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Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

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


Zapytanie: NILE DELTA
Liczba odnalezionych rekordów: 1



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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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