Deposits of clastic carbonate-dominated (calciclastic) sedimentary slope systems in the rock record have been identified mostly as linearly-consistent carbonate apron deposits, even though most ancient clastic carbonate slope deposits fit the submarine fan systems better. Calciclastic submarine fans are consequently rarely described and are poorly understood. Subsequently, very little is known especially in mud-dominated calciclastic submarine fan systems. Presented in this study are a sedimentological core and petrographic characterisation of samples from eleven boreholes from the Lower Carboniferous of Bowland Basin (Northwest England) that reveals a >250 m thick calciturbidite complex deposited in a calciclastic submarine fan setting. Seven facies are recognised from core and thin section characterisation and are grouped into three carbonate turbidite sequences. They include: 1) Calciturbidites, comprising mostly of highto low-density, wavy-laminated bioclast-rich facies; 2) low-density densite mudstones which are characterised by planar laminated and unlaminated muddominated facies; and 3) Calcidebrites which are muddy or hyper-concentrated debrisflow deposits occurring as poorly-sorted, chaotic, mud-supported floatstones. These

Phd by thesis

J. Appl. Cryst.の発刊に際して

I read this book the same weekend that the Packers took on the Rams, and the experience of the latter event, obviously, colored my judgment. Although I abhor anything that smacks of being a handbook (like, \"How to Earn a Merit Badge in Neurosurgery\") because too many volumes in biomedical science already evince a boyscout-like approach, I must confess that parts of this volume are fast, scholarly, and significant, with certain reservations. I like parts of this well-illustrated book because Dr. Sj6strand, without so stating, develops certain subjects on technique in relation to the acquisition of judgment and sophistication. And this is important! So, given that the author (like all of us) is somewhat deficient in some areas, and biased in others, the book is still valuable if the uninitiated reader swallows it in a general fashion, realizing full well that what will be required from the reader is a modulation to fit his vision, propreception, adaptation and response, and the kind of problem he is undertaking. A major deficiency of this book is revealed by comparison of its use of physics and of chemistry to provide understanding and background for the application of high resolution electron microscopy to problems in biology. Since the volume is keyed to high resolution electron microscopy, which is a sophisticated form of structural analysis, but really morphology in a modern guise, the physical and mechanical background of The instrument and its ancillary tools are simply and well presented. The potential use of chemical or cytochemical information as it relates to biological fine structure , however, is quite deficient. I wonder when even sophisticated morphol-ogists will consider fixation a reaction and not a technique; only then will the fundamentals become self-evident and predictable and this sine qua flon will become less mystical. Staining reactions (the most inadequate chapter) ought to be something more than a technique to selectively enhance contrast of morphological elements; it ought to give the structural addresses of some of the chemical residents of cell components. Is it pertinent that auto-radiography gets singled out for more complete coverage than other significant aspects of cytochemistry by a high resolution microscopist, when it has a built-in minimal error of 1,000 A in standard practice? I don't mean to blind-side (in strict football terminology) Dr. Sj6strand's efforts for what is \"routinely used in our laboratory\"; what is done is usually well done. It's just that …

Methods in Enzymology.

We are just beginning to understand the metabolism of heavy metals and to use their metabolic functions in biotechnology, although heavy metals comprise the major part of the elements in the periodic table. Because they can form complex compounds, some heavy metal ions are essential trace elements, but, essential or not, most heavy metals are toxic at higher concentrations. This review describes the workings of known metal-resistance systems in microorganisms. After an account of the basic principles of homoeostasis for all heavy-metal ions, the transport of the 17 most important (heavy metal) elements is compared.

Microbial heavy-metal resistance

https://publikationen.bibliothek.kit.edu/1000050288/18451059

Renewable Power-to-Gas: A technological and economic review

Cell suspensions of Methanobrevibacter arboriphilus catalyzed the reduction of O2 with H2 at a maximal specific rate of 0.4 U (μmol/min) per mg protein with an apparent Km for O2 of 30 μM. The reaction was not inhibited by cyanide. The oxidase activity was traced back to a coenzyme F420-dependent enzyme that was purified to apparent homogeneity and that catalyzed the oxidation of 2 F420H2 with 1 O2 to 2 F420 and 2 H2O. The apparent Km for F420 was 30 μM and that for O2 was 2 μM with a Vmax of 240 U/mg at 37°C and pH 7.6, the pH optimum of the oxidase. The enzyme did not use NADH or NADPH as electron donor or H2O2 as electron acceptor and was not inhibited by cyanide. The 45-kDa protein, whose gene was cloned and sequenced, contained 1 FMN per mol and harbored a binuclear iron center as indicated by the sequence motif H–X–E–X–D–X62–H–X18–D–X60–H. Sequence comparisons revealed that the F420H2 oxidase from M. arboriphilus is phylogenetically closely related to FprA from Methanothermobacter marburgensis (71% sequence identity), a 45-kDa flavoprotein of hitherto unknown function, and to A-type flavoproteins from bacteria (30–40%), which all have dioxygen reductase activity. With heterologously produced FprA from M. marburgensis it is shown that this protein is also a highly efficient F420H2 oxidase and that it contains 1 FMN and 2 iron atoms. The presence of F420H2 oxidase in methanogenic archaea may explain why some methanogens, e.g., the Methanobrevibacter species in the termite hindgut, cannot only tolerate but thrive under microoxic conditions.

