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  • 1
    Online Resource
    Online Resource
    Singapore :Springer,
    Keywords: Bones-Diseases-Genetic aspects. ; Non-coding RNA. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (186 pages)
    Edition: 1st ed.
    ISBN: 9789811624025
    DDC: 572.88
    Language: English
    Note: Intro -- Preface -- Contents -- Part I: MicroRNAs and Bone -- Chapter 1: MicroRNAs and Osteoporosis -- 1.1 Introduction -- 1.2 MiRNAs Involved in the Regulation of Osteoblasts -- 1.3 MiRNAs Involved in the Regulation of Osteoclasts -- 1.4 MiRNAs Involved in the Regulation of Bone-Related Signaling Pathways -- 1.4.1 MiRNAs Involved in the Regulation of Wnt Signaling Pathway -- 1.4.2 MiRNAs Involved in the Regulation of BMP Signaling Pathway -- 1.4.3 MiRNAs Involved in the Regulation of TGF-β Signaling Pathway -- 1.4.4 MiRNAs Involved in the Regulation of RANK/RANKL/OPG Signaling Pathway -- 1.4.5 MiRNAs Involved in the Regulation of M-CSF/c-FMS Signaling Pathway -- 1.5 Conclusion and Future Perspectives -- References -- Chapter 2: MicroRNAs and the Diagnosis of Osteoporosis -- 2.1 Introduction -- 2.2 General Overview of miRNAs as Biomarkers for Different Types of Osteoporosis -- 2.2.1 miRNAs as Diagnostic Biomarkers in Primary Osteoporosis -- 2.2.1.1 miRNAs and Postmenopausal Osteoporosis -- 2.2.1.2 miRNAs and Senile Osteoporosis -- 2.2.2 miRNAs as Diagnostic Biomarkers in Secondary Osteoporosis -- 2.2.2.1 miRNAs and Drug-Induced Osteoporosis -- 2.2.2.2 miRNAs and Disuse Osteoporosis -- 2.3 Application of miRNAs in the Diagnosis of Osteoporosis and Osteoporotic Fracture Risk Assessment -- 2.4 Advantages and Disadvantages of miRNAs as Novel Biomarker Compared to the Conventional Methods for Osteoporosis Diagnosis -- 2.5 Clinical Status of miRNAs as Diagnostic Markers -- 2.6 Conclusion -- References -- Chapter 3: MicroRNAs and Osteoarthritis -- 3.1 Introduction -- 3.2 MicroRNAs and Chondrocytes -- 3.3 miRNAs and the Degenerative Changes of Extracellular Matrix of Articular Cartilage -- 3.4 miRNAs and Chondrocyte Inflammation -- 3.5 miRNAs and Joint Pain -- 3.6 microRNA Regulatory Pathways in OA -- 3.6.1 NF-κB Signaling Pathway. , 3.6.2 TGF-β Signaling Pathway -- 3.6.3 Wnt Signaling Pathway -- 3.6.4 PI3K/Akt Pathway -- 3.6.5 p53 Signaling Pathway -- 3.7 Early Diagnosis and Treatment Using microRNAs -- 3.7.1 miRNAs and Osteoarthritis Diagnosis -- 3.7.2 miRNAs and Osteoarthritis Treatment -- 3.8 Conclusion -- References -- Chapter 4: Mechanosensitive MicroRNAs and Bone Formation -- 4.1 