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  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Peptides. ; Solvation. ; Hydrogen bonding. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (313 pages)
    Edition: 1st ed.
    ISBN: 9780080463568
    Series Statement: Issn Series
    DDC: 572.6533
    Language: English
    Note: Cover page -- Contents -- New Directions in the Study of Peptide H-Bonds and.Peptide Solvation -- Chapter 1: Potential Functions for Hydrogen Bonds in Protein Structure Prediction and Design -- I. Introduction -- II. Physical Mechanism of Hydrogen Bond Formation -- III. Main Approaches to Modeling Hydrogen Bonds in Biomolecular Simulations -- A. Potentials Derived from Hydrogen Bonding Geometries Observed in Crystal Structures -- B. Molecular Mechanics: Comparison with the Structure-Derived, Orientation-Dependent Potential -- C. Quantum Mechanics: Comparison with Molecular Mechanics and the Structure-Derived Potential -- IV. Applications of Hydrogen Bonding Potentials -- A. Protein Structure Prediction and Refinement -- B. Prediction of Protein-Protein Interfaces -- C. Protein Design -- V. Conclusions and Perspectives -- References -- Chapter 2: Backbone-Backbone H-Bonds Make Context-Dependent Contributions to Protein Folding Kinetics and Thermodynamics: Lessons from Amide-to-Ester Mutations -- I. Introduction -- II. Nomenclature and Synthesis of Amide-to-Ester Mutants -- III. Esters as Amide Replacements -- A. Geometry and Conformation -- B. Structural Effects of Amide-to-Ester Mutations -- IV. Interpretation of Energetic Data from Amide-to-Ester Mutants -- A. H-Bond Energies and the Thermodynamic Analysis of Amide-to-Ester Mutants -- B. Kinetic Analysis of Amide-to-Ester Mutants -- V. Amide-to-Ester Mutations in Studies of Protein Function -- VI. Amide-to-Ester Mutations in Studies of Protein Folding Thermodynamics -- VII. Analysis of DeltaDeltaGb and DeltaDeltaGf Values from Amide-to-Ester Mutants -- A. General Observations -- B. Quantitative Analysis of DeltaDeltaGf/b Values -- VIII. Amide-to-Ester Mutations in Studies of Protein Folding Kinetics -- IX. Conclusions and Future Directions -- References. , Chapter 3: Modeling Polarization in Proteins and Protein-ligand Complexes: Methods and Preliminary Results -- I. Introduction -- II. Incorporation of Polarization in Molecular Mechanics Models -- A. Overview -- B. Development of the OPLS/PFF Force Field -- C. Simulation Methodology -- D. Evaluation of the Polarizable Force Field in the Gas Phase and Condensed Phase -- III. Aqueous Solvation Models for Polarizable Simulations -- A. Overview -- B. Polarizable Explicit Water Models -- IV. Modeling Polarizability with Mixed Quantum Mechanics/Molecular Mechanics Methods -- A. Overview -- B. Protein-Ligand Docking Using a Mixed Mixed Quantum Mechanics/Molecular Mechanics Methodology to Compute Ligand Charges -- V. Protein Simulations in Explicit Solvent Using a Polarizable Force Field -- A. Overview -- B. Simulations of BPTI with Polarizable and Fixed Charge Protein and Water Models -- VI. Conclusion -- References -- Chapter 4: Hydrogen Bonds In Molecular Mechanics Force Fields -- I. Introduction -- II. Geometric Deformation -- III. Nonbonded Interactions -- IV. Conclusion -- References -- Chapter 5: Resonance Character of Hydrogen-bonding Interactions in Water and Other H-bonded Species -- I. Introduction -- II. Natural Bond Orbital Donor-Acceptor Description of H-Bonding -- III. Quantum Cluster Equilibrium Theory of H-Bonded Fluids -- IV. Recent Experimental Advances in Determining Water Coordination Structure -- V. General Enthalpic and Entropic Principles of H-Bonding -- A. Torsional, Angular, and Dissociative Entropic Contributions -- B. Binary and Cooperative Enthalpic Contributions -- VI. Hydrophobic Solvation: A Cluster Equilibrium View -- VII. Summary and Conclusions: The Importance of Resonance in H-Bonding and Its Possible Representation by Molecular Dynamics Simulations -- References. , Chapter 6: How hydrogen bonds shape membrane protein structure -- I. Introduction -- II. Structure of Fluid Lipid Bilayers -- III. Energetics of Peptides in Bilayers -- A. Folding in the Membrane Interface -- B. Transmembrane Helices -- IV. Helix-Helix Interactions in Bilayers -- V. Perspectives -- References -- Chapter 7: Peptide and Protein Folding and Conformational Equilibria: Theoretical Treatment of Electrostatics and Hydrogen Bonding with Implicit Solvent Models -- I. Introduction -- II. Generalized Born (GB) Models -- A. GB Electrostatics Theory -- B. Advances and