7/17
Nr opisu: ccumulation on talus cones, and movement of the protalus rampart. The measurements were performed in 1987, 2007 and 2016. The results obtained revealed a very slow rate of changes on the surface of the analysed area. During 30 years, only one out of 84 points where the gelifluction rate was measured was displaced by 15 cm down-slope. The maximal annual and average gelifluction rates were calculated at 0.5 cm and 0.18 cm a-1, respectively. Several measurement points did not change their position over the observation period. As shown by the observations, the gelifluction rate largely does not depend on slope inclination. Studies of talus cones allowed the level of cone increment to be determined as 314.3 kg of scree per square metre. Analysis of factors influencing the rate of mass movement allowed for correlation of the small-scale gelifluction movement at the analysed sites with the general trends of climate warming. In this part of the Arctic, these trends are manifested by soil desiccation. It appears that slope processes depend on very local topoclimatic factors. Analysis of the obtained data with regard to palaeogeographical and climatic investigations suggests that the ice segregation forms on raised marine terraces developed during the last Holocene cooling, i.e. the Little Ice Age.^awaste movement^agelifluction^aScottbreen glacier^aArctic^aSpitsbergen Autorzy: , waste movementgelifluctionScottbreen glacierArcticSpitsbergen. Tytuł czasopisma: Strony: Charakterystyka merytoryczna: Język publikacji: Wskaźnik Impact Factor ISI: Punktacja ministerstwa: Praca recenzowana Słowa kluczowe ang.: rt of the Arctic, these trends are manifested by soil desiccation. It appears that slope processes depend on very local topoclimatic factors. Analysis of the obtained data with regard to palaeogeographical and climatic investigations suggests that the ice segregation forms on raised marine terraces developed during the last Holocene cooling, i.e. the Little Ice Age.^awaste movement^agelifluction^aScottbreen glacier^aArctic^aSpitsbergen Słowa kluczowe ang.: ; ;
9/17
Nr opisu: the natural environment in the light of lacus-trine sediments study)^bNarodowe Centrum Nauki^cUMO-2016/21/B/ST10/03059^d2017-2022^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^apalynology^anort-eastern Poland^aRoman periods^aMigration periods Autorzy: , . Tytuł pracy w innym języku: 003Environmental transformations during Roman and Migration Periods (100-700 AD) reflected in palynological data from selected lakes in the north-eastern PolandThe 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regionsP. 19Zagreb2018/2019Nitychoruk, Jerzyenvironmental transformationsKopia dostępna w Sekcji Bibliometrii.Korelacja 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)The 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regionsZagrebpalynologynort-eastern PolandRoman periodsMigration periods : 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 Strony: 003Environmental transformations during Roman and Migration Periods (100-700 AD) reflected in palynological data from selected lakes in the north-eastern PolandThe 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regionsP. 19Zagreb2018/2019Nitychoruk, Jerzyenvironmental transformationsKopia dostępna w Sekcji Bibliometrii.Korelacja 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 , 003, programme and book of abstracts, 2019-01-03, 10:00, 2018, y, 2021-06-29, 11:47 Strony zajęte przez pracę: Miejsce wydania: The 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regionsZagrebpalynologynort-eastern PolandRoman periodsMigration periods : Narodowe Centrum Nauki : Institute of Archeology Cardinal Stefan Wyszyński University in Warsaw, Institute of Archeology in Zagreb : 2018.10.23, UMO-2016/21/B/ST10/03059, 2018.10.24 Charakterystyka formalna: Słowa kluczowe ang.: ; Projekt/grant:
10/17
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 Słowa kluczowe ang.: Uwaga: DOI: Streszczenie: Projekt/grant:
12/17
Nr opisu: asz Jan^c047^dWNET0105^eWNET^f0000000227^g^h^i*^j_^k_^lZbucki Łukasz Jan^pZbucki Łukasz Jan^rZBUCKI^sŁUKASZ JAN^u^tZakład Gospodarki Przestrzennej^qZbucki Ł^w930623^x0000009201^zZbucki Łukasz JanWoronko Barbara Nitychoruk Jerzy Antoni Hrychanik Mikalai Majecka Aleksandra Marks Leszek Pochocka-Szwarc Katarzyna^achapter-in-a-book^bRozdział w książce^apeer-reviewed^bPublikacja recenzowanaRMProzdział w monografii polskiej^a998899^b9999992.500PUNKTACJA UWM^a009999.000^b009999.000^c009999.000^d009996.500201720172017Interpretacja budowy geologicznej w odsłonięciach reperowych0000034528000000197200000345270.000PUBLIKACJAPEŁNA PUBLIKACJAROProzdział w monografii - j. polski lub innym poza kongres.AFILIACJA PODANAPOLPRACA RECENZOWANA200^a001^b003^c2017-10-05, 14:42^d2021-12-02, 15:49^e3720998797^f3319028690^aInterpretacja budowy geologicznej w odsłonięciach reperowych^aMapa geologiczna południowej części obszaru przygranicznego Polski i Białorusi^brejon Białej Podlaskiej i Brestu 1:250 000 : tekst objaśniający^cred. nauk. Leszek Marks, Alexandr K. Karabanov^aS. 24-82^aWarszawa^bPaństwowy Instytut Geologiczny - Państwowy Instytut Badawczy^c2017^a978-83-7863-768-4^b2,9^aZbucki, Łukasz^cy^abudowa geologiczna^aKopia dostepna w Sekcji Bibliometrii.^aModel of geological structure, regional key horizons and Middle-Late Pleistocene climate in the southern part of the Polish-Belarusian cross-border area^bNarodowe Centrum Nauki^c2013/09/B/ST10/02040^aNitychoruk, Jerzy^cy^astrefa marginalna lądolodu^astadiał Warty/Soża^aobszar przygraniczny^aBiałoruś Zachodnia^aNizina Południowopodlaskaasz Jan^c047^dWNET0105^eWNET^f0000000227^g^h^i*^j_^k_^lZbucki Łukasz Jan^pZbucki Łukasz Jan^rZBUCKI^sŁUKASZ JAN^u^tZakład Gospodarki Przestrzennej^qZbucki Ł^w930623^x0000009201^zZbucki Łukasz JanWoronko Barbara Nitychoruk Jerzy Antoni Hrychanik Mikalai Majecka Aleksandra Marks Leszek Pochocka-Szwarc Katarzyna^achapter-in-a-book^bRozdział w książce^apeer-reviewed^bPublikacja recenzowanaRMProzdział w monografii polskiej^a998899^b9999992.500PUNKTACJA UWM^a009999.000^b009999.000^c009999.000^d009996.500201720172017Interpretacja budowy geologicznej w odsłonięciach reperowych0000034528000000197200000345270.000PUBLIKACJAPEŁNA PUBLIKACJAROProzdział w monografii - j. polski lub innym poza kongres.AFILIACJA PODANAPOLPRACA RECENZOWANA200^a001^b003^c2017-10-05, 14:42^d2021-12-02, 15:49^e3720998797^f3319028690^aInterpretacja budowy geologicznej w odsłonięciach reperowych^aMapa geologiczna południowej części obszaru przygranicznego Polski i Białorusi^brejon Białej Podlaskiej i Brestu 1:250 000 : tekst objaśniający^cred. nauk. Leszek Marks, Alexandr K. Karabanov^aS. 24-82^aWarszawa^bPaństwowy Instytut Geologiczny - Państwowy Instytut Badawczy^c2017^a978-83-7863-768-4^b2,9^aZbucki, Łukasz^cy^abudowa geologiczna^aKopia dostepna w Sekcji Bibliometrii.^aModel of geological structure, regional key horizons and Middle-Late Pleistocene climate in the southern part of the Polish-Belarusian cross-border area^bNarodowe Centrum Nauki^c2013/09/B/ST10/02040^aNitychoruk, Jerzy^cy^astrefa marginalna lądolodu^astadiał Warty/Soża^aobszar przygraniczny^aBiałoruś Zachodnia^aNizina Południowopodlaska Autorzy: , , , . Miejsce wydania: MarksPochocka-SzwarcRychelRylovaSzymanekZbuckichapter-in-a-bookpeer-reviewed998899009999.000001Interpretacja budowy geologicznej w odsłonięciach reperowychMapa geologiczna południowej części obszaru przygranicznego Polski i BiałorusiS. 24-82Warszawa978-83-7863-768-4Zbuck Wydawca: LeszekKatarzynaJoannaTatsyanaMarcinŁukasz JanRozdział w książcePublikacja recenzowanaRMProzdział w monografii polskiej9999992.500PUNKTACJA UWM009999.000003rejon Białej Podlaskiej i Brestu 1:250 000 : tekst objaśniającyPaństwowy Instytut Geologiczny - Państwowy Instytut Badawczy2,9 Rok wydania: 047009999.0002017-10-05, 14:42red. nauk. Leszek Marks, Alexandr K. Karabanov2017 ISBN: MarksPochocka-SzwarcRychelRylova Tytuł całości: W: ISBN: Słowa kluczowe: ;