Introduction -- 4.2 Mechanosensitive miRNAs and Osteogenic Differentiation -- 4.2.1 Mechanosensitive miRNAs Promoted Osteogenic Differentiation -- 4.2.2 Mechanosensitive miRNAs Inhibited Osteogenic Differentiation -- 4.3 Mechanosensitive miRNAs and Osteoblast Proliferation -- 4.4 Mechanosensitive miRNAs and Bone Formation -- 4.5 Conclusions -- References -- Part II: Long Noncoding RNAs and Bone -- Chapter 5: Roles and Mechanism of Long Noncoding RNAs in Bone Diseases -- 5.1 Introduction of lncRNA -- 5.2 LncRNAs and Bone Cells -- 5.2.1 LncRNAs and Osteoblasts (OBs) -- 5.2.2 LncRNAs and Osteoclasts (OCs) -- 5.2.3 LncRNAs and Osteocytes (OCY) -- 5.2.4 LncRNA in Chondrocytes -- 5.3 LncRNAs and Bone Diseases -- 5.3.1 LncRNAs and Osteosarcoma (OS) -- 5.3.2 LncRNAs and Osteoporosis (OP) -- 5.3.3 LncRNAs and Osteoarthritis (OA) -- 5.3.4 LncRNA in Other Bone Related Diseases -- 5.4 Mechanisms of lncRNAs Involved in Bone Diseases -- 5.4.1 LncRNAs and MicroRNAs -- 5.4.1.1 miRNAs Triggering lncRNAs to Decay -- 5.4.1.2 LncRNAs Generating miRNAs -- 5.4.1.3 lncRNAs Binding miRNAs to Derepress mRNAs -- 5.4.2 LncRNAs Bind the mRNAs to Degrade/Stabilize Them -- 5.4.3 Natural Antisense Transcripts -- 5.4.4 LncRNAs and Transcription Factor/Signal Pathways -- 5.5 Conclusions and Perspectives -- References -- Chapter 6: Long Noncoding RNAs Regulate Osteoblast Function and Bone Formation -- 6.1 Introduction -- 6.2 Obstacle on Osteogenic lncRNA Researches -- 6.3 Screening of Osteogenic lncRNAs. , 6.4 Osteogenic lncRNA Researches In Vivo -- 6.5 Mechanism Researches of Osteogenic lncRNAs -- 6.6 Osteogenic lncRNA as Endogenous miRNA Sponge -- 6.7 Conclusion -- References -- Part III: RNA Synthesis Technology and RNA Therapy in Bone Diseases -- Chapter 7: Synthetic Technology of Noncoding RNAs Used in Bone Disease Research and Therapeutics -- 7.1 Introduction -- 7.2 Viral Vector Mediated RNA Therapy -- 7.3 Chemical Synthesis of RNA Molecules and Their Applications in Bone Disease Therapy -- 7.4 In Vivo Production of RNA Molecules and Their Applications in Bone Disease Therapy -- 7.5 Conclusion -- References -- Chapter 8: RNA Therapy in Bone Diseases -- 8.1 Introduction -- 8.2 The Therapeutics of ncRNA to Osteoarthritis -- 8.3 The Therapeutics of ncRNAs to Osteoporosis -- 8.3.1 The Therapy of miRNA to Osteoporosis -- 8.3.2 The Therapy of LncRNA and siRNA to Osteoporosis -- 8.4 The Therapeutics of ncRNA to Bone Tumor -- 8.4.1 The Therapy of ncRNA to Primary Bone Tumors -- 8.4.2 The Therapy of ncRNA to Metastatic Bone Tumors -- 8.5 Conclusion -- References.
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  • 2
    ISSN: 1471-4159
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Abstract: Three chimeric receptors were constructed by exchanging exons between human neurokinin NK1 and NK3 receptor genes. The N-terminal sequences of these chimeric receptors are encoded by exon 1, exon 1–2, or exon 1–3 of the NK1 receptor gene, whereas the remaining C-terminal sequences of these chimeric receptors are encoded by corresponding exons of the human NK3 receptor gene. Substance P bound with high affinities to all three chimeric receptors, suggesting that in addition to the common structures composed of conserved amino acid residues among neurokinin receptors, structural elements encoded by the first exon of the human NK1 receptor gene may also play an important role for substance P binding. On the contrary, potent NK1 antagonists L703,606 and SR140,333 did not show any detectable binding to these chimeric receptors. In accordance, sequences encoded by exon 4, and possibly exon 5, are likely to contain important structural motifs that may directly or indirectly influence the binding of these antagonists. Further comparison of the binding affinities of highly selective NK1 agonists, [Sar9,Met(O2)11]substance P, substance P methyl ester, and septide, revealed that each agonist may interact differently with the human NK1 receptor. These results show that the exon-exchanging technique can be a useful tool for studying structure-function relationships of receptors in which exon-intron junctions are fully conserved among receptor subtypes.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Acta mathematica sinica 16 (2000), S. 229-236 
    ISSN: 1000-9574
    Keywords: Key words Elliptic curve, BSD conjecture, Graph, 2-component ; 1991MR Subject Classification 14H52
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mathematics
    Notes: Abstract We prove in this paper that the BSD conjecture holds for a certain kind of elliptic curves.
    Type of Medium: Electronic Resource
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  • 4
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    PANGAEA
    In:  Supplement to: Tian, Ye; Xue, Chao; Liu, Chun-Ying; Yang, Gui-Peng; Li, Pei-Feng; Feng, Wei-Hua; Bange, Hermann Werner (2019): Nitric oxide (NO) in the Bohai Sea and the Yellow Sea. Biogeosciences, 16(22), 4485-4496, https://doi.org/10.5194/bg-16-4485-2019
    Publication Date: 2023-01-13
    Description: Here we present the measurements of dissolved NO in the surface and bottom layers at 75 stations in the Bohai Sea (BS) and Yellow Sea (YS) in June 2011. The NO concentrations in the surface and bottom layers were highly variable and ranged from below the detection limit (i.e. 32 pmol L-1) to 616 pmol L-1 in the surface layer and to 482 pmol L−1 in the bottom layer. There was no significant difference between the mean NO concentrations in the surface (186 ± 108 pmol L-1) and bottom (174 ± 123 pmol L-1) layers.
    Keywords: BS_YS_B01; BS_YS_B03; BS_YS_B05; BS_YS_B07; BS_YS_B09; BS_YS_B10; BS_YS_B12; BS_YS_B13; BS_YS_B14; BS_YS_B15; BS_YS_B17; BS_YS_B18; BS_YS_B19; BS_YS_B21; BS_YS_B22; BS_YS_B23; BS_YS_B25; BS_YS_B27; BS_YS_B28; BS_YS_B30; BS_YS_B32; BS_YS_B33; BS_YS_B35; BS_YS_B38; BS_YS_B39; BS_YS_B40; BS_YS_B42; BS_YS_B43; BS_YS_B45; BS_YS_B47; BS_YS_B49; BS_YS_B50; BS_YS_B51; BS_YS_B52; BS_YS_B55; BS_YS_B56; BS_YS_B59; BS_YS_B65; BS_YS_B66; BS_YS_B68; BS_YS_B70; BS_YS_B71; BS_YS_BY03; BS_YS_BY04; BS_YS_H01; BS_YS_H03; BS_YS_H05; BS_YS_H07; BS_YS_H08; BS_YS_H09; BS_YS_H10; BS_YS_H11; BS_YS_H13; BS_YS_H15; BS_YS_H17; BS_YS_H19; BS_YS_H20; BS_YS_H21; BS_YS_H23; BS_YS_H25; BS_YS_H27; BS_YS_H29; BS_YS_H30-1; BS_YS_H31; BS_YS_H32; BS_YS_H33; BS_YS_H35; BS_YS_H36; BS_YS_H37; BS_YS_H38; BS_YS_H39; BS_YS_H41; BS_YS_H42; BS_YS_H44; BS_YS_HF1; Chlorophyll a; CTD, Seabird; CTD-R; Date/Time of event; DEPTH, water; Event label; Illuminance; Latitude of event; Longitude of event; nitric oxide; Nitric oxide; Oxygen; Salinity; Station label; Temperature, water; Western Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 805 data points
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  • 5
    Publication Date: 2020-02-06
    Description: We developed a new method for the determination of dissolved nitric oxide (NO) in discrete seawater samples based on the combination of a purge-and-trap setup and a fluorometric detection of NO. 2,3-diaminonaphthalene (DAN) reacts with NO in seawater to form the highly fluorescent 2,3-naphthotriazole (NAT). The fluorescence intensity was linear for NO concentrations in the range from 0.14 to 19 nmol L−1. We determined a detection limit of 0.068 nmol L−1, an average recovery coefficient of 83.8 % (80.2–90.0 %), and a relative standard deviation of ±7.2 %. With our method we determined for the first time the temporal and spatial distributions of NO surface concentrations in coastal waters of the Yellow Sea off Qingdao and in Jiaozhou Bay during a cruise in November 2009. The concentrations of NO varied from below the detection limit to 0.50 nmol L−1 with an average of 0.26 ± 0.14 nmol L−1. NO surface concentrations were generally enhanced significantly during daytime, implying that NO formation processes such as NO2− photolysis are much higher during daytime than chemical NO consumption, which, in turn, lead to a significant decrease in NO concentrations during nighttime. In general, NO surface concentrations and measured NO production rates were higher compared to previously reported measurements. This might be caused by the high NO2− surface concentrations encountered during the cruise. Moreover, additional measurements of NO production rates implied that the occurrence of particles and a temperature increase can enhance NO production rates. With the method introduced here, we have a reliable and comparably easy to use method at hand to measure oceanic NO surface concentrations, which can be used to decipher both its temporal and spatial distributions as well as its biogeochemical pathways in the oceans.
    Type: Article , PeerReviewed
    Format: text
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  • 6
    Publication Date: 2011-06-16
    Description: Author(s): Xu-hong Tian, Ye-han Zheng, Xiong Jiao, Cai-xing Liu, and Shan Chang The protein folding problem is one of the fundamental and important questions in molecular biology. However, the all-atom molecular dynamics studies of protein folding and unfolding are still computationally expensive and severely limited by the time scale of simulation. In this paper, a simple and ... [Phys. Rev. E 83, 061910] Published Wed Jun 15, 2011
    Keywords: Biological physics
    Print ISSN: 1539-3755
    Electronic ISSN: 1550-2376
    Topics: Physics
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  • 7
    Publication Date: 2023-02-08
    Description: Nitric oxide (NO) is a short-lived intermediate of the oceanic nitrogen cycle. However, our knowledge about its production and consumption pathways in oceanic environments is rudimentary. In order to decipher the major factors affecting NO photochemical production, we irradiated several artificial seawater samples as well as 31 natural surface seawater samples in laboratory experiments. The seawater samples were collected during a cruise to the western tropical North Pacific Ocean (WTNP, a N-S section from 36 to 2 degrees N along 146 to 143 degrees E with 6 and 12 stations, respectively, and a W-E section from 137 to 161 degrees E along the Equator with 13 stations) from November 2015 to January 2016. NO photoproduction rates from dissolved nitrite in artificial seawater showed increasing trends with decreasing pH, increasing temperature, and increasing salinity. In contrast, NO photoproduction rates (average: 0.5 +/- 0.2 x 10(-12) mol L-1 s(-1)) in the natural seawater samples from the WTNP did not show any correlations with pH, water temperature, salinity, or dissolved inorganic nitrite concentrations. The flux induced by NO photoproduction in the WTNP (average: 13 x 10(-12) mol M-2 S-1) was significantly larger than the NO air-sea flux density (average: 1.8 x 10(-12) Mol M-2 S-1), indicating a further NO loss process in the surface layer.
    Type: Article , PeerReviewed
    Format: text
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  • 8
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    Copernicus Publications (EGU)
    In:  Biogeosciences (BG), 16 (22). pp. 4485-4496.
    Publication Date: 2022-01-31
    Description: Nitric oxide (NO) is a short-lived compound of the marine nitrogen cycle; however, our knowledge about its oceanic distribution and turnover is rudimentary. Here we present the measurements of dissolved NO in the surface and bottom layers at 75 stations in the Bohai Sea (BS) and the Yellow Sea (YS) in June 2011. Moreover, NO photoproduction rates were determined at 27 stations in both seas. The NO concentrations in the surface and bottom layers were highly variable and ranged from below the limit of detection (i.e., 32 pmol L−1) to 616 pmol L−1 in the surface layer and 482 pmol L−1 in the bottom layer. There was no significant difference (p〉0.05) between the mean NO concentrations in the surface (186±108 pmol L−1) and bottom (174±123 pmol L−1) layers. A decreasing trend of NO in bottom-layer concentrations with salinity indicates a NO input by submarine groundwater discharge. NO in the surface layer was supersaturated at all stations during both day and night and therefore the BS and YS were a persistent source of NO to the atmosphere at the time of our measurements. The average flux was about 4.5×10−16 mol cm−2 s−1 and the flux showed significant positive relationship with the wind speed. The accumulation of NO during daytime was a result of photochemical production, and photoproduction rates were correlated to illuminance. The persistent nighttime NO supersaturation pointed to an unidentified NO dark production. NO sea-to-air flux densities were much lower than the NO photoproduction rates. Therefore, we conclude that the bulk of the NO produced in the mixed layer was rapidly consumed before its release to the atmosphere.
    Type: Article , PeerReviewed
    Format: text
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  • 9
    Publication Date: 2024-02-07
    Description: Nitric oxide (NO) is an atmospheric pollutant and climate forcer as well as a key intermediary in the marine nitrogen cycle, but the ocean’s NO contribution and production mechanisms remain unclear. Here, high-resolution NO observations were conducted simultaneously in the surface ocean and the lower atmosphere of the Yellow Sea and the East China Sea; moreover, NO production from photolysis and microbial processes was analyzed. The NO sea–air exchange showed uneven distributions (RSD = 349.1%) with an average flux of 5.3 ± 18.5 × 10–17 mol cm–2 s–1. In coastal waters where nitrite photolysis was the predominant source (89.0%), NO concentrations were remarkably higher (84.7%) than the overall average of the study area. The NO from archaeal nitrification accounted for 52.8% of all microbial production (11.0%). We also examined the relationship between gaseous NO and ozone which helped identify sources of atmospheric NO. The sea-to-air flux of NO in coastal waters was narrowed by contaminated air with elevated NO concentrations. These findings indicate that the emissions of NO from coastal waters, mainly controlled by reactive nitrogen inputs, will increase with the reduced terrestrial NO discharge.
    Type: Article , PeerReviewed
    Format: text
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  • 10
    Publication Date: 2024-02-07
    Description: Nitric oxide (NO) is a short-lived intermediate of the oceanic nitrogen cycle, and it is produced by biological and photochemical processes in the ocean. Nitrogen dioxide (NO2) is a reactive atmospheric compound which has not been determined in the ocean so far. Here, we present the setup and validation of a novel continuous underway measurement system to measure dissolved NO and NO2 in the surface ocean. The system consists of a seawater/gas equilibration component coupled to a chemiluminescence detector. It was successfully deployed during a 12 day cruise to the East China Sea in May 2018. Dissolved NO and NO2 surface concentrations ranged from 〈limit of detection (LOD) to 98 × 10-12 mol L-1 and 〈LOD to 83 × 10-12 mol L-1, respectively. The ECS was supersaturated with NO but significantly undersaturated with NO2, indicating that the surface waters were a source for atmospheric NO but a sink for atmospheric NO2 at the time of our measurements.
    Type: Article , PeerReviewed
    Format: text
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