ammonia-bound OEC is active, the ammonia-binding Mn site is not a substrate water site10, 11, 12, 13. This approach, together with a comparison of the native dark and 2F states, is used to discriminate between proposed O–O bond formation mechanisms.	Nov 2016
	Drop-on-demand sample delivery for studying biocatalysts in action at X-ray free-electron lasers Franklin D Fuller , Sheraz Gul , Ruchira Chatterjee , E. Sethe Burgie , Iris D. Young , Hugo Lebrette , Vivek Srinivas , Aaron Brewster , Tara Michels-Clark , Jonathan A Clinger , Babak Andi , Mohamed Ibrahim , Ernest Pastor , Casper De Lichtenberg , Rana Hussein , Christopher J Pollock , Miao Zhang , Claudiu A Stan , Thomas Kroll , Thomas Fransson , Clemens Weninger , Markus Kubin , Pierre Aller , Louise Lassalle , Philipp Braeuer , Mitchell D. Miller , Muhamed Amin , Sergey Koroidov , Christian G. Roessler , Marc Allaire , Raymond G Sierra , Peter T. Docker , James M. Glownia , Silke Nelson , Jason E Koglin , Diling Zhu , Matthieu Chollet , Sanghoon Song , Henrik Lemke , Mengning Liang , Dimosthenis Sokaras , Roberto Alonso-Mori , Athina Zouni , Johannes Messinger , Uwe Bergmann , Amie K. Boal , J. Martin Bollinger , Carsten Krebs , Martin Högbom , George N. Phillips , Richard D. Vierstra , Nicholas K Sauter , Allen M. Orville , Jan Kern , Vittal K Yachandra , Junko Yano Nature Methods 5 DOI: 10.1038/nmeth.4195 Show Abstract ▼ Abstract: X-ray crystallography at X-ray free-electron laser sources is a powerful method for studying macromolecules at biologically relevant temperatures. Moreover, when combined with complementary techniques like X-ray emission spectroscopy, both global structures and chemical properties of metalloenzymes can be obtained concurrently, providing insights into the interplay between the protein structure and dynamics and the chemistry at an active site. The implementation of such a multimodal approach can be compromised by conflicting requirements to optimize each individual method. In particular, the method used for sample delivery greatly affects the data quality. We present here a robust way of delivering controlled sample amounts on demand using acoustic droplet ejection coupled with a conveyor belt drive that is optimized for crystallography and spectroscopy measurements of photochemical and chemical reactions over a wide range of time scales. Studies with photosystem II, the phytochrome photoreceptor, and ribonucleotide reductase R2 illustrate the power and versatility of this method.	Feb 2017
	Structures of the intermediates of Kok’s photosynthetic water oxidation clock Jan Kern , Ruchira Chatterjee , Iris D. Young , Franklin D. Fuller , Louise Lassalle , Mohamed Ibrahim , Sheraz Gul , Thomas Fransson , Aaron S. Brewster , Roberto Alonso-Mori , Rana Hussein , Miao Zhang , Lacey Douthit , Casper De Lichtenberg , Mun Hon Cheah , Dmitry Shevela , Julia Wersig , Ina Seuffert , Dimosthenis Sokaras , Ernest Pastor , Clemens Weninger , Thomas Kroll , Raymond G. Sierra , Pierre Aller , Agata Butryn , Allen M. Orville , Mengning Liang , Alexander Batyuk , Jason E. Koglin , Sergio Carbajo , Sébastien Boutet , Nigel W. Moriarty , James M. Holton , Holger Dobbek , Paul D. Adams , Uwe Bergmann , Nicholas K. Sauter , Athina Zouni , Johannes Messinger , Junko Yano , Vittal K. Yachandra Nature 11 DOI: 10.1038/s41586-018-0681-2 Show Abstract ▼ Abstract: Inspired by the period-four oscillation in flash-induced oxygen evolution of photosystem II discovered by Joliot in 1969, Kok performed additional experiments and proposed a five-state kinetic model for photosynthetic oxygen evolution, known as Kok’s S-state clock or cycle1,2. The model comprises four (meta)stable intermediates (S0, S1, S2 and S3) and one transient S4 state, which precedes dioxygen formation occurring in a concerted reaction from two water-derived oxygens bound at an oxo-bridged tetra manganese calcium (Mn4CaO5) cluster in the oxygen-evolving complex3,4,5,6,7. This reaction is coupled to the two-step reduction and protonation of the mobile plastoquinone QB at the acceptor side of PSII. Here, using serial femtosecond X-ray crystallography and simultaneous X-ray emission spectroscopy with multi-flash visible laser excitation at room temperature, we visualize all (meta)stable states of Kok’s cycle as high-resolution structures (2.04–2.08 Å). In addition, we report structures of two transient states at 150 and 400 µs, revealing notable structural changes including the binding of one additional ‘water’, Ox, during the S2→S3 state transition. Our results suggest that one water ligand to calcium (W3) is directly involved in substrate delivery. The binding of the additional oxygen Ox in the S3 state between Ca and Mn1 supports O–O bond formation mechanisms involving O5 as one substrate, where Ox is either the other substrate oxygen or is perfectly positioned to refill the O5 position during O2 release. Thus, our results exclude peroxo-bond formation in the S3 state, and the nucleophilic attack of W3 onto W2 is unlikely.	Nov 2018
	Untangling the sequence of events during the S 2 → S 3 transition in photosystem II and implications for the water oxidation mechanism Mohamed Ibrahim , Thomas Fransson , Ruchira Chatterjee , Mun Hon Cheah , Rana Hussein , Louise Lassalle , Kyle D. Sutherlin , Iris D. Young , Franklin D. Fuller , Sheraz Gul , In-Sik Kim , Philipp S. Simon , Casper De Lichtenberg , Petko Chernev , Isabel Bogacz , Cindy C. Pham , Allen M. Orville , Nicholas Saichek , Trent Northen , Alexander Batyuk , Sergio Carbajo , Roberto Alonso-Mori , Kensuke Tono , Shigeki Owada , Asmit Bhowmick , Robert Bolotovsky , Derek Mendez , Nigel W. Moriarty , James M. Holton , Holger Dobbek , Aaron S. Brewster , Paul D. Adams , Nicholas K. Sauter , Uwe Bergmann , Athina Zouni , Johannes Messinger , Jan Kern , Vittal K. Yachandra , Junko Yano Proceedings Of The National Academy Of Sciences 766 DOI: 10.1073/pnas.2000529117 Open Access Show Abstract ▼ Abstract: In oxygenic photosynthesis, light-driven oxidation of water to molecular oxygen is carried out by the oxygen-evolving complex (OEC) in photosystem II (PS II). Recently, we reported the room-temperature structures of PS II in the four (semi)stable S-states, S1, S2, S3, and S0, showing that a water molecule is inserted during the S2 → S3 transition, as a new bridging O(H)-ligand between Mn1 and Ca. To understand the sequence of events leading to the formation of this last stable intermediate state before O2 formation, we recorded diffraction and Mn X-ray emission spectroscopy (XES) data at several time points during the S2 → S3 transition. At the electron acceptor site, changes due to the two-electron redox chemistry at the quinones, QA and QB, are observed. At the donor site, tyrosine YZ and His190 H-bonded to it move by 50 µs after the second flash, and Glu189 moves away from Ca. This is followed by Mn1 and Mn4 moving apart, and the insertion of OX(H) at the open coordination site of Mn1. This water, possibly a ligand of Ca, could be supplied via a “water wheel”-like arrangement of five waters next to the OEC that is connected by a large channel to the bulk solvent. XES spectra show that Mn oxidation (τ of ∼350 µs) during the S2 → S3 transition mirrors the appearance of OX electron density. This indicates that the oxidation state change and the insertion of water as a bridging atom between Mn1 and Ca are highly correlated.	May 2020
	High resolution XFEL structure of the soluble methane monooxygenase hydroxylase complex with its regulatory component at ambient temperature in two oxidation states Vivek Srinivas , Rahul Banerjee , Hugo Lebrette , Jason C. Jones , Oskar Aurelius , In-Sik Kim , Cindy C. Pham , Sheraz Gul , Kyle Sutherlin , Asmit Bhowmick , Juliane John , Esra Bozkurt , Thomas Fransson , Pierre Aller , Agata Butryn , Isabel Bogacz , Philipp Stefan Simon , Stephen Keable , Alexander Britz , Kensuke Tono , Kyung-Sook Kim , Sang-Youn Park , Sang-Jae Lee , Jaehyun Park , Roberto Alonso-Mori , Franklin Fuller , Alexander Batyuk , Aaron S. Brewster , Uwe Bergmann , Nicholas Sauter , Allen M. Orville , Vittal K. Yachandra , Junko Yano , John D. Lipscomb , Jan F. Kern , Martin Högbom Journal Of The American Chemical Society DOI: 10.1021/jacs.0c05613 Show Abstract ▼ Abstract: Soluble methane monooxygenase (sMMO) is a multicomponent metalloenzyme that catalyzes the conversion of methane to methanol at ambient temperature using a nonheme, oxygen-bridged dinuclear iron cluster in the active site. Structural changes in the hydroxylase component (sMMOH) containing the diiron cluster caused by complex formation with a regulatory component (MMOB) and by iron reduction are important for the regulation of O2 activation and substrate hydroxylation. Structural studies of metalloenzymes using traditional synchrotron-based X-ray crystallography are often complicated by partial X-ray-induced photoreduction of the metal center, thereby obviating determination of the structure of pure oxidation states. Here microcrystals of the sMMOH:MMOB complex from Methylosinus trichosporium OB3b were serially exposed to X-ray free electron laser (XFEL) pulses, where the ≦35 fs duration of exposure of an individual crystal yields diffraction data before photoreduction-induced structural changes can manifest. Merging diffraction patterns obtained from thousands of crystals generates radiation damage free, 1.95 Å resolution crystal structures for the fully oxidized and fully reduced states of the sMMOH:MMOB complex for the first time. The results provide new insight into the manner by which the diiron cluster and the active site environment are reorganized by the regulatory protein component in order to enhance the steps of oxygen activation and methane oxidation. This study also emphasizes the value of XFEL and serial femtosecond crystallography (SFX) methods for investigating the structures of metalloenzymes with radiation sensitive metal active sites.	Jul 2020
I03-Macromolecular Crystallography I04-1-Macromolecular Crystallography (fixed wavelength) I04-Macromolecular Crystallography I24-Microfocus Macromolecular Crystallography	X-ray free-electron laser studies reveal correlated motion during isopenicillin N synthase catalysis Patrick Rabe , Jos J. A. G. Kamps , Kyle D. Sutherlin , James D. S. Linyard , Pierre Aller , Cindy C. Pham , Mikako Makita , Ian Clifton , Michael A. Mcdonough , Thomas M. Leissing , Denis Shutin , Pauline A. Lang , Agata Butryn , Jurgen Brem , Sheraz Gul , Franklin D. Fuller , In-Sik Kim , Mun Hon Cheah , Thomas Fransson , Asmit Bhowmick , Iris D. Young , Lee O'Riordan , Aaron S. Brewster , Ilaria Pettinati , Margaret Doyle , Yasumasa Joti , Shigeki Owada , Kensuke Tono , Alexander Batyuk , Mark S. Hunter , Roberto Alonso-Mori , Uwe Bergmann , Robin L. Owen , Nicholas K. Sauter , Timothy D. W. Claridge , Carol V. Robinson , Vittal K. Yachandra , Junko Yano , Jan F. Kern , Allen M. Orville , Christopher J. Schofield Science Advances 7 DOI: 10.1126/sciadv.abh0250 Diamond Proposal Number(s): [23459, 19458] Open Access Show Abstract ▼ Abstract: Isopenicillin N synthase (IPNS) catalyzes the unique reaction of L-δ-(α-aminoadipoyl)-L-cysteinyl-D-valine (ACV) with dioxygen giving isopenicillin N (IPN), the precursor of all natural penicillins and cephalosporins. X-ray free-electron laser studies including time-resolved crystallography and emission spectroscopy reveal how reaction of IPNS:Fe(II):ACV with dioxygen to yield an Fe(III) superoxide causes differences in active site volume and unexpected conformational changes that propagate to structurally remote regions. Combined with solution studies, the results reveal the importance of protein dynamics in regulating intermediate conformations during conversion of ACV to IPN. The results have implications for catalysis by multiple IPNS-related oxygenases, including those involved in the human hypoxic response, and highlight the power of serial femtosecond crystallography to provide insight into long-range enzyme dynamics during reactions presently impossible for nonprotein catalysts.	Aug 2021
I18-Microfocus Spectroscopy	Leaf metallome preserved over 50 million years N. P. Edwards , P. L. Manning , U. Bergmann , P. L. Larson , B. E. Van Dongen , W. I. Sellers , S. M. Webb , D. Sokaras , R. Alonso-Mori , K. Ignatyev , H. E. Barden , A. Van Veelen , J. Anne , V. M. Egerton , R. A. Wogelius Metallomics DOI: 10.1039/c3mt00242j Diamond Proposal Number(s): [8597] Open Access Show Abstract ▼ Abstract: Large-scale Synchrotron Rapid Scanning X-ray Fluorescence (SRS-XRF) elemental mapping and X-ray absorption spectroscopy are applied here to fossil leaf material from the ∼50 Mya Green River Formation (USA) in order to improve our understanding of the chemistry of fossilized plant remains. SRS-XRF of fossilized animals has previously shown that bioaccumulated trace metals and sulfur compounds may be preserved in their original distributions and these elements can also act as biomarkers for specific biosynthetic pathways. Similar spatially resolved chemical data for fossilized plants is sparsely represented in the literature despite the multitude of other chemical studies performed. Here, synchrotron data from multiple specimens consistently show that fossil leaves possess chemical inventories consisting of organometallic and organosulfur compounds that: (1) map discretely within the fossils, (2) resolve fine scale biological structures, and (3) are distinct from embedding sedimentary matrices. Additionally, the chemical distributions in fossil leaves are directly comparable to those of extant leaves. This evidence strongly suggests that a significant fraction of the chemical inventory of the examined fossil leaf material is derived from the living organisms and that original bioaccumulated elements have been preserved in situ for 50 million years. Chemical information of this kind has so far been unknown for fossilized plants and could for the first time allow the metallome of extinct flora to be studied.	Apr 2014
I18-Microfocus Spectroscopy	Synchrotron imaging reveals bone healing and remodelling strategies in extinct and extant vertebrates J. Anne , N. P. Edwards , R. A. Wogelius , A. R. Tumarkin-Deratzian , W. I. Sellers , A. Van Veelen , U. Bergmann , D. Sokaras , R. Alonso-Mori , K. Ignatyev , V. M. Egerton , P. L. Manning Journal Of The Royal Society Interface 11 (96), 20140277 - 20140277 DOI: 10.1098/rsif.2014.0277 PMID: 24806709 Open Access Show Abstract ▼ Abstract: Current understanding of bone healing and remodelling strategies in vertebrates has traditionally relied on morphological observations through the histological analysis of thin sections. However, chemical analysis may also be used in such interpretations, as different elements are known to be absorbed and used by bone for different physiological purposes such as growth and healing. These chemical signatures are beyond the detection limit of most laboratory-based analytical techniques (e.g. scanning electron microscopy). However, synchrotron rapid scanningX-ray fluorescence (SRSXRF) is an elemental mapping technique that uniquely combines high sensitivity (ppm), excellent sample resolution (20100 µm) and the ability to scan large specimens (decimetre scale) approximately 3000 times faster than other mapping techniques. Here, we use SRSXRF combined with microfocus elemental mapping (220 µm) to determine the distribution and concentration of trace elements within pathological and normal bone of both extant and extinct archosaurs (Cathartes aura and Allosaurus fragilis). Results reveal discrete chemical inventories within different bone tissue types and preservation modes. Chemical inventories also revealed detail of histological features not observable in thin section, including fine structures within the interface between pathological and normal bone as well as woven texture within pathological tissue.	Jul 2014
I18-Microfocus Spectroscopy	Bacteria or melanosomes? A geochemical analysis of micro-bodies on a tadpole from the Oligocene Enspel Formation of Germany Holly Barden , Uwe Bergmann , Nicholas Edwards , Victoria Egerton , Phillip Manning , Sarah Perry , Arjen Van Veelen , R A Wogelius , Bart Van Dongen Palaeobiodiversity And Palaeoenvironments DOI: 10.1007/s12549-014-0177-5 Diamond Proposal Number(s): [8597] Open Access Show Abstract ▼ Abstract: Many exceptionally preserved fossils have long been thought the product of preservation by bacterial autolithification, based largely upon the presence of, micron-sized, spherical or elongate bodies on their surface. This has recently been challenged by studies of similar fossils which cite morphological and geochemical evidence that these structures could be fossilized melanosomes, melanin-containing organelles. We geochemically analysed a tadpole from the Oligocene Enspel Formation, Germany, which displays such spherical bodies on its surface. Pyrolysis gas chromatography mass spectroscopy (Py-GCMS) and Fourier transform infrared spectrometry (FTIR) indicate that the organic remains of the tadpole are original and are not the result of external contamination, shown by the different chemical compositions of the fossil and its enclosing matrix. Py-GCMS also demonstrates the presence of bacterial and plant biomarkers in the matrix but not the tadpole, suggesting that the spherical bodies are unlikely to be bacterial, and also that such fossils do not develop their dark colour from incorporating plant material, as has been suggested. X-ray absorption spectroscopy (XAS) shows high levels of organically bound Zn(II) in the fossilized soft tissue, a metal known to chelate both eu- and pheomelanin. The zinc in the tadpole shows greater similarity to that bound in pheomelanized extant samples than to that in eumelanized ones. Though further geochemical analysis of both pure pheomelanin and bacterial samples is required to completely exclude a bacterial origin, these results are in line with a pheomelanic origin for the spherical bodies on the tadpole.	Nov 2014
I18-Microfocus Spectroscopy	The mapping and differentiation of biological and environmental elemental signatures in the fossil remains of a 50 million year old bird Victoria Egerton , Roy A. Wogelius , Mark A. Norell , Nicholas Edwards , William Sellers , Uwe Bergmann , Dimosthenis Sokaras , Roberto Alonso-Mori , Konstantin Ignatyev , Arjen Van Veelen , Jennifer Anné , Bart Van Dongen , Fabien Knoll , Phillip Manning Journal Of Analytical Atomic Spectrometry DOI: 10.1039/C4JA00395K Diamond Proposal Number(s): [8597, 9488] Open Access Show Abstract ▼ Abstract: The preservation of fossils reflects the interplay of inorganic and organic chemical processes, which should be clearly differentiated to make interpretations about the biology of extinct organisms. A new coliiformes bird (mouse bird) from the [similar]50 million year old Green River Formation (Wyoming, USA) has here been analysed using synchrotron X-ray fluorescence and environmental scanning electron microscopy with an attached X-ray energy dispersive system (ESEM-EDS). The concentration and distribution of 16 elements (Si, P, S, Cl, K, Ca, Ti, Mg, Fe, Ni, Cu, Zn, As, Br, Ba, Hg) has been mapped for individual points on the sample. S, Cu and Zn map distinctly within visibly preserved feathers and X-ray Absorption Spectroscopy (XAS) shows that S and Cu within the feathers are organically bound in a similar manner to modern feathers. The morphological preservation of the feathers, on both macro- and microscopic scales, is variable throughout the fossil and the differences in the lateral microfacies have resulted in a morphological preservation gradient. This study clearly differentiates endogenous organic remains from those representing exogenous overprinted geochemical precipitates and illustrates the chemical complexity of the overall taphonomic process.	Jan 2015

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