Achievements -- C. Remaining Opportunities for Continued Improvement -- III. Peptide Folding and Conformational Equilibria -- A. Influence of Backbone H-Bond Strength on Conformational Equilibria -- B. Influence of Backbone Dihedral Energetics on Conformational Equilibria -- IV. Concluding Discussion -- References -- Chapter 8: Thermodynamics Of alpha-Helix Formation -- I. First 50 Years of Study of the Thermodynamics of the Helix-Coil Transition -- II. The Quest for Enthalpy of the Helix-Coil Transition -- III. Temperature Dependence of Enthalpy of the Helix-Coil Transition -- IV. Thermodynamic Helix Propensity Scale: Importance of Peptide Backbone Hydration -- V. Other Instances When Peptide Backbone Hydration is Important for Stability -- VI. Future Directions -- References -- Chapter 9: The Importance of Cooperative Interactions and a Solid-State Paradigm to Proteins: What Peptide Chemists Can Learn from Molecular Crystals -- I. Introduction -- II. Similarities and Differences Between Proteins/Peptides and Molecular Crystals -- A. Similarities -- B. Differences -- III. The Importance of H-Bond Cooperativity in Molecular Crystals -- A. Enthalpy Is Relatively More Important in the Solid Than in the Liquid -- B. H-Bonds Are More Stable in the Solid Than in the Liquid State. , IV. Structural Consequences of H-Bond Cooperativity in Molecular Crystals -- A. Acetic Acid -- B. 1,3-Cyclohexanedione -- C. Urea -- D. Formamide -- E. CH...O H-Bonding Interactions and Parabenzoquinone -- V. How Does the Use of the Crystal Paradigm Affect Protein/Peptide Study? -- A. Low-Barrier H-Bonds -- VI. Are H-Bonds Electrostatic? -- A. Water-Water H-Bonding Cannot be Described Adequately Purely by Electrostatic Interactions -- B. Comparison of H-Bonds with the Behavior of Molecules in an Electric Field -- VII. How Strong are Peptide H-Bonds? -- A. Amide Dimers -- B. Formamide Chains -- C. alpha-Helices -- D. Protonated alpha-Helices -- E. beta-Sheets -- F. Collagen-like Triple Helices -- VIII. Comparison with Experimental Data from Studies in Solution -- A. alpha-Helices -- IX. The Importance of a Suitable Reference State(s) -- A. Differences between Reference States for Experimental and Theoretical Studies -- B. Multiple Reference States -- C. Component Amino Acids -- D. Extended beta-Strand -- E. Choosing More Than One Reference State -- X. How Protein Chemists Can Deal with Problems Posed by Dual Paradigms -- A. Theoretical and Modeling Studies -- B. Experimental Studies -- XI. Water, the Hydrophobic Effect and Entropy -- A. Water -- B. The Hydrophobic Effect and Entropy -- C. Another Origin of Entropy Control of Protein Folding -- XII. Concluding Remarks -- References -- Author Index -- Subject Index.
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2008. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 113 (2008): G01010, doi:10.1029/2007JG000408.
    Description: Seasonal and interannual variability in atmospheric carbon dioxide (CO2) concentrations was simulated using fluxes from fossil fuel, ocean and terrestrial biogeochemical models, and a tracer transport model with time-varying winds. The atmospheric CO2 variability resulting from these surface fluxes was compared to observations from 89 GLOBALVIEW monitoring stations. At northern hemisphere stations, the model simulations captured most of the observed seasonal cycle in atmospheric CO2, with the land tracer accounting for the majority of the signal. The ocean tracer was 3–6 months out of phase with the observed cycle at these stations and had a seasonal amplitude only ∼10% on average of observed. Model and observed interannual CO2 growth anomalies were only moderately well correlated in the northern hemisphere (R ∼ 0.4–0.8), and more poorly correlated in the southern hemisphere (R 〈 0.6). Land dominated the interannual variability (IAV) in the northern hemisphere, and biomass burning in particular accounted for much of the strong positive CO2 growth anomaly observed during the 1997–1998 El Niño event. The signals in atmospheric CO2 from the terrestrial biosphere extended throughout the southern hemisphere, but oceanic fluxes also exerted a strong influence there, accounting for roughly half of the IAV at many extratropical stations. However, the modeled ocean tracer was generally uncorrelated with observations in either hemisphere from 1979–2004, except during the weak El Niño/post-Pinatubo period of the early 1990s. During that time, model results suggested that the ocean may have accounted for 20–25% of the observed slowdown in the atmospheric CO2 growth rate.
