Decadal variability of chlorophyll a in the South China Sea: a possible mechanism
Four climatologies on a monthly scale (January, April, May and November) of chlorophyll a within the South China Sea (SCS) were calculated using a Coastal Zone Color Scanner (CZCS) (1979-1983) and the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) (1998-2002). We analyzed decadal variability of chl...
Gespeichert in:
Veröffentlicht in: | Chinese journal of oceanology and limnology 2012-11, Vol.30 (6), p.1054-1062 |
---|---|
Hauptverfasser: | , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 1062 |
---|---|
container_issue | 6 |
container_start_page | 1054 |
container_title | Chinese journal of oceanology and limnology |
container_volume | 30 |
creator | Liu, Fenfen Chen, Chuqun Zhan, Haigang |
description | Four climatologies on a monthly scale (January, April, May and November) of chlorophyll a within the South China Sea (SCS) were calculated using a Coastal Zone Color Scanner (CZCS) (1979-1983) and the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) (1998-2002). We analyzed decadal variability of chlorophyll a by comparing the products of the two observation periods. The relationships of variability in chlorophyll a with sea surface wind speed (SSW), sea surface temperature (SST), wind stress (WS), and mixed layer depth (MLD) were determined. The results indicate that there is obvious chlorophyll a decadal variability in the SCS. The decadal chlorophyll a presents distinct seasonal variability in characteristics, which may be as a result of various different dynamic processes. The negative chlorophyll a concentration anomaly in January was associated with the warming of SST and a shallower MLD. Generally, there were higher chlorophyll a concentrations in spring during the SeaWiFS period compared with the CZCS period. However, the chlorophyll a concentration exhibits some regional differences during this season, leading to an explanation being difficult. The deepened MLD may have contributed to the positive chlorophyll a concentration anomalies from the northwestern Luzon Island to the northeastern region of Vietnam during April and May. The increases of chlorophyll a concentration in northwestern Borneo during May may be because the stronger SSW and higher WS produce a deeper mixed layer and convective mixing, leading to high levels of nutrient concentrations. The higher chlorophyll a off southeastern Vietnam may be associated with the advective transport of the colder water extending from the Karimata Strait to southeastern Vietnam. |
doi_str_mv | 10.1007/s00343-012-1282-9 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_1170530060</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>43767445</cqvip_id><sourcerecordid>1257760932</sourcerecordid><originalsourceid>FETCH-LOGICAL-c399t-43f34e9b0bd17d48585e30386a8e2baa5231b9664d306270fe99b4a5883536f33</originalsourceid><addsrcrecordid>eNp9kMFu1DAURS1EJYaWD2CFERs2gWc_O4mXaIAWqRKLoWvrJeNMXHniqZ1Bml_hW_in_gKuUiHEoisv3jlX15ex1wI-CIDmYwZAhRUIWQnZyso8YythDFYaQD9nK5BaVQq0ecFe5nxbaKPArNjms-tpS4H_pOSp88HPJx4H3o8hpngYTyFw4n7i8-j4Jh7nka9HPxHfOLr__avcDjFn3wXH964fafJ5f8HOBgrZvXp8z9nN1y8_1lfV9ffLb-tP11WPxsyVwgGVMx10W9FsVatb7RCwral1siPSEkVn6lptEWrZwOCM6RTptkWN9YB4zt4vuYcU744uz3bvc-9CoMnFY7ZC6qapwaAs6Lv_0Nt4TFNpZ4VoQCNADYUSC9Wn8qnkBntIfk_pZAXYh5ntMrMtM9uHma0pjlycXNhp59I_yU9IbxZpoGhpl3y2NxsJQgEIrY1sC_H2scoYp91dSf7bRWFTN0pp_ANE3pLB</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1170530060</pqid></control><display><type>article</type><title>Decadal variability of chlorophyll a in the South China Sea: a possible mechanism</title><source>ProQuest Central Essentials</source><source>ProQuest Central (Alumni Edition)</source><source>ProQuest Central Student</source><source>SpringerNature Journals</source><source>ProQuest Central Korea</source><source>ProQuest Central UK/Ireland</source><source>Alma/SFX Local Collection</source><source>ProQuest Central</source><creator>Liu, Fenfen ; Chen, Chuqun ; Zhan, Haigang</creator><creatorcontrib>Liu, Fenfen ; Chen, Chuqun ; Zhan, Haigang</creatorcontrib><description>Four climatologies on a monthly scale (January, April, May and November) of chlorophyll a within the South China Sea (SCS) were calculated using a Coastal Zone Color Scanner (CZCS) (1979-1983) and the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) (1998-2002). We analyzed decadal variability of chlorophyll a by comparing the products of the two observation periods. The relationships of variability in chlorophyll a with sea surface wind speed (SSW), sea surface temperature (SST), wind stress (WS), and mixed layer