13/17
Nr opisu: rtress. The remains of the wooden building located directly on the prehistoric lacustrine sediments created a unique opportunity to reconstruct the near-shore sedimentation of the Drużno Lake. Geological, malacological and palynological methods were applied during the investigation. The results, compared with the ranges of both the Drużno Lake and the Vistula Lagoon, known from previous studies of the region, allowed the correlation of a phase of a deep lake with the "Roman Period". Rapid shallowing of the lake occured in the "Migration Period". The final disappearance of the lake in the area of modern Elbląg occured in the early Middle Ages.^aZbucki, Łukasz^cy^atwierdza krzyżacka^aTeutonic fortress^amalakologia^amalacology^apalinologia^apalynology Autorzy: . Tytuł pracy w innym języku: 0001-5709003Changes for sedimentation in the Drużno Lake based on geoarchaeological data from the Teutonic fortress in Elbląg, North PolandActa Geologica Polonica20160001-57092015/201610.1515/agp-2016-0004Nitychoruk, Jerzyosady jeziorneLacustrine sedimentsIF za rok Kopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki PSW.FINAL_PUBLISHEDThe wooden structures unearthed in 2012 during archaeological excavation in the courtyard of the Museum of Archaeology and History in Elbląg have been dated using the dendrochronological method to the period between 1245 and 1302, which allows them to be considered to be parts of a Teutonic fortress. The remains of the wooden building located directly on the prehistoric lacustrine sediments created a unique opportunity to reconstruct the near-shore sedimentation of the Drużno Lake. Geological, malacological and palynological methods were applied during the investigation. The results, compared with the ranges of both the Drużno Lake and the Vistula Lagoon, known from previous studies of the region, allowed the correlation of a phase of a deep lake with the "Roman Period". Rapid shallowing of the lake occured in the "Migration Period". The final disappearance of the lake in the area of modern Elbląg occured in the early Middle Ages.Zbucki, Łukasztwierdza krzyżackaTeutonic fortressmalakologiamalacologypalinologiapalynology : A : 001 : Vol. 66 : OTHER Szczegóły: Tytuł monografii w innym języku: 0001-5709003Changes for sedimentation in the Drużno Lake based on geoarchaeological data from the Teutonic fortress in Elbląg, North PolandActa Geologica Polonica20160001-57092015/201610.1515/agp-2016-0004Nitychoruk, Jerzyosady jeziorneLacustrine sedimentsIF za rok Kopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki PSW.FINAL_PUBLISHEDThe wooden structures unearthed in 2012 during archaeological excavation in the courtyard of the Museum of Archaeology and History in Elbląg have been dated using the dendrochronological method to the period between 1245 and 1302, which allows them to be considered to be parts of a Teutonic fortress. The remains of the wooden building located directly on the prehistoric lacustrine sediments created a unique opportunity to reconstruct the near-shore sedimentation of the Drużno Lake. Geological, malacological and palynological methods were applied during the investigation. The results, compared with the ranges of both the Drużno Lake and the Vistula Lagoon, known from previous studies of the region, allowed the correlation of a phase of a deep lake with the "Roman Period". Rapid shallowing of the lake occured in the "Migration Period". The final disappearance of the lake in the area of modern Elbląg occured in the