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Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

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


Zapytanie: SALEM ALAA
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Nr opisu: 0^b998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.700^b009899.000^c009999.000^d009899.000202220222022High-resolution insight into the Holocene environmental history of the Burullus Lagoon in norther00000426000000000609AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://www.cambridge.org/core/journals/quaternary-research/article/abs/highresolution-insight-into-the-holocene-environmental-history-of-the-burullus-lagoon-in-northern-nile-delta-egypt/B3B5C71601138100^a0033-5894^bQ^e1096-0287^fA^hABC^iX^jXY^kQ016946^a003^b003^c2021-12-01, 14:27^d2023-06-28, 10:07^e3319038812^f3124769232^aHigh-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, Egypt^aQuaternary Research^a2022^bVol. 107^dp. 87--103^a0033-5894^b1096-0287^a2021/2022^a10.1017/qua.2021.63^aNitychoruk, Jerzy^cy^aclimate change^aFINAL_PUBLISHED^bCC-BY-NC-ND^cAT_PUBLICATION^eOPEN_JOURNAL^aThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity of the Burullus Lagoon at 6.0-5.5 and 4.8-4.2 cal ka BP reflected droughts in the Nile catchment. Thereafter, the river reactivated in the Burullus Lagoon area, and since 2.8 cal ka BP was accompanied by occasional inflows of sea water. Since ca. 0.8 cal ka BP, increased fluvial activity occurred in this part of the Nile delta, which terminated after construction of the Aswan dams in the twentieth century.^aEastern Mediterranean^aIntertropical Convergence Zone^alagoon^aNile delta^asea-level change^aSebennitic branch.300IF^a996600^b998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.700^b009899.000^c009999.000^d009899.000202220222022High-resolution insight into the Holocene environmental history of the Burullus Lagoon in norther00000426000000000609AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://www.cambridge.org/core/journals/quaternary-research/article/abs/highresolution-insight-into-the-holocene-environmental-history-of-the-burullus-lagoon-in-northern-nile-delta-egypt/B3B5C71601138100^a0033-5894^bQ^e1096-0287^fA^hABC^iX^jXY^kQ016946^a003^b003^c2021-12-01, 14:27^d2023-06-28, 10:07^e3319038812^f3124769232^aHigh-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, Egypt^aQuaternary Research^a2022^bVol. 107^dp. 87--103^a0033-5894^b1096-0287^a2021/2022^a10.1017/qua.2021.63^aNitychoruk, Jerzy^cy^aclimate change^aFINAL_PUBLISHED^bCC-BY-NC-ND^cAT_PUBLICATION^eOPEN_JOURNAL^aThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity of the Burullus Lagoon at 6.0-5.5 and 4.8-4.2 cal ka BP reflected droughts in the Nile catchment. Thereafter, the river reactivated in the Burullus Lagoon area, and since 2.8 cal ka BP was accompanied by occasional inflows of sea water. Since ca. 0.8 cal ka BP, increased fluvial activity occurred in this part of the Nile delta, which terminated after construction of the Aswan dams in the twentieth century.^aEastern Mediterranean^aIntertropical Convergence Zone^alagoon^aNile delta^asea-level change^aSebennitic branch
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Tytuł pracy w innym języku: NitychorukChenSalemZalatoriginal-article996600009996.7000033-5894003High-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, EgyptQuaternary Research20220033-58942021/202210.1017/qua.2021.63Nitychoruk, Jerzyclimate changeFINAL_PUBLISHEDThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity of the Burullus Lagoon at 6.0-5.5 and 4.8-4.2 cal ka BP reflected droughts in the Nile catchment. Thereafter, the river reactivated in the Burullus Lagoon area, and since 2.8 cal ka BP was accompanied by occasional inflows of sea water. Since ca. 0.8 cal ka BP, increased fluvial activity occurred in this part of the Nile delta, which terminated after construction of the Aswan dams in the twentieth century.Eastern MediterraneanIntertropical Convergence ZonelagoonNile deltasea-level changeSebennitic branch : Jerzy Antoni : Zhongyuan : Alaa : Abdelfattah : Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.300IF : 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM : 009899.000 : Q : 003 : Vol. 107 : 1096-0287 : CC-BY-NC-ND
Miejsce wydania: NitychorukChenSalemZalatoriginal-article996600009996.7000033-5894003High-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, EgyptQuaternary Research20220033-58942021/202210.1017/qua.2021.63Nitychoruk, Jerzyclimate changeFINAL_PUBLISHEDThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed
Wydawca: Jerzy AntoniZhongyuanAlaaAbdelfattahOryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.300IF998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM009899.000Q003Vol. 1071096-0287CC-BY-NC-ND
Rok wydania: 033009999.0002021-12-01, 14:27yAT_PUBLICATION