depth (MLD) were determined. The results indicate that there is obvious chlorophyll a decadal variability in the SCS. The decadal chlorophyll a presents distinct seasonal variability in characteristics, which may be as a result of various different dynamic processes. The negative chlorophyll a concentration anomaly in January was associated with the warming of SST and a shallower MLD. Generally, there were higher chlorophyll a concentrations in spring during the SeaWiFS period compared with the CZCS period. However, the chlorophyll a concentration exhibits some regional differences during this season, leading to an explanation being difficult. The deepened MLD may have contributed to the positive chlorophyll a concentration anomalies from the northwestern Luzon Island to the northeastern region of Vietnam during April and May. The increases of chlorophyll a concentration in northwestern Borneo during May may be because the stronger SSW and higher WS produce a deeper mixed layer and convective mixing, leading to high levels of nutrient concentrations. The higher chlorophyll a off southeastern Vietnam may be associated with the advective transport of the colder water extending from the Karimata Strait to southeastern Vietnam.</description><identifier>ISSN: 0254-4059</identifier><identifier>ISSN: 2096-5508</identifier><identifier>EISSN: 1993-5005</identifier><identifier>EISSN: 2523-3521</identifier><identifier>DOI: 10.1007/s00343-012-1282-9</identifier><language>eng</language><publisher>Heidelberg: Springer-Verlag</publisher><subject>Algae ; Carbon cycle ; Chlorophyll ; Chlorophylls ; Climate science ; Coastal zone ; Coastal Zone Color Scanner ; Coastal zones ; coasts ; color ; Earth and Environmental Science ; Earth Sciences ; Field of view ; Marine ; Mixed layer ; Mixed layer depth ; Nutrient concentrations ; nutrient content ; Oceanography ; Sea surface ; Sea surface temperature ; Sea-viewing Wide Field-of-view Sensor ; Seasonal variation ; Seasonal variations ; SeaWiFS ; spring ; Surface temperature ; Surface wind ; Wind speed ; Wind stress ; 中国南海 ; 可能机制 ; 叶绿素a浓度 ; 季节变化特征 ; 年代际变化 ; 海洋观测 ; 混合层深度</subject><ispartof>Chinese journal of oceanology and limnology, 2012-11, Vol.30 (6), p.1054-1062</ispartof><rights>Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag Berlin Heidelberg 2012</rights><rights>Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag Berlin Heidelberg 2012.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c399t-43f34e9b0bd17d48585e30386a8e2baa5231b9664d306270fe99b4a5883536f33</citedby><cites>FETCH-LOGICAL-c399t-43f34e9b0bd17d48585e30386a8e2baa5231b9664d306270fe99b4a5883536f33</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/84119X/84119X.jpg</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/1170530060/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/1170530060?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>315,781,785,21393,21394,21395,21396,23261,27929,27930,33535,33708,33749,34010,34319,43664,43792,43810,43958,44072,64390,64394,72474,74109,74288,74307,74478,74595</link.rule.ids></links><search><creatorcontrib>Liu, Fenfen</creatorcontrib><creatorcontrib>Chen, Chuqun</creatorcontrib><creatorcontrib>Zhan, Haigang</creatorcontrib><title>Decadal variability of chlorophyll a in the South China Sea: a possible mechanism</title><title>Chinese journal of oceanology and limnology</title><addtitle>Chin. J. Ocean. Limnol</addtitle><addtitle>Chinese Journal of Oceanology and Limnology</addtitle><description>Four climatologies on a monthly scale (January, April, May and November) of chlorophyll a within the South China Sea (SCS) were calculated using a Coastal Zone Color Scanner (CZCS) (1979-1983) and the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) (1998-2002). We analyzed decadal variability of chlorophyll a by comparing the products of the two observation periods. The relationships of variability in chlorophyll a with sea surface wind speed (SSW), sea surface temperature (SST), wind stress (WS), and mixed layer depth (MLD) were determined. The results indicate that there is obvious chlorophyll a decadal variability in the SCS. The decadal chlorophyll a presents distinct seasonal variability in characteristics, which may be as a result of various different dynamic processes. The negative chlorophyll a concentration anomaly in January was associated with the warming of SST and a shallower MLD. Generally, there were higher chlorophyll a concentrations in spring during the SeaWiFS period compared with the CZCS period. However, the chlorophyll a concentration exhibits some regional differences during this season, leading to an explanation being difficult. The deepened MLD may have contributed to the positive chlorophyll a concentration anomalies from the northwestern Luzon Island to the northeastern region of Vietnam during April and May. The increases of chlorophyll a concentration in northwestern Borneo during May may be because the stronger SSW and higher WS produce a deeper mixed layer and convective mixing, leading to high levels of nutrient concentrations. The higher chlorophyll a off southeastern Vietnam may be associated with the advective transport of the colder water extending from the Karimata Strait to southeastern Vietnam.</description><subject>Algae</subject><subject>Carbon cycle</subject><subject>Chlorophyll</subject><subject>Chlorophylls</subject><subject>Climate science</subject><subject>Coastal zone</subject><subject>Coastal Zone Color Scanner</subject><subject>Coastal zones</subject><subject>coasts</subject><subject>color</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Field of view</subject><subject>Marine</subject><subject>Mixed layer</subject><subject>Mixed layer depth</subject><subject>Nutrient concentrations</subject><subject>nutrient content</subject><subject>Oceanography</subject><subject>Sea surface</subject><subject>Sea surface temperature</subject><subject>Sea-viewing Wide Field-of-view Sensor</subject><subject>Seasonal variation</subject><subject>Seasonal variations</subject><subject>SeaWiFS</subject><subject>spring</subject><subject>Surface temperature</subject><subject>Surface wind</subject><subject>Wind speed</subject><subject>Wind stress</subject><subject>中国南海</subject><subject>可能机制</subject><subject>叶绿素a浓度</subject><subject>季节变化特征</subject><subject>年代际变化</subject><subject>海洋观测</subject><subject>混合层深度</subject><issn>0254-4059</issn><issn>2096-5508</issn><issn>1993-5005</issn><issn>2523-3521</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kMFu1DAURS1EJYaWD2CFERs2gWc_O4mXaIAWqRKLoWvrJeNMXHniqZ1Bml_hW_in_gKuUiHEoisv3jlX15ex1wI-CIDmYwZAhRUIWQnZyso8YythDFYaQD9nK5BaVQq0ecFe5nxbaKPArNjms-tpS4H_pOSp88HPJx4H3o8hpngYTyFw4n7i8-j4Jh7nka9HPxHfOLr__avcDjFn3wXH964fafJ5f8HOBgrZvXp8z9nN1y8_1lfV9ffLb-tP11WPxsyVwgGVMx10W9FsVatb7RCwral1siPSEkVn6lptEWrZwOCM6RTptkWN9YB4zt4vuYcU744uz3bvc-9CoMnFY7ZC6qapwaAs6Lv_0Nt4TFNpZ4VoQCNADYUSC9Wn8qnkBntIfk_pZAXYh5ntMrMtM9uHma0pjlycXNhp59I_yU9IbxZpoGhpl3y2NxsJQgEIrY1sC_H2scoYp91dSf7bRWFTN0pp_ANE3pLB</recordid><startdate>20121101</startdate><enddate>20121101</enddate><creator>Liu, Fenfen</creator><creator>Chen, Chuqun</creator><creator>Zhan, Haigang</creator><general>Springer-Verlag</general><general>SP Science Press</general><general>Springer Nature B.V</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7QL</scope><scope>7SN</scope><scope>7TN</scope><scope>7U7</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>M7N</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>7TG</scope><scope>8FD</scope><scope>FR3</scope><scope>H95</scope><scope>H99</scope><scope>KL.</scope><scope>L.F</scope><scope>P64</scope></search><sort><creationdate>20121101</creationdate><title>Decadal variability of chlorophyll a in the South China Sea: a possible mechanism</title><author>Liu, Fenfen ; Chen, Chuqun ; Zhan, Haigang</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c399t-43f34e9b0bd17d48585e30386a8e2baa5231b9664d306270fe99b4a5883536f33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Algae</topic><topic>Carbon cycle</topic><topic>Chlorophyll</topic><topic>Chlorophylls</topic><topic>Climate science</topic><topic>Coastal zone</topic><topic>Coastal Zone Color Scanner</topic><topic>Coastal zones</topic><topic>coasts</topic><topic>color</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Field of view</topic><topic>Marine</topic><topic>Mixed layer</topic><topic>Mixed layer depth</topic><topic>Nutrient concentrations</topic><topic>nutrient content</topic><topic>Oceanography</topic><topic>Sea surface</topic><topic>Sea surface temperature</topic><topic>Sea-viewing Wide Field-of-view Sensor</topic><topic>Seasonal variation</topic><topic>Seasonal variations</topic><topic>SeaWiFS</topic><topic>spring</topic><topic>Surface temperature</topic><topic>Surface wind</topic><topic>Wind speed</topic><topic>Wind stress</topic><topic>中国南海</topic><topic>可能机制</topic><topic>叶绿素a浓度</topic><topic>季节变化特征</topic><topic>年代际变化</topic><topic>海洋观测</topic><topic>混合层深度</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liu, Fenfen</creatorcontrib><creatorcontrib>Chen, Chuqun</creatorcontrib><creatorcontrib>Zhan, Haigang</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>AGRIS</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Ecology Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Toxicology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>ASFA: Marine Biotechnology Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Marine Biotechnology Abstracts</collection><collection>Biotechnology and BioEngineering Abstracts</collection><jtitle>Chinese journal of oceanology and limnology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liu, Fenfen</au><au>Chen, Chuqun</au><au>Zhan, Haigang</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Decadal variability of chlorophyll a in the South China Sea: a possible mechanism</atitle><jtitle>Chinese journal of oceanology and limnology</jtitle><stitle>Chin. J. Ocean. Limnol</stitle><addtitle>Chinese Journal of Oceanology and Limnology</addtitle><date>2012-11-01</date><risdate>2012</risdate><volume>30</volume><issue>6</issue><spage>1054</spage><epage>1062</epage><pages>1054-1062</pages><issn>0254-4059</issn><issn>2096-5508</issn><eissn>1993-5005</eissn><eissn>2523-3521</eissn><abstract>Four climatologies on a monthly scale (January, April, May and November) of chlorophyll a within the South China Sea (SCS) were calculated using a Coastal Zone Color Scanner (CZCS) (1979-1983) and the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) (1998-2002). We analyzed decadal variability of chlorophyll a by comparing the products of the two observation periods. The relationships of variability in chlorophyll a with sea surface wind speed (SSW), sea surface temperature (SST), wind stress (WS), and mixed layer depth (MLD) were determined. The results indicate that there is obvious chlorophyll a decadal variability in the SCS. The decadal chlorophyll a presents distinct seasonal variability in characteristics, which may be as a result of various different dynamic processes. The negative chlorophyll a concentration anomaly in January was associated with the warming of SST and a shallower MLD. Generally, there were higher chlorophyll a concentrations in spring during the SeaWiFS period compared with the CZCS period. However, the chlorophyll a concentration exhibits some regional differences during this season, leading to an explanation being difficult. The deepened MLD may have contributed to the positive chlorophyll a concentration anomalies from the northwestern Luzon Island to the northeastern region of Vietnam during April and May. The increases of chlorophyll a concentration in northwestern Borneo during May may be because the stronger SSW and higher WS produce a deeper mixed layer and convective mixing, leading to high levels of nutrient concentrations. The higher chlorophyll a off southeastern Vietnam may be associated with the advective transport of the colder water extending from the Karimata Strait to southeastern Vietnam.</abstract><cop>Heidelberg</cop><pub>Springer-Verlag</pub><doi>10.1007/s00343-012-1282-9</doi><tpages>9</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0254-4059 |
ispartof | Chinese journal of oceanology and limnology, 2012-11, Vol.30 (6), p.1054-1062 |
issn | 0254-4059 2096-5508 1993-5005 2523-3521 |
language | eng |
recordid | cdi_proquest_journals_1170530060 |
source | ProQuest Central Essentials; ProQuest Central (Alumni Edition); ProQuest Central Student; SpringerNature Journals; ProQuest Central Korea; ProQuest Central UK/Ireland; Alma/SFX Local Collection; ProQuest Central |
subjects | Algae Carbon cycle Chlorophyll Chlorophylls Climate science Coastal zone Coastal Zone Color Scanner Coastal zones coasts color Earth and Environmental Science Earth Sciences Field of view Marine Mixed layer Mixed layer depth Nutrient concentrations nutrient content Oceanography Sea surface Sea surface temperature Sea-viewing Wide Field-of-view Sensor Seasonal variation Seasonal variations SeaWiFS spring Surface temperature Surface wind Wind speed Wind stress 中国南海 可能机制 叶绿素a浓度 季节变化特征 年代际变化 海洋观测 混合层深度 |
title | Decadal variability of chlorophyll a in the South China Sea: a possible mechanism |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-15T21%3A37%3A23IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Decadal%20variability%20of%20chlorophyll%20a%20in%20the%20South%20China%20Sea%EF%BC%9A%20a%20possible%20mechanism&rft.jtitle=Chinese%20journal%20of%20oceanology%20and%20limnology&rft.au=Liu,%20Fenfen&rft.date=2012-11-01&rft.volume=30&rft.issue=6&rft.spage=1054&rft.epage=1062&rft.pages=1054-1062&rft.issn=0254-4059&rft.eissn=1993-5005&rft_id=info:doi/10.1007/s00343-012-1282-9&rft_dat=%3Cproquest_cross%3E1257760932%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1170530060&rft_id=info:pmid/&rft_cqvip_id=43767445&rfr_iscdi=true |