    Description: We acknowledge the support of NASA grant NNG05GG30G and NSF grant ATM0628472.
    Keywords: Atmospheric CO2 ; Interannual variability ; Seasonal cycles ; Transport model
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/postscript
    Format: application/pdf
    Format: text/plain
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  • 3
    Publication Date: 2022-05-25
    Description: Author Posting. © Blackwell, 2006. This is the author's version of the work. It is posted here by permission of Blackwell for personal use, not for redistribution. The definitive version was published in Tellus B 58 (2006):359-365, doi:10.1111/j.1600-0889.2006.00218.x.
    Description: The sources and sinks of important climatic trace gases such as carbon dioxide (CO2) are often deduced from spatial and temporal variations in atmospheric concentrations. Reducing uncertainties in our understanding of the contemporary carbon budget and its underlying dynamics, however, requires significantly denser observations globally than is practical with in situ measurements. Space-based measurements appear technically feasible but require innovations in data analysis approaches. We develop a variational data assimilation scheme to estimate surface CO2 fluxes at fine time/space scales from such dense atmospheric data. Global flux estimates at a daily time step and model-grid spatial resolution (4° × 5° here) are rapidly achieved after only a few dozen minimization steps. We quantify the flux errors from existing, planned and hypothetical surface and space-borne observing systems. Simulations show that the planned NASA Orbital Carbon Observatory (OCO) satellite should provide significant additional information beyond that from existing and proposed in situ observations. Improvements in data assimilation techniques and in mechanistic process models are both needed to fully exploit the emerging global carbon observing system.
    Description: This work was made possible through support from the Office of Global Programs (OGP) of the National Atmospheric and Oceanographic Administration (NOAA) (Grant NA16GP2935 at NCAR, NA16GP2008 at WHOI). NCAR is sponsored by the National Science Foundation.
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: 2208648 bytes
    Format: application/pdf
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  • 4
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2008. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Global Biogeochemical Cycles 22 (2008): GB3025, doi:10.1029/2007GB003082.
    Description: Interannually varying net carbon exchange fluxes from the TransCom 3 Level 2 Atmospheric Inversion Intercomparison Experiment are presented for the 1980 to 2005 time period. The fluxes represent the model mean, net carbon exchange for 11 land and 11 ocean regions after subtraction of fossil fuel CO2 emissions. Both aggregated regional totals and the individual regional estimates are accompanied by a model uncertainty and model spread. We find that interannual variability is larger on the land than the ocean, with total land exchange correlated to the timing of both El Niño/Southern Oscillation (ENSO) as well as the eruption of Mt. Pinatubo. The post-Pinatubo negative flux anomaly is evident across much of the tropical and northern extratropical land regions. In the oceans, the tropics tend to exhibit the greatest level of interannual variability, while on land, the interannual variability is slightly greater in the tropics and northern extratropics. The interannual variation in carbon flux estimates aggregated by land and ocean across latitudinal bands remains consistent across eight different CO2 observing networks. The interannual variation in carbon flux estimates for individual flux regions remains mostly consistent across the individual observing networks. At all scales, there is considerable consistency in the interannual variations among the 13 participating model groups. Finally, consistent with other studies using different techniques, we find a considerable positive net carbon flux anomaly in the tropical land during the period of the large ENSO in 1997/1998 which is evident in the Tropical Asia, Temperate Asia, Northern African, and Southern Africa land regions. Negative anomalies are estimated for the East Pacific Ocean and South Pacific Ocean regions. Earlier ENSO events of the 1980s are most evident in southern land positive flux anomalies.
    Keywords: Carbon cycle ; Atmospheric inversion ; Interannual variability
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 5
    Publication Date: 2022-05-26
    Description: © The Authors, 2010. This article is distributed under the terms of the Creative Commons Attribution 3.0 License. The definitive version was published in Atmospheric Chemistry and Physics 10 (2010): 4145-4165, doi:10.5194/acp-10-4145-2010.