Strony: NitychorukChenSalemZalatoriginal-article996600009996.7000033-5894003High-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, EgyptQuaternary Research20220033-58942021/202210.1017/qua.2021.63Nitychoruk, Jerzyclimate changeFINAL_PUBLISHEDThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity, Jerzy Antoni, Zhongyuan, Alaa, Abdelfattah, Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.300IF, 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM, 009899.000, Q, 003, Vol. 107, 1096-0287, CC-BY-NC-ND, 033, , , , 009999.000, 2021-12-01, 14:27, y, AT_PUBLICATION, WNET0201, , , , 009899.000202220222022High-resolution insight into the Holocene environmental history of the Burullus Lagoon in norther00000426000000000609AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://www.cambridge.org/core/journals/quaternary-research/article/abs/highresolution-insight-into-the-holocene-environmental-history-of-the-burullus-lagoon-in-northern-nile-delta-egypt/B3B5C71601138100, 2023-06-28, 10:07, p. 87--103
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Nr opisu: and geoarcheological research^aThe 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regions^bprogramme and book of abstracts^aP. 30^aZagreb^c2018^a2018/2019^aNitychoruk, Jerzy^cy^alake sediments^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^d2013-2016^aThe 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regions^bInstitute of Archeology Cardinal Stefan Wyszyński University in Warsaw, Institute of Archeology in Zagreb^aZagreb^dHR^b2018.10.23^c2018.10.24^aenvironmental conditions^aholocene^aFaiyum Oasis^aEgypt
Autorzy: , , .
Tytuł pracy w innym języku: SalemMajecka998899009999.000003Environmental conditions in late Antiquty in the Faiyum Oasis (Egypt) based on the Lake Qarun sediments studies and geoarcheological researchThe 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regionsP. 30Zagreb2018/2019Nitychoruk, Jerzylake sedimentsKopia dostępna w Sekcji Bibliometrii.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuThe 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regionsZagrebenvironmental conditionsholoceneFaiyum OasisEgypt : Alaa : Aleksandra : 999999BEZ PUNKTACJI UWM : 009999.000 : 003 : programme and book of abstracts : Narodowe Centrum Nauki : Institute of Archeology Cardinal Stefan Wyszyński University in Warsaw, Institute of Archeology in Zagreb : 2018.10.23
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Uwagi: SalemMajecka998899009999.000003Environmental conditions in late Antiquty in the Faiyum Oasis (Egypt) based on the Lake Qarun sediments studies and geoarcheological researchThe 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regionsP. 30Zagreb2018/2019Nitychoruk, Jerzylake sedimentsKopia dostępna w Sekcji Bibliometrii.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuThe 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regionsZagrebenvironmental conditionsholoceneFaiyum OasisEgypt
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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
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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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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
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    Nr opisu: 15^x0000013953^zChodyka Marta^aSzymanek
    Autorzy: , , , , Marcin Anna Oryginalny artykuł naukowyACPartykuł w czasopiśmie polskim 99985914.0000014.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA14.000PUNKTACJA MNISW4L 009985.000 B 003 Vol. 33 2300-0384 Narodowe Centrum Nauki CC-BY-NC-ND SzymanekTołoczko-Pasekoriginal-article998899009999.0001641-5558003Preliminary report on unique laminated holocene sediments from the Qarun Lake in EgyptStudia Quaternaria20161641-55582015/201610.1515/squa-2016-0004Nitychoruk, JerzyholocenholoceneKopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuFINAL_PUBLISHEDThe Lake Qarun (Faiyum Oasis, northern Egypt) is a relic of the much larger Holocene lake. Past lake levels and extensions were reconstructed, based on setting of archaeological sites scattered along northern paleoshores of the ancient lake. However, geoarcheological works did not yield enough data to establish continuous environmental history of the lake. A deep drilling FA-1 on the southeastern shore of the lake, performed in 2014, supplied with a core, 26 m long that is the one of the longest lake sediment cores in northeastern Africa. The basal section of the core consisted of thin-laminated diatom marly deposits, underlain at the Late Pleistocene/Holocene boundary by coarse-grained sands. The sediment lamine were quite well developed, especially in the lower part of the core. Preliminary results indicated annually deposited sediment sequence with seasonality signals provided by microlamine of diatoms, calcite, organic matter and clastic material. Early Holocene varved sediments from the Faiyum Oasis supplied with exceptional paleoenvironmental data for northeastern Africa, which enriched a record from previous logs drilled at the southwestern margin of the Qarun Lake.Chodyka, Martaosady jeziornelaminated sedimentsosady laminowaneQarun Lakejezioro KarunFaiyum OasisFajumEgyptEgipt.