early Middle Ages.Zbucki, Łukasztwierdza krzyżackaTeutonic fortressmalakologiamalacologypalinologiapalynology : A : 001 : Vol. 66 : OTHER Charakterystyka formalna: Punktacja ministerstwa: ew/25291/17234PRACA RECENZOWANA100^a0001-5709^bA^fA^gABC^hABC^iX^jXY^a003^b001^c2016-02-02, 12:57^d2017-06-19, 09:30^e3829028982^f3724859309^aChanges for sedimentation in the Drużno Lake based on geoarchaeological data from the Teutonic fortress in Elbląg, North Poland^aActa Geologica Polonica^a2016^bVol. 66^cno. 1^dp. 85--98^a0001-5709^a2015/2016^a10.1515/agp-2016-0004^aNitychoruk, Jerzy^cy^aosady jeziorne^aLacustrine sediments^aIF za rok Kopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki PSW.^aFINAL_PUBLISHED^bOTHER^cAT_PUBLICATION^eOPEN_JOURNAL^aThe wooden structures unearthed in 2012 during archaeological excavation in the courtyard of the Museum of Archaeology and History in Elbląg have been dated using the dendrochronological method to the period between 1245 and 1302, which allows them to be considered to be parts of a Teutonic fortress. The remains of the wooden building located directly on the prehistoric lacustrine sediments created a unique opportunity to reconstruct the near-shore sedimentation of the Drużno Lake. Geological, malacological and palynological methods were applied during the investigation. The results, compared with the ranges of both the Drużno Lake and the Vistula Lagoon, known from previous studies of the region, allowed the correlation of a phase of a deep lake with the "Roman Period". Rapid shallowing of the lake occured in the "Migration Period". The final disappearance of the lake in the area of modern Elbląg occured in the early Middle Ages.^aZbucki, Łukasz^cy^atwierdza krzyżacka^aTeutonic fortress^amalakologia^amalacology^apalinologia^apalynology Praca recenzowana Słowa kluczowe ang.: DANAENGhttps://geojournals.pgi.gov.pl/agp/article/view/25291/17234PRACA RECENZOWANA100^a0001-5709^bA^fA^gABC^hABC^iX^jXY^a003^b001^c2016-02-02, 12:57^d2017-06-19, 09:30^e3829028982^f3724859309^aChanges for sedimentation in the Drużno Lake based on geoarchaeological data from the Teutonic fortress in Elbląg, North Poland^aActa Geologica Polonica^a2016^bVol. 66^cno. 1^dp. 85--98^a0001-5709^a2015/2016^a10.1515/agp-2016-0004^aNitychoruk, Jerzy^cy^aosady jeziorne^aLacustrine sediments^aIF za rok Kopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki PSW.^aFINAL_PUBLISHED^bOTHER^cAT_PUBLICATION^eOPEN_JOURNAL^aThe wooden structures unearthed in 2012 during archaeological excavation in the courtyard of the Museum of Archaeology and History in Elbląg have been dated using the dendrochronological method to the period between 1245 and 1302, which allows them to be considered to be parts of a Teutonic fortress. The remains of the wooden building located directly on the prehistoric lacustrine sediments created a unique opportunity to reconstruct the near-shore sedimentation of the Drużno Lake. Geological, malacological and palynological methods were applied during the investigation. The results, compared with the ranges of both the Drużno Lake and the Vistula Lagoon, known from previous studies of the region, allowed the correlation of a phase of a deep lake with the "Roman Period". Rapid shallowing of the lake occured in the "Migration Period". The final disappearance of the lake in the area of modern Elbląg occured in the early Middle Ages.^aZbucki, Łukasz^cy^atwierdza krzyżacka^aTeutonic fortress^amalakologia^amalacology^apalinologia^apalynology Słowa kluczowe: Słowa kluczowe ang.: ; DOI: Streszczenie:
16/17
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 Tytuł całości: W: Miejsce wydania: Wydawca: Rok wydania: 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 Słowa kluczowe: ;
17/17
Nr opisu: Adres wydawniczy: Kopia niedostępna: Słowa kluczowe: Słowa kluczowe:
