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Yang JH, Wang H, Chung SL, Zhu YS, Cole R. Initial subduction-related magmatism in southern Alaska identified by geochemistry and zircon Hf-O isotopes. Sci Bull (Beijing) 2021; 66:1030-1036. [PMID: 36654247 DOI: 10.1016/j.scib.2021.01.016] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/19/2020] [Revised: 12/12/2020] [Accepted: 12/21/2020] [Indexed: 01/20/2023]
Abstract
Abundant arc-type magmatic and metamorphic rocks exist on Earth today, which provide insights into the equilibrium state of the subduction process. However, magmatic samples generated during the initial stage of subduction is largely unknown. This hinders our understanding of the subduction initiation process and by inference, the onset of plate tectonics as well as the history of crustal formation. To address this issue, we carried out a comprehensive geochemical-geochronological study of a suite of Late Triassic to mid-Jurassic plutonic rocks from southern Alaska that potentially represent magmas from the initial to mature stages of arc formation. While all studied samples show typical arc-type geochemical signatures, i.e., enrichment of large ion lithophile elements (LILEs) and depletion of high field strength elements (HFSEs) relative to the heavy rare earth elements (HREEs), the Late Triassic trondhjemites show unique geochemical features such as strongly positive εHf(t) and εNd(t) coupled with lower δ18O (average 4.77‰ ± 0.09‰). These signatures, along with its higher zircon saturation temperatures compared with younger plutonic rocks, are best explained by shallow partial melting of subducting high-temperature hydrothermally altered lower oceanic crust (i.e., gabbro). If true, these surprising findings would open up new ways to study subduction initiation which would have important bearing on future research on the onset of global plate tectonics and the formation of the continental crust.
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Affiliation(s)
- Jin-Hui Yang
- State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China.
| | - Hao Wang
- State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
| | - Sun-Lin Chung
- Institute of Earth Sciences, Academia Sinica, Taipei 11529, China
| | - Yu-Sheng Zhu
- State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
| | - Ronald Cole
- Department of Geology, Allegheny College, Meadville PA 16335, USA
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Rezal R, Chung SL, Abd Ghani A, Lee HY, Iizuka Y. Zircon U-Pb Ages and Geochemical Characteristics of Mafic Rocks from Northern Sabah Ophiolite (Borneo), Malaysia. Goldschmidt Abstracts 2020. [DOI: 10.46427/gold2020.2197] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 09/01/2023]
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Wang Q, Hawkesworth CJ, Wyman D, Chung SL, Wu FY, Li XH, Li ZX, Gou GN, Zhang XZ, Tang GJ, Dan W, Ma L, Dong YH. Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow. Nat Commun 2016; 7:11888. [PMID: 27307135 PMCID: PMC4912662 DOI: 10.1038/ncomms11888] [Citation(s) in RCA: 60] [Impact Index Per Article: 7.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/24/2015] [Accepted: 05/10/2016] [Indexed: 11/10/2022] Open
Abstract
There is considerable controversy over the nature of geophysically recognized low-velocity–high-conductivity zones (LV–HCZs) within the Tibetan crust, and their role in models for the development of the Tibetan Plateau. Here we report petrological and geochemical data on magmas erupted 4.7–0.3 Myr ago in central and northern Tibet, demonstrating that they were generated by partial melting of crustal rocks at temperatures of 700–1,050 °C and pressures of 0.5–1.5 GPa. Thus Pliocene-Quaternary melting of crustal rocks occurred at depths of 15–50 km in areas where the LV–HCZs have been recognized. This provides new petrological evidence that the LV–HCZs are sources of partial melt. It is inferred that crustal melting played a key role in triggering crustal weakening and outward crustal flow in the expansion of the Tibetan Plateau. The role of the low velocity-high conductivity zones (LV–HCZs) in developing the Tibetan Plateau has remained controversial. Here, Wang et al. present new geochemical and petrological data that show the LV–HCZs are sources of partial melt thus giving insight into the development of the Tibetan Plateau.
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Affiliation(s)
- Qiang Wang
- State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China.,CAS Center for Excellence in Tibetan Plateau Earth Sciences (CETES), Beijing 100101, China
| | - Chris J Hawkesworth
- School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK.,Department of Earth and Environmental Sciences, University of St Andrews, North Street, St Andrews KY16 9AL, UK
| | - Derek Wyman
- School of Geosciences, The University of Sydney, Sydney, New South Wales 2006, Australia
| | - Sun-Lin Chung
- Institute of Earth Sciences, Academia Sinica, Nangang, Taipei 11529, Taiwan.,Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan
| | - Fu-Yuan Wu
- Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
| | - Xian-Hua Li
- Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
| | - Zheng-Xiang Li
- ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) and the Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin University, Perth, Western Australia 6845, Australia
| | - Guo-Ning Gou
- State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Xiu-Zheng Zhang
- State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Gong-Jian Tang
- State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Wei Dan
- State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Lin Ma
- State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Yan-Hui Dong
- State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
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Li S, Chung SL, Wilde SA, Wang T, Xiao WJ, Guo QQ. Linking magmatism with collision in an accretionary orogen. Sci Rep 2016; 6:25751. [PMID: 27167207 PMCID: PMC4863176 DOI: 10.1038/srep25751] [Citation(s) in RCA: 65] [Impact Index Per Article: 8.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/02/2015] [Accepted: 04/21/2016] [Indexed: 11/09/2022] Open
Abstract
A compilation of U-Pb age, geochemical and isotopic data for granitoid plutons in the southern Central Asian Orogenic Belt (CAOB), enables evaluation of the interaction between magmatism and orogenesis in the context of Paleo-Asian oceanic closure and continental amalgamation. These constraints, in conjunction with other geological evidence, indicate that following consumption of the ocean, collision-related calc-alkaline granitoid and mafic magmatism occurred from 255 ± 2 Ma to 251 ± 2 Ma along the Solonker-Xar Moron suture zone. The linear or belt distribution of end-Permian magmatism is interpreted to have taken place in a setting of final orogenic contraction and weak crustal thickening, probably as a result of slab break-off. Crustal anatexis slightly post-dated the early phase of collision, producing adakite-like granitoids with some S-type granites during the Early-Middle Triassic (ca. 251–245 Ma). Between 235 and 220 Ma, the local tectonic regime switched from compression to extension, most likely caused by regional lithospheric extension and orogenic collapse. Collision-related magmatism from the southern CAOB is thus a prime example of the minor, yet tell-tale linking of magmatism with orogenic contraction and collision in an archipelago-type accretionary orogen.
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Affiliation(s)
- Shan Li
- Xinjiang Research Center for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China.,Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China.,Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan.,Xinjiang Key Laboratory of Mineral Resources and Digital Geology, Urumqi 830011, China
| | - Sun-Lin Chung
- Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan.,Institute of Earth Sciences, Academia Sinica, Taipei 11529, Taiwan
| | - Simon A Wilde
- Department of Applied Geology, Curtin University, G.P.O. Box U1987, Perth, Western Australia 6845, Australia
| | - Tao Wang
- Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
| | - Wen-Jiao Xiao
- Xinjiang Research Center for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China.,Xinjiang Key Laboratory of Mineral Resources and Digital Geology, Urumqi 830011, China.,State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
| | - Qian-Qian Guo
- Key Laboratory of Computational Geodynamics, University of Chinese Academy of Sciences, Beijing 100049, China
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Zhu DC, Wang Q, Zhao ZD, Chung SL, Cawood PA, Niu Y, Liu SA, Wu FY, Mo XX. Magmatic record of India-Asia collision. Sci Rep 2015; 5:14289. [PMID: 26395973 PMCID: PMC4585790 DOI: 10.1038/srep14289] [Citation(s) in RCA: 241] [Impact Index Per Article: 26.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/21/2014] [Accepted: 08/24/2015] [Indexed: 11/25/2022] Open
Abstract
New geochronological and geochemical data on magmatic activity from the India-Asia collision zone enables recognition of a distinct magmatic flare-up event that we ascribe to slab breakoff. This tie-point in the collisional record can be used to back-date to the time of initial impingement of the Indian continent with the Asian margin. Continental arc magmatism in southern Tibet during 80–40 Ma migrated from south to north and then back to south with significant mantle input at 70–43 Ma. A pronounced flare up in magmatic intensity (including ignimbrite and mafic rock) at ca. 52–51 Ma corresponds to a sudden decrease in the India-Asia convergence rate. Geological and geochemical data are consistent with mantle input controlled by slab rollback from ca. 70 Ma and slab breakoff at ca. 53 Ma. We propose that the slowdown of the Indian plate at ca. 51 Ma is largely the consequence of slab breakoff of the subducting Neo-Tethyan oceanic lithosphere, rather than the onset of the India-Asia collision as traditionally interpreted, implying that the initial India-Asia collision commenced earlier, likely at ca. 55 Ma.
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Affiliation(s)
- Di-Cheng Zhu
- State Key Laboratory of Geological Processes and Mineral Resources, and School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
| | - Qing Wang
- State Key Laboratory of Geological Processes and Mineral Resources, and School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
| | - Zhi-Dan Zhao
- State Key Laboratory of Geological Processes and Mineral Resources, and School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
| | - Sun-Lin Chung
- Institute of Earth Sciences, Academia Sinica, Taipei 11529, Taiwan.,Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan
| | - Peter A Cawood
- Department of Earth Sciences, University of St Andrews, North Street, St Andrews KY16 9AL, UK.,Centre for Exploration Targeting, School of Earth and Environment, University of Western Australia, 35 Stirling Hwy., Crawley WA, 6009, Australia
| | - Yaoling Niu
- State Key Laboratory of Geological Processes and Mineral Resources, and School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China.,Department of Earth Sciences, Durham University, Durham DH1 3LE, UK
| | - Sheng-Ao Liu
- State Key Laboratory of Geological Processes and Mineral Resources, and School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
| | - Fu-Yuan Wu
- Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
| | - Xuan-Xue Mo
- State Key Laboratory of Geological Processes and Mineral Resources, and School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
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Lee VW, Chiu LY, Chung SL, Lau CY, Yousaf S, Wong H, Lam YY, Yan BP. Clnical Management Of Non-Valvular Atrial Fibrillation In Hong Kong. Value Health 2014; 17:A483. [PMID: 27201416 DOI: 10.1016/j.jval.2014.08.1407] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/05/2023]
Affiliation(s)
- V W Lee
- Chinese University of Hong Kong, Hong Kong, Hong Kong
| | - L Y Chiu
- Chinese University of Hong Kong, Hong Kong, Hong Kong
| | - S L Chung
- Chinese University of Hong Kong, Hong Kong, Hong Kong
| | - C Y Lau
- Chinese University of Hong Kong, Hong Kong, Hong Kong
| | - S Yousaf
- Chinese University of Hong Kong, Hong Kong, Hong Kong
| | - H Wong
- Chinese University of Hong Kong, Hong Kong, Hong Kong
| | - Y Y Lam
- Chinese University of Hong Kong, Shatin, Hong Kong, China
| | - B P Yan
- Chinese University of Hong Kong, Shatin, Hong Kong, China
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Cheung KW, Chung SL, Chung KY, Chiu KH. Patient perception and knowledge on total joint replacement surgery. Hong Kong Med J 2013; 19:33-37. [PMID: 23378352] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 06/01/2023] Open
Abstract
OBJECTIVES To study patients' perceptions and knowledge about total joint replacement surgery. DESIGN; Cross-sectional survey. SETTING; University teaching hospital, Hong Kong. PATIENTS Three hundred consecutive patients with the diagnosis of osteoarthritis or inflammatory arthritis attending the out-patient clinic from June 2010 to May 2011. MAIN OUTCOME MEASURES Patients' knowledge and how they got the knowledge about total joint replacement surgery, and concerns about the outcome of such operations. RESULTS Whilst 94% of the patients knew about total joint replacement surgery, 77% obtained such knowledge from their friends and relatives. The three most common concerns related to this type of operation were whether they might: be wheelchair bound after surgery (64%), need to be taken care of by others for more than 3 months (61%), and have post-surgery complications (54%). Most of them recognised the advantages of the surgery, 82% knew about good pain relief after surgery, and 87% realised that total joint replacement surgery could improve their mobility. Patients did not have a realistic idea regarding the survival of the prosthesis; 41% thought the prosthesis might last for less than 10 years and 34% had no idea about its longevity. CONCLUSION; Patients did recognise the advantages of total joint replacement surgery in treating arthritis. However, they had many concerns about its outcome that warrant clarification. Public education on these aspects is necessary to address concerns, and may be achieved in cooperation with the media.
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Affiliation(s)
- K W Cheung
- Department of Orthopaedics and Traumatology, The Chinese University of Hong Kong, Prince of Wales Hospital, Shatin, Hong Kong.
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Lin SC, Kuo BY, Chung SL. Thermomechanical models for the dynamics and melting processes in the Mariana subduction system. ACTA ACUST UNITED AC 2010. [DOI: 10.1029/2010jb007658] [Citation(s) in RCA: 14] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Sobolev AV, Hofmann AW, Kuzmin DV, Yaxley GM, Arndt NT, Chung SL, Danyushevsky LV, Elliott T, Frey FA, Garcia MO, Gurenko AA, Kamenetsky VS, Kerr AC, Krivolutskaya NA, Matvienkov VV, Nikogosian IK, Rocholl A, Sigurdsson IA, Sushchevskaya NM, Teklay M. The amount of recycled crust in sources of mantle-derived melts. Science 2007; 316:412-7. [PMID: 17395795 DOI: 10.1126/science.1138113] [Citation(s) in RCA: 982] [Impact Index Per Article: 57.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/03/2022]
Abstract
Plate tectonic processes introduce basaltic crust (as eclogite) into the peridotitic mantle. The proportions of these two sources in mantle melts are poorly understood. Silica-rich melts formed from eclogite react with peridotite, converting it to olivine-free pyroxenite. Partial melts of this hybrid pyroxenite are higher in nickel and silicon but poorer in manganese, calcium, and magnesium than melts of peridotite. Olivine phenocrysts' compositions record these differences and were used to quantify the contributions of pyroxenite-derived melts in mid-ocean ridge basalts (10 to 30%), ocean island and continental basalts (many >60%), and komatiites (20 to 30%). These results imply involvement of 2 to 20% (up to 28%) of recycled crust in mantle melting.
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Affiliation(s)
- Alexander V Sobolev
- Max Planck Institute (MPI) for Chemistry, Post Office Box 3060, 55020 Mainz, Germany.
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Abstract
BACKGROUND Many hair transplant surgeons have advocated the use of micrograft megasessions for the purpose of a more natural looking end result, especially in the Oriental with higher skin/hair color contrast and darker, coarse, straight hairs. But it also has some fundamental limitations. Most important are a low graft yield and a low density after transplantation. There are several reports about the survival rate of micrografts in Caucasians, though the results are variable, but few reports about the survival rate and fate of micrografts in Orientals. OBJECTIVE To compare the survival rate of one-hair follicular units with that of two-hair follicular units using the KNU implanter, to ascertain the average survival rate of micrografts (one- and two-hair follicular units), and to evaluate the fate of grafted hair according to time. METHODS Two templates of 1.5 cm2 were made by tattooing on both sides of the frontoparietal recess areas in 11 patients with male pattern baldness (beyond Norwood type IIIa). The authors planted one-hair unit micrografts in the left template and two-hair unit micrografts in the right template, which were prepared by the concept of follicular unit, and counted the surviving number of follicular units at 1 and 3 months and total hairs at 6 and 12 months after transplantation. RESULTS The mean survival rate by the number of follicular units was 47.3 and 57.4% at 1 and 3 months after transplantation, respectively. The mean survival rate by the total number of hairs was 92.0 and 90.4% at 6 and 12 months after transplantation, respectively. CONCLUSION About 50% of the transplanted hairs fell out in 1 month, but at 6 months the survival rate of follicular unit transplantation using the KNU implanter showed a good result (92%), and there were no significant differences in the mean survival rate of follicular unit and total hairs between one-hair and two-hair units at 1, 3, 6, and 12 months after transplantation.
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Affiliation(s)
- S J Lee
- Departments of Dermatology and Immunology, Kyungpook National University School of Medicine, Taegu, Korea
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Abstract
We report a 47-year-old woman who presented with asymptomatic reticulate hyperpigmentations on the neck, lateral face, axillae, trunk, inguinal areas, and dorsa of both hands and feet. We thought it was an unusual case in the spectrum between the pole of Dowling-Degos disease (DDD) and that of reticulate acropigmentation of Kitamura (RAK). Another interesting point was that the biopsied specimens from the abdomen, neck, and axillary lesions showed somewhat different histopathologic features from typical DDD, suggesting an evolutional sequence. From these findings we suggest that a lichenoid inflammation may be responsible for the typical maculo-papular lesions of DDD.
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Affiliation(s)
- S J Lee
- Department of Dermatology, Kyungpook National University School of Medicine, Taegu, Korea
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Chung SL, Ding YA. Fatal hemoptysis in dissecting aortic aneurysm and salmonellosis: a case report. Zhonghua Yi Xue Za Zhi (Taipei) 1999; 62:817-22. [PMID: 10575811] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Subscribe] [Scholar Register] [Indexed: 04/14/2023]
Abstract
Hemoptysis is a rare manifestation of dissecting aortic aneurysm and aortobronchial fistula may occur when an aortic aneurysm is mycotic, atherosclerotic, traumatic or postoperative. Aortobronchial fistulas are generally fatal if not treated surgically. An aggressive diagnostic approach to patients with hemoptysis and prompt surgical intervention in those suspected of aortobronchial fistulas should result in additional survivors. Imaging studies, including chest radiography, chest computerized tomography, arteriography and bronchoscopy provide useful diagnostic information. However, challenges remain when we encounter this condition. Sometimes, the final exsanguinating hemorrhage is preceded by a distinct prodromal period of intermittent hemoptysis. This allows clinicians time to recognize such fistulas and perform emergency surgery. We present a patient with this condition to alert clinicians to this potentially deadly cause of hemoptysis.
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Affiliation(s)
- S L Chung
- Department of Medicine, Taipei Veterans General Hospital, National Yang-Ming University School of Medicine, Taiwan, ROC
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Abstract
Location of the bladder neck and its dynamic motion are believed to be influenced by body position. This study was designed to evaluate factors affecting bladder neck mobility in both supine and standing positions. The parameters of 75 GSI patients and 49 controls were compared by Student's t-test. Receiver operating characteristic curves and multiple logistic regression analysis were used to analyze the effects of potential contributing factors on bladder neck mobility. We were unable to find any significant correlation between bladder neck hypermobility and GSI. We also failed to demonstrate that bladder neck hypermobility in the supine or standing position relative to previous believed risk factors, including parity, vaginal delivery, menopause, cystocele, rectocele, uterine prolapse or body mass index. In order to elucidate the pathophysiology of bladder neck mobility clearly, changes in intraabdominal pressure and gravitational direction in different positions should be evaluated carefully and scientifically in further studies.
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Affiliation(s)
- L Y Lin
- Department of Obstetrics and Gynecology, Chung Shan Medical and Dental College Hospital, Taichung, Taiwan
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15
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Shinjo R, Chung SL, Kato Y, Kimura M. Geochemical and Sr-Nd isotopic characteristics of volcanic rocks from the Okinawa Trough and Ryukyu Arc: Implications for the evolution of a young, intracontinental back arc basin. ACTA ACUST UNITED AC 1999. [DOI: 10.1029/1999jb900040] [Citation(s) in RCA: 306] [Impact Index Per Article: 12.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Abstract
BACKGROUND The tropical rat mite, Ornithonyssus bacoti (0. bacoti), is an ectoparasite on many rodents, but when the rodent is not available, humans may become the victim of the mite's bite. The bite induces a nonspecific dermatitis; therefore, it is not easy to diagnose rat mite dermatitis unless the parasites are found. MATERIALS AND METHODS Ten cases of rat mite dermatitis were found in medical students who had studied in the same room of the library. Their nonspecific dermatitis consisted of small papules, and parasites were found in the skin or in the environment. The mites were collected and identified as O. bacoti, female. Histopathologic studies showed moderate perivascular lymphohistiocytic infiltrations intermingled with some eosinophils. The presence of rodents in or around the room was confirmed by the students, but there had been no preceding rodent eradication. Although the rats were not captured in the library, insecticides were sprayed, and no further problem with either mites or dermatitis developed during the follow-up period. CONCLUSIONS Rat mite dermatitis can occur in clusters that involve a common source of exposure to the rat mite epidemiologically. Prompt identification of rat mites and the eradication of mites and rodents from the environment can prevent further spreading of the disease.