    Szczegóły:
    Uwagi: SzymanekTołoczko-Pasekoriginal-article998899009999.0001641-5558003Preliminary report on unique laminated holocene sediments from the Qarun Lake in EgyptStudia Quaternaria20161641-55582015/201610.1515/squa-2016-0004Nitychoruk, JerzyholocenholoceneKopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuFINAL_PUBLISHEDThe Lake Qarun (Faiyum Oasis, northern Egypt) is a relic of the much larger Holocene lake. Past lake levels and extensions were reconstructed, based on setting of archaeological sites scattered along northern paleoshores of the ancient lake. However, geoarcheological works did not yield enough data to establish continuous environmental history of the lake. A deep drilling FA-1 on the southeastern shore of the lake, performed in 2014, supplied with a core, 26 m long that is the one of the longest lake sediment cores in northeastern Africa. The basal section of the core consisted of thin-laminated diatom marly deposits, underlain at the Late Pleistocene/Holocene boundary by coarse-grained sands. The sediment lamine were quite well developed, especi
    Punktacja ministerstwa: ka Marta^aSzymanek
    Praca recenzowana
    Słowa kluczowe ang.: ad Informatyki^qChodyka M^w930515^x0000013953^zChodyka Marta^aSzymanek
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    6/6
    Autorzy: , , , .
    Tytuł pracy w innym języku: ChenChodykaMajeckaToloczkoSzymanekZalatabstract998899009999.000003Dynamics of Holocene climate change in northeastern Africa recorded in laminated lake sediments from Faiyum Oasis, EgyptXIX INQUA Congress Quaternary Perspectoves on Climate Change, Natural Hazards and Civilization at Nagoya Congress Center, Nagoya, Japan 26 July - 2 August 2015T00268Oral presentation P27-06.Tokyo2015/2016Nitychoruk, Jerzyzmiany klimatyczneKopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki PSW.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuXIX INQUA Congress Quaternary Perspectives on Climate Change, Natural Hazards and CivilizationNagoyaChodyka, Martaholocenosady laminowaneEgipt : Zhongyuan : Marta : Aleksandra : Anna : Marcin : Abdelfattah : AbstraktSZMstreszczenie zjazdowe międzynarodowe (książka streszczeń) : 999999 : 009999.000 : 003 : Science Council of Japan, Japan Association for Quaternary Research, International Union for Quaternary Research : Narodowe Centrum Nauki : 2015.07.26
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    Uwagi: ChenChodykaMajeckaToloczkoSzymanekZalatabstract998899009999.000003Dynamics of Holocene climate change in northeastern Africa recorded in laminated lake sediments from Faiyum Oasis, EgyptXIX INQUA Congress Quaternary Perspectoves on Climate Change, Natural Hazards and Civilization at Nagoya Congress Center, Nagoya, Japan 26 July - 2 August 2015T00268Oral presentation P27-06.Tokyo2015/2016Nitychoruk, Jerzyzmiany klimatyczneKopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki PSW.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuXIX INQUA Congress Quaternary Perspectives on Climate Change, Natural Hazards and CivilizationNagoya
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