F420H2 oxidase (FprA) from Methanobrevibacter arboriphilus, a coenzyme F420-dependent enzyme involved in O2 detoxification.

https://febs.onlinelibrary.wiley.com/doi/pdf/10.1016/S0014-5793%2800%2902172-4

Learning from hydrogenases: location of a proton pump and of a second FMN in bovine NADH--ubiquinone oxidoreductase (Complex I).

The reduction of the heterodisulfide (CoM-S-S-HTP) of coenzyme M (H-S-CoM) and N-7-mercaptoheptanoylthreonine phosphate (H-S-HTP) with H2 is an energy-conserving step in most methanogenic Archaea. In this study, we show that in Methanobacterium thermoautotrophicum (strain Marburg) this reaction is catalyzed by a stable H2-heterodisulfide oxidoreductase complex of F420-non-reducing hydrogenase and heterodisulfide reductase. This complex, which was loosely associated with the cytoplasmic membrane, was purified 17-fold with 80% yield to apparent homogeneity. The purified complex was composed of six different subunits of apparent molecular masses 80, 51, 41, 36, 21 and 17 kDa, and 1 mol complex, with apparent molecular mass 250 kDa, contained approximately 0.6 mol nickel, 0.9 mol FAD, 26 mol non-heme iron and 22 mol acid-labile sulfur. In 25 mM Chaps, the complex partially dissociated into two subcomplexes. The first subcomplex was was composed of the 51-, 41- and 17-kDa subunits; 1 mol trimer contained 0.7 mol nickel, 10 mol non-heme iron and 9 mol acid-labile sulfur and exhibited F420-non-reducing hydrogenase activity. The other subcomplex was composed of the 80-, 36- and 21-kDa subunits; 1 mol trimer contained 0.8 mol FAD, 22 mol non-heme iron and 15 mol acid-labile sulfur and exhibited heterodi-sulfide-reductase activity. The stimulatory effects of potassium phosphate, a membrane component, uracil derivatives and coenzyme F430 on the H2:heterodisulfide-oxidoreductase activity of the purified complex are described.

H2: heterodisulfide oxidoreductase complex from Methanobacterium thermoautotrophicum. Composition and properties.

Heterodisulfide reductase (HDR) from methanogenic archaea is an iron-sulfur protein that catalyzes reversible reduction of the heterodisulfide (CoM-S-S-CoB) of the methanogenic thiol-coenzymes, coenzyme M (CoM-SH) and coenzyme B (CoB-SH). Via the characterization of a paramagnetic reaction intermediate generated upon oxidation of the enzyme in the presence of coenzyme M, the enzyme was shown to contain a [4Fe-4S] cluster in its active site that catalyzes reduction of the disulfide substrate in two one-electron reduction steps. The formal thiyl radical generated by the initial one-electron reduction of the disulfide is stabilized via reduction and coordination of the resultant thiol to the [4Fe-4S] cluster.

/pdf/heterodisulfide-reductase-from-methanogenic-archaea-a-new-697xh31iht.pdf

Heterodisulfide reductase from methanogenic archaea: a new catalytic role for an iron-sulfur cluster.

F420-non-reducing hydrogenase (Mvh) from Methanothermobacter marburgensis is a [NiFe] hydrogenase composed of the three subunits MvhA, MvhG, and MvhD. Subunits MvhA and MvhG form the basic hydrogenase module conserved in all [NiFe] hydrogenases, whereas the 17-kDa MvhD subunit is unique to Mvh. The function of this extra subunit is completely unknown. In this work, the physiological function of this hydrogenase, and in particular the role of the MvhD subunit, is addressed. In cells of Mt. marburgensis
from Ni2+-limited chemostat cultures the amount of Mvh decreased about 70-fold. However, the amounts of mvh transcripts did not decrease in these cells as shown by competitive RT-PCR, arguing against a regulation at the level of transcription. In cells grown in the presence of non-limiting amounts of Ni2+, Mvh was found in two chromatographically distinct forms—a free form and in a complex with heterodisulfide reductase. In cells from Ni2+-limited chemostat cultures, Mvh was only found in a complex with heterodisulfide reductase. The EPR spectrum of the purified enzyme reduced with sodium dithionite was dominated by a signal with g 
zyx
 =2.006, 1.936 and 1.912. The signal could be observed at temperatures up to 80 K without broadening, indicative of a [2Fe–2S] cluster. Subunit MvhD contains five cysteine residues that are conserved in MvhD homologues of other organisms. Four of these conserved cysteine residues can be assumed to coordinate the [2Fe–2S] cluster that was detected by EPR spectroscopy. The MvhG subunit contains 12 cysteine residues, which are known to ligate three [4Fe–4S] clusters. Data base searches revealed that in some organisms, including the Methanosarcina species and Archaeoglobus fulgidus, a homologue of mvhD is fused to the 3′ end of an hdrA
homologue, which encodes a subunit of heterodisulfide reductase. These data allow the conclusion that the only function of Mvh is to provide reducing equivalents for heterodisulfide reductase and that the MvhD subunit is an electron transfer protein that forms the contact site to heterodisulfide reductase.

Reiner Hedderich

Papers

F420H2 oxidase (FprA) from Methanobrevibacter arboriphilus, a coenzyme F420-dependent enzyme involved in O2 detoxification.

Learning from hydrogenases: location of a proton pump and of a second FMN in bovine NADH--ubiquinone oxidoreductase (Complex I).

H2: heterodisulfide oxidoreductase complex from Methanobacterium thermoautotrophicum. Composition and properties.

Heterodisulfide reductase from methanogenic archaea: a new catalytic role for an iron-sulfur cluster.

Physiological role of the F420-non-reducing hydrogenase (Mvh) from Methanothermobacter marburgensis