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Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

Baza tworzona przez Bibliotekę Akademii Bialskiej im. Jana Pawła II.


Zapytanie: SUN QIANLI
Liczba odnalezionych rekordów: 3



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Autorzy: , , , , Qianli Marcin Izabela Anna Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.833IF 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM 009899.000 Q 003 Vol. 528 Narodowe Centrum Nauki SunSzymanekGałeckaTołoczko-Pasekoriginal-article996066009996.1670031-0182003Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, EgyptPalaeogeography, Palaeoclimatology, Palaeoecology20190031-01822019/202010.1016/j.palaeo.2019.04.032Nitychoruk, JerzyholoceneKopia dostępna w Sekcji Bibliometrii.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.atmospheric circulationIntertropical Convergence Zonepalaeowesterliespollen recorddiatoms.
Szczegóły:
Oznaczenie wydania: SunSzymanekGałecka
Miejsce wydania: SunSzymanekGałeckaTołoczko-Pasekoriginal-article996066009996.1670031-0182003Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, EgyptPalaeogeography, Palaeoclimatology, Palaeoecology20190031-01822019/202010.1016/j.palaeo.2019.04.032Nitychoruk, JerzyholoceneKopia dostępna w Sekcji Bibliometrii.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.atmospheric circulationIntertropical Convergence Zonepalaeowesterliespollen recorddiatoms
Wydawca: AalaQianliMarcinIzabelaAnnaOryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.833IF998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM009899.000Q003Vol. 528Narodowe Centrum Nauki
Rok wydania: 009999.0002019-11-07, 09:20yDEC-2012/05/B/ST10/00558
Charakterystyka wg MNiSW:
Język publikacji: ACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.167^b009899.000^c009999.000^d009899.000201920192019Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records i00000381710000001226AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGPRACA RECENZOWANA100^a0031-0182^bQ^iX^jXY^kQ015676^a003^b003^c2019-11-07, 09:20^d2020-06-30, 11:30^e3519979319^f3424749109^aCyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, Egypt^aPalaeogeography, Palaeoclimatology, Palaeoecology^a2019^bVol. 528^dp. 120--132^a0031-0182^a2019/2020^a10.1016/j.palaeo.2019.04.032^aNitychoruk, Jerzy^cy^aholocene^aKopia dostępna w Sekcji Bibliometrii.^aRekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego Egiptu^bNarodowe Centrum Nauki^cDEC-2012/05/B/ST10/00558^aDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.^aatmospheric circulation^aIntertropical Convergence Zone^apalaeowesterlies^apollen record^adiatoms
Wskaźnik Impact Factor ISI: ACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.167^b009899.000^c009999.000^d009899.000201920192019Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records i00000381710000001226AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGPRACA RECENZOWANA100^a0031-0182^bQ^iX^jXY^kQ015676^a003^b003^c2019-11-07, 09:20^d2020-06-30, 11:30^e3519979319^f3424749109^aCyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, Egypt^aPalaeogeography, Palaeoclimatology, Palaeoecology^a2019^bVol. 528^dp. 120--132^a0031-0182^a2019/2020^a10.1016/j.palaeo.2019.04.032^aNitychoruk, Jerzy^cy^aholocene^aKopia dostępna w Sekcji Bibliometrii.^aRekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego Egiptu^bNarodowe Centrum Nauki^cDEC-2012/05/B/ST10/00558^aDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.^aatmospheric circulation^aIntertropical Convergence Zone^apalaeowesterlies^apollen record^adiatoms
Praca recenzowana
Słowa kluczowe ang.: pSalem Aala^rSalem^sAala^u^t^qSalem A^w^x0000028618^zSalem Aala^aSun
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  • DOI:

    2/3
    Autorzy: , , , .
    Tytuł równoległy: MajeckaSzymanekChodykaTołoczko-PasekSunZhaoJiangoriginal-article995368009995.4690300-9483001Holocene lake sediments from the Faiyum Oasis in Egypt:BOREAS20180300-94832017/201810.1111/bor.12251Nitychoruk, JerzyholoceneKopia dostępna w Sekcji BibliometriiKorelacja faz osadnictwa pradziejowego i wczesnośredniowiecznego w Polsce północno-wschodniej z przemianami środowiska przyrodniczego w świetle badań osadów jeziornych (Correlation of prehistoric and early medieval settlement phases in northeast Poland with the changes of the natural environment in the light of lacus-trine sediments study)FINAL_PUBLISHEDThe Qarun Lake in the Faiyum Oasis (Egypt) provides a unique record of Holocene environmental and climate change in an arid area largely devoid of fossil proxy records. Multiple lithological, palaeontological and geochemical proxies and 32 radiocarbon dates from the 26-m-long core FA-1 provide a time series of the lake's transformation. Our results confirm that a permanent lake appeared in the Holocene at c. 10 cal. ka BP. The finely laminated lake sediments consist of diatomite, in which diatoms and ostracods together with lower concentrations of ions indicate a freshwater environment at the end of the early and middle Holocene. This freshwater supply was closely associated with regular inflows of the Nile water during flood seasons, when the Intertropical Convergence Zone (ITCZ) migrated northwards in Africa, although it has probably never reached the Faiyum Oasis. Local rainfall, possibly connected with a northern atmospheric circulation, may have been important during winter. Several phases in the lake's evolution are recognized, represented by oscillations between deep open freshwater conditions during more humid climate and shallow fresh to brackish water during drier episodes. After a long freshwater phase, the lake setting has become more brackish since c. 6.2 cal. ka BP as indicated by diatoms and increasing contents of evaporite ions in the sediment. This clearly shows that since that time the lake has occasionally become partly desiccated. This is a result of reduced discharge of the Nile. In the late Holocene the lake was mostly brackish and then gradually turned into a saline lake. This natural process was interrupted about 2.3 cal. ka BP when a man-made canal facilitated water inflow from the Nile. The examined FA-1 core can be used as a reference age model of climate change in the Holocene and its impact on the development and decline of ancient civilizations in northeastern Africa.Chodyka, Martalake sedimentsZastosowanie innowacyjnej : Aleksandra : Marcin : Marta : Anna : Qianli : Xiaoshuang : Jun : Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym3.531IF : 99964935.0000035.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR30.000PUNKTACJA UWM : 009964.000 : A : 003 : a record of environmental and climate change : Vol. 47 : 1502-3885 : Narodowe Centrum Nauki : CC-BY
    Tytuł pracy w innym języku: MajeckaSzymanekChodykaTołoczko-PasekSunZhaoJiangoriginal-article995368009995.4690300-9483001Holocene lake sediments from the Faiyum Oasis in Egypt:BOREAS20180300-94832017/201810.1111/bor.12251Nitychoruk, JerzyholoceneKopia dostępna w Sekcji BibliometriiKorelacja faz osadnictwa pradziejowego i wczesnośredniowiecznego w Polsce północno-wschodniej z przemianami środowiska przyrodniczego w świetle badań osadów jeziornych (Correlation of prehistoric and early medieval settlement phases in northeast Poland with the changes of the natural environment in the light of lacus-trine sediments study)FINAL_PUBLISHEDThe Qarun Lake in the Faiyum Oasis (Egypt) provides a unique record of Holocene environmental and climate change in an arid area largely devoid of fossil proxy records. Multiple lithological, palaeontological and geochemical proxies and 32 radiocarbon dates from the 26-m-long core FA-1 provide a time series of the lake's transformation. Our results confirm that a permanent lake appeared in the Holocene at c. 10 cal. ka BP. The finely laminated lake sediments consist of diatomite, in which diatoms and ostracods together with lower concentrations of ions indicate a freshwater environment at the end of the early and middle Holocene. This freshwater supply was closely associated with regular inflows of the Nile water during flood seasons, when the Intertropical Convergence Zone (ITCZ) migrated northwards in Africa, although it has probably never reached the Faiyum Oasis. Local rainfall, possibly connected with a northern atmospheric circulation, may have been important during winter. Several phases in the lake's evolution are recognized, represented by oscillations between deep open freshwater conditions during more humid climate and shallow fresh to brackish water during drier episodes. After a long freshwater phase, the lake setting has become more brackish since c. 6.2 cal. ka BP as indicated by diatoms and increasing contents of evaporite ions in the sediment. This clearly shows that since that time the lake has occasionally become partly desiccated. This is a result of reduced discharge of the Nile. In the late Holocene the lake was mostly brackish and then gradually turned into a saline lake. This natural process was interrupted about 2.3 cal. ka BP when a man-made canal facilitated water inflow from the Nile. The examined FA-1 core can be used as a reference age model of climate change in the Holocene and its impact on the development and decline of ancient civilizations in northeastern Africa.Chodyka, Martalake sedimentsZastosowanie innowacyjnej metody komputerowej do analizy obrazu okrzemek i zmian paleośrodowiskowychw Holocenie na Pojezierzu IławskimFaiyum Oasisenvironmental changeclimate change : Aleksandra : Marcin : Marta : Anna : Qianli : Xiaoshuang : Jun : Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym3.531IF : 99964935.0000035.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR30.000PUNKTACJA UWM : 009964.000 : A : 003 : a record of environmental and climate change : Vol. 47 : 1502-3885 : Narodowe Centrum Nauki : CC-BY : Fundusz Grantów na Badania Własne / PSW Biała Podlaska
    Szczegóły:
    Strony: MajeckaSzymanekChodykaTołoczko-PasekSunZhaoJiangoriginal-article995368009995.4690300-9483001Holocene lake sediments from the Faiyum Oasis in Egypt:BOREAS20180300-94832017/201810.1111/bor.12251Nitychoruk, JerzyholoceneKopia dostępna w Sekcji BibliometriiKorelacja faz osadnictwa pradziejowego i wczesnośredniowiecznego w Polsce północno-wschodniej z przemianami środowiska przyrodniczego w świetle badań osadów jeziornych (Correlation of prehistoric and early medieval settlement phases in northeast Poland with the changes of the natural environment in the light of lacus-trine sediments study)FINAL_PUBLISHEDThe Qarun Lake in the Faiyum Oasis (Egypt) provides a unique record of Holocene environmental and climate change in an arid area largely devoid of fossil proxy records. Multiple lithological, palaeontological and geochemical proxies and 32 radiocarbon dates from the 26-m-long core FA-1 provide a time series of the lake's transformation. Our results confirm that a permanent lake appeared in the Holocene at c. 10 cal. ka BP. The finely laminated lake sediments consist of diatomite, in which diatoms and ostracods together with lower concentrations of ions indicate a freshwater environment at the end of the early and middle Holocene. This freshwater supply was closely associated with regular inflows of the Nile water during flood seasons, when the Intertropical Convergence Zone (ITCZ) migrated northwards in Africa, although it has probably never reached the Faiyum Oasis. Local rainfall, possibly connected with a northern atmospheric circulation, may have been important during winter. Several phases in the lake's evolution are, Abdelfattah, Aleksandra, Marcin, Marta, Anna, Qianli, Xiaoshuang, Jun, Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym3.531IF, 99964935.0000035.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR30.000PUNKTACJA UWM, 009964.000, A, 003, a record of environmental and climate change, Vol. 47, 1502-3885, Narodowe Centrum Nauki, CC-BY, , , , 034, , , , , 009999.000, 2018-01-05, 14:52, Issue 1, y, UMO-2016/21/B/ST10/03059, AT_PUBLICATION, , , , WNET0202, , , , , 009969.000201820182018Holocene lake sediments from the Faiyum Oasis in Egypt: a record of environmental and climate cha00000349740000001601AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttp://onlinelibrary.wiley.com/doi/10.1111/bor.12251/abstractPRACA RECENZOWANA100, 2021-06-29, 11:48, p. 62--79, 2017-2022
    Charakterystyka formalna:
    Index Copernicus: i ^m_^n_^oSun Qianli^pSun Qianli^rSun^sQianli^u^t^qSun Q^w^x0000024855^zSun Qianli^aZhao
    Praca recenzowana
    Słowa kluczowe ang.: lat Abdelfattah^pZalat Abdelfattah^rZalat^sAbdelfattah^u^t^qZalat A^w^x0000022653^zZalat Abdelfattah^aMajecka
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    3/3
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    Autorzy: , , , , , Anna Qianli Xiaoshuang Jun 99985914.0000014.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA14.000PUNKTACJA UWM 009985.000 B 003 Vol. 34 działalność statutowa WNET PSW CC-BY-NC-ND Tołoczko-PasekSunZhaoJiang998899009999.0001641-5558001Diatom Stratigraphy of FA-1 Core, Qarun Lake, Records of Holocene Environmental and Climatic Change in Faiyum Oasis, EgyptStudia Quaternaria20171641-55582016/201710.1515/squa-017-0005Nitychoruk, JerzyholocenholoceneKopia dostepna w Sekcji BibliometriiOpracowanie nowych algorytmów analizy obrazu z wykorzystaniem sztucznych sieci komputerowychFINAL_PUBLISHEDThis study evaluates changes in the environmental and climatic conditions in the Faiyum Oasis during the Holocene based on diatom analyses of the sediment FA-1 core from the southern seashore of the Qarun