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Państwowej Szkoły Wyższej w Białej Podlaskiej

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Zapytanie: SEA-LEVEL CHANGE
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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
Autorzy: , , .
Tytuł pracy:
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
Charakterystyka formalna:
Słowa kluczowe ang.: ;
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Autorzy: , , geomorphologyGotlandlimestoneraukRocky coastsea-level changewave-cut notchweathering.
Szczegóły:
Miejsce wydania: 2021/202210.3389/feart.2022.895419Zbuc
Charakterystyka wg MNiSW:
Wskaźnik Impact Factor ISI: in the degree of coastal landforms weathering; traversing micro-erosion meters (TMEM) - to calculate shore platform downwearing rates; and terrestrial laser scanning (TLS) to monitor coastal abrasion and detect sea-level markers (notches) and describe their size and shapes. Our study shows the dominance of mesoscale changes in the shore platform morphology (erosion scars, spalling, and block erosion) over the microscale downwearing carried out by abrasion. We argue that the preservation of rauks along the modern coast of Baltic islands is a result of a favorable sequence of events including the rapid land uplift and their lithological resistance, significantly higher than observed on surrounding platforms and cliffs formed in different types of limestone. Our findings prove that the microrelief of rauks in the form of well-preserved notches records the sea-level changes from at least the late Ancylus Lake period. Finally, we incorporate the results of our observations into the classic notions of rauk formation and highlight the effect of cutting off sea stacks from the operation of littoral processes as a consequence of land uplift and dominance of subaerial weathering over the wave action.^ageomorphology^aGotland^alimestone^arauk^aRocky coast^asea-level change^awave-cut notch^aweathering
Index Copernicus: holoceńskich zmian poziomu morza i rozwoju wybrzeży skalnych Bałtyku (RAUK - forgotten witness of Holocene sea-level changes and development of Baltic rocky coasts)^bNarodowe Centrum Nauki^cUMO-2016/21/D/ST10/01976^aFINAL_PUBLISHED^bCC-BY^cAT_PUBLICATION^eOPEN_JOURNAL^aIn this article, we explore the potential for sea-level change and rocky coastal evolution reconstruction hidden in one of the most intriguing rocky coastal landforms in the Baltic Sea region - rauks. Those unique limestone sea stacks are preserved along the coasts of a number of Swedish islands, with Gotland and Farö as primary locations. We contributed to the long-standing debate on their origin and attempted to investigate the modern geomorphological processes operating on rauks using novel approaches in rock coast studies, including Schmidt hammer rock tests (SHRT) - to characterize zonation in the degree of coastal landforms weathering; traversing micro-erosion meters (TMEM) - to calculate shore platform downwearing rates; and terrestrial laser scanning (TLS) to monitor coastal abrasion and detect sea-level markers (notches) and describe their size and shapes. Our study shows the dominance of mesoscale changes in the shore platform morphology (erosion scars, spalling, and block erosion) over the microscale downwearing carried out by abrasion. We argue that the preservation of rauks along the modern coast of Baltic islands is a result of a favorable sequence of events including the rapid land uplift and their lithological resistance, significantly higher than observed on surrounding platforms and cliffs formed in different types of limestone. Our findings prove that the microrelief of rauks in the form of well-preserved notches records the sea-level changes from at least the late Ancylus Lake period. Finally, we incorporate the results of our observations into the classic notions of rauk formation and highlight the effect of cutting off sea stacks from the operation of littoral processes as a consequence of land uplift and dominance of subaerial weathering over the wave action.^ageomorphology^aGotland^alimestone^arauk^aRocky coast^asea-level change^awave-cut notch^aweathering
Słowa kluczowe ang.: ; ;
Inne bazy podające opis:
  • f coastal landforms weathering; traversing micro-erosion meters (TMEM) - to calculate shore platform downwearing rates; and terrestrial laser scanning (TLS) to monitor coastal abrasion and detect sea-level markers (notches) and describe their size and shapes. Our study shows the dominance of mesoscale changes in the shore platform morphology (erosion scars, spalling, and block erosion) over the microscale downwearing carried out by abrasion. We argue that the preservation of rauks along the modern coast of Baltic islands is a result of a favorable sequence of events including the rapid land uplift and their lithological resistance, significantly higher than observed on surrounding platforms and cliffs formed in different types of limestone. Our findings prove that the microrelief of rauks in the form of well-preserved notches records the sea-level changes from at least the late Ancylus Lake period. Finally, we incorporate the results of our observations into the classic notions of rauk formation and highlight the effect of cutting off sea stacks from the operation of littoral processes as a consequence of land uplift and dominance of subaerial weathering over the wave action.^ageomorphology^aGotland^alimestone^arauk^aRocky coast^asea-level change^awave-cut notch^aweathering


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