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Abstract: Fossils of juvenile Mesozoic birds provide insight into the early evolution of avian development, however such fossils are rare. The analysis of the ossification sequence in these early-branching birds has the potential to address important questions about their comparative developmental biology and to help understand their morphological evolution and ecological differentiation. Here we report on an early juvenile enantiornithine specimen from the Early Cretaceous of Europe, which sheds new light on the osteogenesis in this most species-rich clade of Mesozoic birds. Consisting of a nearly complete skeleton, it is amongst the smallest known Mesozoic avian fossils representing post-hatching stages of development. Comparisons between this new specimen and other known early juvenile enantiornithines support a clade-wide asynchronous pattern of osteogenesis in the sternum and the vertebral column, and strongly indicate that the hatchlings of these phylogenetically basal birds varied greatly in size and tempo of skeletal maturation.

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Abstract: Iron sulfur (Fe–S) phases have been implicated in the emergence of life on early Earth due to their catalytic role in the synthesis of prebiotic molecules. Similarly, Fe–S phases are currently of high interest in the development of green catalysts and energy storage. Here we report the synthesis and structure of a nanoparticulate phase (FeSnano) that is a necessary solid-phase precursor to the conventionally assumed initial precipitate in the iron sulfide system, mackinawite. The structure of FeSnano contains tetrahedral iron, which is compensated by monosulfide and polysulfide sulfur species. These together dramatically affect the stability and enhance the reactivity of FeSnano.

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Abstract: Measuring the low bromine abundances in Earth’s materials remains an important challenge in order to constrain the geodynamical cycle of this element. Suitable standard materials are therefore required to establish reliable analytical methods to quantify Br abundances. In this study we characterise 21 Br-doped glasses synthesized from natural volcanic rocks of mafic to silicic compositions, in order to produce a new set of standards for Br analyses using various techniques. The nominal Br contents (amounts of Br loaded in the experimental samples) of 15 of 21 glasses were confirmed within 20% by instrumental neutron activation analysis (INAA). Using this new set of standards, we compare three micro-analytical approaches to measure Br contents in silicate glasses: synchrotron X-ray fluorescence (SR-XRF), laser ablation-inductively coupled plasma mass spectrometry (LA-ICP-MS), and secondary ion mass spectrometry (SIMS). With SR-XRF, the Br contents of the standard glasses were determined with the highest accuracy (< 10% for Br ≥ 10 ppm; > 25% for Br ≤ 5 ppm), and high precision (< 10% for Br contents > 10 ppm; 20-30% for Br ≤ 10 ppm). The detection limit was estimated to be less than 1 ppm Br. All those factors combined with a high spatial resolution (5x5 μm for the presented measurements), means that SR-XRF is well suited to determine the low Br abundance in natural volcanic glasses (crystal-hosted melt inclusions or matrix glasses of crystallized samples). At its current stage of development, the LA-ICP-MS method allows the measurement of hundreds to thousands ppm Br in silicate glasses with a precision and accuracy generally within 20 %. The Br detection limit of this method has not been estimated but its low spatial resolution (90 μm) currently prevents its use to characterise natural volcanic glasses, however it is fully appropriate to analyse super liquidus or sparsely phyric, Br-rich experimental charges. Our study shows that SIMS appears to be a promising technique to measure the low Br contents of natural volcanic glasses. Its spatial resolution is relatively good (~ 15 μm) and, similarly to SR-XRF, the detection limit is estimated to be ≤ 1 ppm. Using our new set of standards, the Br contents of two MPI-DING reference glasses containing less than 1.2 ppm of Br were reproduced with precision < 5% and accuracy < 20%. Moreover, SIMS presents the advantage of being a more accessible instrument than SR-XRF and data processing is more straightforward.

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Abstract: The first experimental results from a new transmissive diagnostic instrument for synchrotron X-ray beamlines are presented. The instrument utilizes a single-crystal chemical-vapour-deposition diamond plate as the detector material, with graphitic wires embedded within the bulk diamond acting as electrodes. The resulting instrument is an all-carbon transmissive X-ray imaging detector. Within the instrument's transmissive aperture there is no surface metallization that could absorb X-rays, and no surface structures that could be damaged by exposure to synchrotron X-ray beams. The graphitic electrodes are fabricated in situ within the bulk diamond using a laser-writing technique. Two separate arrays of parallel graphitic wires are fabricated, running parallel to the diamond surface and perpendicular to each other, at two different depths within the diamond. One array of wires has a modulated bias voltage applied; the perpendicular array is a series of readout electrodes. X-rays passing through the detector generate charge carriers within the bulk diamond through photoionization, and these charge carriers travel to the nearest readout electrode under the influence of the modulated electrical bias. Each of the crossing points between perpendicular wires acts as an individual pixel. The simultaneous read-out of all pixels is achieved using a lock-in technique. The parallel wires within each array are separated by 50 µm, determining the pixel pitch. Readout is obtained at 100 Hz, and the resolution of the X-ray beam position measurement is 600 nm for a 180 µm size beam.

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Abstract: This thesis reports a study of the sulfur problem which is the production of sulfuric acid via the oxidation of iron sulfide in the timbers of the Mary Rose a flagship of Henry VIII 's navy which sunk in 1535 and was raised in 1982. The work has involved a range of chemical and physical techniques with particular use of synchrotron sources to measure the iron and sulfur speciation in the timbers with X-ray absorption spectroscopy (XAS) measurements. XAS measurements are almost unique in providing the speciation of atoms in a sample via the XANES. They are particularly useful for sulfur, which has a wide range of oxidation states. However, the current work has shown the need to use the bulk and microfocus XAS measurements in parallel, particularly for archaeological samples. It is clear that the iron and sulfur contents and speciation can vary widely from sample to sample of the Mary Rose timbers. In the study on the effectiveness of chelating agents in the removal of iron species from the timbers care was taken, wherever possible, to ensure that the same samples and sample positions were used for the before and after treatment measurements. The nature of the iron and su~ur species is of extreme importance because it is assumed that it is Fe" that gives rise to the production of su~uric acid. The current study has shown that in the timbers that had not been PEG treated contained iron in the surface regions that was predominantly Fe", similar to the findings of other workers. Most of the work in this thesis used samples close to the surface of the timbers. It was only in samples taken deep into the timbers experiments that there were significant concentrations of Fe". A range of sulfur species were found in the samples. The predominant species were reduced sulfur species, elemental sulfur and sulfate. Very little pyrite was found -in the timbers studied, but it should be noted that these timbers had not been PEG treated. Some pyrite was found in the cell walls. The present studies were predominantly on the surface regions of the timbers and the conclusion is that the bulk of the pyrite which may have been present had oxidised in the moist, oxygen containing environment in which they had been stored after recovery from the sea bed. A key finding of the present study is the co-location of iron and sulfate in the timbers. This had been suggested but had not been experimentally verified. The production of sulfuric acid in the timbers is thought to involve the oxidation of iron sulfides in the presence of water to produce is iron sulfate and sulfuric acid. The fact that the present experiments show iron and sulfate in the same positions i'] the XANES maps strongly supports the proposed oxidation mechanism of iron sulfides. The bulk and microfocus XAS experiments show that a large fraction of the iron in the current samples was in the form of an oxide. This is most likely to be goethite (FeO(OH)). The XANES analysis and the fitting of the EXAFS are consistent with this identification. All the four chelating agents used in this work (EDTA, DTPA, ammonium citrate and calcium phytate) were effective in removing iron from the timbers. However, the more efficient are DTPA and calcium phytate in terms of amount removed at fixed molarity. For samples that had been treated with PEG the current work showed that the chelating agents were less effective. This is presumably due to the PEG blocking the penetration of the solutions of the chelating agents into the wood.