Lake. The studied FA-1 core was 26 m long and covered the time span ca. 9.000 cal. yrs BP. Diatom taxa were abundant and moderately to well-preserved throughout the core sediments. Planktonic taxa were most abundant than the benthic and epiphytic forms, which were very rare and sparsely distributed. The most dominant planktonic genera were Aulacoseira and Stephanodiscus followed by frequently distribution of Cyclostephanos and Cyclotella species. The stratigraphic distribution patterns of the recorded diatoms through the Holocene sediments explained five ecological diatom groups. These groups represent distinctive environmental conditions, which were mainly related to climatic changes through the early and middle Holocene, in addition to anthropogenic activity during the late Holocene. Comparison of diatom assemblages in the studied sediment core suggests that considerable changes occurred in water level as well as salinity. There were several high stands of the freshwater lake level during humid, warmer-wet climatic phases marked by dominance of planktonic, oligohalobous and alkaliphilous diatoms alternated with lowering of the lake level and slight increases in salinity and alkalinity during warm arid conditions evident by prevalence of brackish water diatoms.Chodyka, Martaśrodowiskoenvironmentzmiany klimatuclimate changejezioro KarunQarun Lakeokrzemkidiatomsoaza FajumFaiyum OasisEgiptEgypt, Anna Qianli Xiaoshuang Jun 99985914.0000014.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA14.000PUNKTACJA UWM 009985.000 B 003 Vol. 34 działalność statutowa WNET PSW CC-BY-NC-ND Tołoczko-PasekSunZhaoJiang998899009999.0001641-5558001Diatom Stratigraphy of FA-1 Core, Qarun Lake, Records of Holocene Environmental and Climatic Change in Faiyum Oasis, EgyptStudia Quaternaria20171641-55582016/201710.1515/squa-017-0005Nitychoruk, JerzyholocenholoceneKopia dostepna w Sekcji BibliometriiOpracowanie nowych algorytmów analizy obrazu z wykorzystaniem sztucznych sieci komputerowychFINAL_PUBLISHEDThis study evaluates changes in the environmental and climatic conditions in the Faiyum Oasis during the Holocene based on diatom analyses of the sediment FA-1 core from the southern seashore of the Qarun Lake. The studied FA-1 core was 26 m long and covered the time span ca. 9.000 cal. yrs BP. Diatom taxa were abundant and moderately to well-preserved throughout the core sediments. Planktonic taxa were most abundant than the benthic and epiphytic forms, which were very rare and sparsely distributed. The most dominant planktonic genera were Aulacoseira and Stephanodiscus followed by frequently distribution of Cyclostephanos and Cyclotella species. The stratigraphic distribution patterns of the recorded diatoms through the Holocene sediments explained five ecological diatom groups. These groups represent distinctive environmental conditions, which were mainly related to climatic changes through the early and middle Holocene, in addition to anthropogenic activity during the late Holocene. Comparison of diatom assemblages in the studied sediment core suggests that considerable changes occurred in water level as well as salinity. There were several high stands of the freshwater lake level during humid, warmer-wet climatic phases marked by dominance of planktonic, oligohalobous and alkaliphilous diatoms alternated with lowering of the lake level and slight increases in salinity and alkalinity during warm arid conditions evident by prevalence of brackish water diatoms.Chodyka, Martaśrodowiskoenvironmentzmiany klimatuclimate changejezioro KarunQarun Lakeokrzemkidiatomsoaza FajumFaiyum OasisEgiptEgypt.
    Tytuł czasopisma:
    Tytuł monografii: Tołoczko-PasekSunZhaoJiang998899009999.0001641-5558001Diatom Stratigraphy of FA-1 Core, Qarun Lake, Records of Holocene Environmental and Climatic Change in Faiyum Oasis, EgyptStudia Quaternaria20171641-55582016/201710.1515/squa-017-0005Nitychoruk, JerzyholocenholoceneKopia dostepna w Sekcji BibliometriiOpracowanie nowych algorytmów analizy obrazu z wykorzystaniem sztucznych sieci komputerowychFINAL_PUBLISHEDThis study evaluates changes in the environmental and climatic conditions in the Faiyum Oasis during the Holocene based o : Anna : Qianli : Xiaoshuang : Jun : 99985914.0000014.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA14.000PUNKTACJA UWM : 009985.000 : B : 003 : Vol. 34 : działalność statutowa WNET PSW : CC-BY-NC-ND, , , , , 2300-0384, 3724009232, OPEN_JOURNAL, , , , , B, 3328888809 / / / / / 009999.000 / 2017-07-04, 10:07 / no. 1 / y / 2017-WNET/KNT/ZI/1 / AT_PUBLICATION
    Charakterystyka formalna:
    Charakterystyka merytoryczna:
    Język publikacji:
    Praca recenzowana
    Słowa kluczowe ang.: WNET^f0000000028^g^h^i*^j_^k_^lChodyka Marta^pChodyka Marta^rCHODYKA^sMARTA^u^tZakład Informatyki^qChodyka M^w930515^x0000013953^zChodyka Marta^aTołoczko-Pasek
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