    Description: We quantify how well column-integrated CO2 measurements from the Orbiting Carbon Observatory (OCO) should be able to constrain surface CO2 fluxes, given the presence of various error sources. We use variational data assimilation to optimize weekly fluxes at a 2°×5° resolution (lat/lon) using simulated data averaged across each model grid box overflight (typically every ~33 s). Grid-scale simulations of this sort have been carried out before for OCO using simplified assumptions for the measurement error. Here, we more accurately describe the OCO measurements in two ways. First, we use new estimates of the single-sounding retrieval uncertainty and averaging kernel, both computed as a function of surface type, solar zenith angle, aerosol optical depth, and pointing mode (nadir vs. glint). Second, we collapse the information content of all valid retrievals from each grid box crossing into an equivalent multi-sounding measurement uncertainty, factoring in both time/space error correlations and data rejection due to clouds and thick aerosols. Finally, we examine the impact of three types of systematic errors: measurement biases due to aerosols, transport errors, and mistuning errors caused by assuming incorrect statistics. When only random measurement errors are considered, both nadir- and glint-mode data give error reductions over the land of ~45% for the weekly fluxes, and ~65% for seasonal fluxes. Systematic errors reduce both the magnitude and spatial extent of these improvements by about a factor of two, however. Improvements nearly as large are achieved over the ocean using glint-mode data, but are degraded even more by the systematic errors. Our ability to identify and remove systematic errors in both the column retrievals and atmospheric assimilations will thus be critical for maximizing the usefulness of the OCO data.
    Description: SD and DB acknowledge support from NASA grant NNG06G127G. DB also acknowledges initial support from NOAA Grant NA16GP2935.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 6
    ISSN: 1546-170X
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Medicine
    Notes: [Auszug] The cannabinoid system is immunomodulatory and has been targeted as a treatment for the central nervous system (CNS) autoimmune disease multiple sclerosis. Using an animal model of multiple sclerosis, experimental autoimmune encephalomyelitis (EAE), we investigated the role of the CB1 and CB2 ...
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1546-170X
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Medicine
    Notes: [Auszug] Accelerated osteoclastic bone resorption has a central role in the pathogenesis of osteoporosis and other bone diseases. Identifying the molecular pathways that regulate osteoclast activity provides a key to understanding the causes of these diseases and to the development of new treatments. Here ...
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The energy-based refinement of low-resolution protein structure models to atomic-level accuracy is a major challenge for computational structural biology. Here we describe a new approach to refining protein structure models that focuses sampling in regions most likely to contain errors while ...
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] There is a clear case for drug treatments to be selected according to the characteristics of an individual patient, in order to improve efficacy and reduce the number and severity of adverse drug reactions. However, such personalization of drug treatments requires the ability to predict how ...
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford, UK : Munksgaard International Publishers
    Journal of clinical periodontology 32 (2005), S. 0 
    ISSN: 1600-051X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Objectives: Periodontal regeneration is contingent on the adsorption, uninterrupted adhesion, and maturation of a fibrin clot to a periodontally compromised root surface. Clot adhesion appears vitally dependent on the formation of a resilient union between the clot and the root surface. Root surface demineralization will remove a root surface smear layer exposing dentin tubules and collagen matrix for enhanced clot adhesion. Recently, protein constructs have been introduced to condition the root during periodontal surgery. The effect of such root conditioning on clot adhesion has not been clarified. The objective of this study was to evaluate clot adhesion to protein conditioned dentin surfaces.Methods: Human dentin blocks (4 × 6 × 1 mm) were exposed to a saturated citric acid solution (CA) or a commercial ethylenediaminetetraacetic acid (EDTA) preparation using standardized protocols. Some dentin blocks were additionally conditioned with proteins, either bovine serum albumin (BSA) or an enamel matrix protein preparation (EMP). Fresh human whole blood was applied to the blocks. The blood was allowed to clot for 20 min. in a humidified chamber. The dentin blocks were rinsed 3 × 5 min. in phosphate-buffered saline under standardized conditions to test clot adhesion. They were then processed for scanning electron microscopy (SEM). Two masked examiners independently evaluated the SEM images.Results: CA removed the dentin smear layer, exposing dentin tubules and collagen. EDTA appeared less efficacious leaving smear layer residues. The BSA or EMP application resulted in a surface morphology similar to that of a smear layer. Fibrin clot adhesion was best supported by the CA-treated dentin surface. Forces produced by the rinse protocol partially removed the fibrin clot from EDTA-treated surfaces. BSA- or EMP-treated surfaces poorly retained the fibrin clot.Conclusions: CA surface demineralization removes a dentin surface smear layer to promote adhesion of a fibrin clot. The EDTA gel appears less effective. Further conditioning of the dentin surface with protein constructs produces a surface morphology similar to that of the smear layer with poor fibrin clot retention.
    Type of Medium: Electronic Resource
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