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Affiliation(s)
- S L Chung
- Department of Dermatology, Kyungpook National University School of Medicine, Taegu, South Korea
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Lee TY, Lo CH, Chung SL, Chen CY, Wang PL, Lin WP, Hoang N, Chi CT, Yem NT. 40Ar/39Ar dating result of Neogene basalts in Vietnam and its tectonic implication. Mantle Dynamics and Plate Interactions in East Asia 1998. [DOI: 10.1029/gd027p0317] [Citation(s) in RCA: 27] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 01/03/2023]
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Chung SL, Jahn BM, Genyao W, Lo CH, Bolin C. The Emeishan flood basalt in SW China: A mantle plume initiation model and its connection with continental breakup and mass extinction at the Permian-Triassic Boundary. Mantle Dynamics and Plate Interactions in East Asia 1998. [DOI: 10.1029/gd027p0047] [Citation(s) in RCA: 81] [Impact Index Per Article: 3.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 12/13/2022]
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19
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Affiliation(s)
- J B Jun
- Department of Dermatology, Kyungpook National University School of Medicine, Taegu, South Korea
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Lee SJ, Kim DW, Jun JB, Chung SL, Kim JC. Lipid composition of the stratum corneum of the sole in patients with leprosy. Int J Lepr Other Mycobact Dis 1994; 62:574-9. [PMID: 7868956] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Subscribe] [Scholar Register] [Indexed: 01/27/2023]
Abstract
Several reports support the view that changes of composition of the stratum corneum (SC) lipids may be the cause of impaired barrier function which, in turn, gives rise to xerosis and ichthyotic skin in leprosy. Many reports about abnormalities of serum lipids and cutaneous manifestations, such as xerosis and ichthyotic changes in leprosy, led us to the idea that the composition of SC lipids in patients with leprosy may be different from that in normal subjects. However, the many studies done in the past do not sufficiently account for this. To investigate the composition of SC lipids in patients with leprosy, thin-layer chromatography (TLC) was undertaken. Extraction of the SC lipids with a methanolchloroform-H2O mixture (4:2:1.6, v/v/v, Bligh-Dyer solvent) was carried out after shaving of the SC from the sole. TLC was performed and the composition of lipids was quantitated by photodensitometry. Our study revealed that the composition of SC lipids in the anesthetic lesions of leprosy patients was higher in cholesterol sulfate and triglycerides and lower in sphingolipids and cholesterol esters than that of normal subjects.
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Affiliation(s)
- S J Lee
- Department of Dermatology, Kyungpook National University School of Medicine, Taegu City, South Korea
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Abstract
Acetylcholine (ACh) was found to markedly enhance the nerve stimulation induced twitch response of isolated, field-stimulated rat vas deferens (RVD). The ED200 (concentration which enhances the twitch response to 200% of control) for this potentiation was 6 X 10(-6)M with the maximum twitch response being increased by more than 3 fold (325 +/- 30%). Carbachol (ED200 = 8.5 X 10(-7)M) showed identical results. With each drug the potentiation was competitively antagonized by atropine (10(-7) - 10(-5)M). Physostigmine 10(-8) - 10(-6)M) both enhanced the basal twitch response (215 +/- 8% of control at 10(-5)M) and the sensitivity of the RVD to ACh (ED200 = 3.3 X 10(-7)M) but not to carbachol. Atropine, on the other hand reduced the basal twitch response by 18 +/- 3% at 10(-5)M. Hemicholinium (10(-4)M) also reduced the basal twitch responses by 23 +/- 5%. ACh (10(-7)M - 10(-5)M) did not modify the responses of unstimulated RVD to norepinephrine or KCl suggesting a pre-synaptic site of action. Taken together these results are compatible with the presence of a pre-junctional, excitatory muscarinic mechanism in the field stimulated RVD. That this cholinergic system may be of physiological significance is supported by the observations that atropine and hemicholinium depress while physostigmine enhances the twitch response in the absence of exogenous ACh.
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Chung SL. [A report on the knowledge of, and attitude toward contraceptive methods of students in National Chung-Hsing University]. Hu Li Za Zhi 1980; 27:67-79. [PMID: 6901768] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [MESH Headings] [Subscribe] [Scholar Register] [Indexed: 01/22/2023]
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Chung SL. The reverse view. Radiography (Lond) 1967; 33:108-9. [PMID: 6040639] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [MESH Headings] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/18/2023]
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