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Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

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



Zapytanie: HOLOCENE
Liczba odnalezionych rekordów: 11



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1/11
Nr opisu: 0000046183
Autorzy: Natalya Yu. Zharinova, Galina Yu. Yamskikh, Łukasz Jan Zbucki, Darya E. Makarchuk.
Tytuł pracy: Geochemistry of Holocene - Late Pleistocene sediments in the Berezovka River valley (Near-Yenisey Siberia)
Tytuł czasopisma:
Szczegóły: 2023, Vol. 68, no. 2, p. 311--330
p-ISSN: 2541-9668
e-ISSN: 2587-585X

Charakterystyka formalna: artykuł w czasopiśmie zagranicznym
Charakterystyka merytoryczna: artykuł oryginalny naukowy
Charakterystyka wg MNiSW: artykuł w czasopiśmie bez IF (wykaz MEiN)
Język publikacji: ENG
Punktacja ministerstwa: 20.000
Słowa kluczowe ang.: alluvial soil ; Berezovka River ; floodplain terrace ; forest-steppe ; geochemistry ; holocene ; late pleistocene ; radiocarbon dating ; sediments
https://escjournal.spbu.ru/article/view/13878
DOI: 10.21638/spbu07.2023.206
Streszczenie: Despite their great importance, Holocene-Late Pleistocene sediments are poorly studied in the valleys of rivers in the Krasnoyarsk forest-steppe territory. We present the first detailed study of the geochemical composition of the first floodplain terrace sediments in the valley of the Berezovka River, and the continuous accumulation that occurred at the Late Pleistocene-Holocene (from 20833 ą 519 cal yr BP). This is of great fundamental importance and is the basis for further studies on the influence of anthropogenic activities on the natural environment in the Krasnoyarsk agglomeration. The sediments were covered by modern alluvial dark-humus hydrometamorphosed soil. Macromorphological studies and investigation of the humus content have revealed a well-developed process of humus formation and humus accumulation, a gley process. The measured contents of some elements (U, Pr, Rb, V, Bi, Cd, As, Th, Ga, Co, and Sm) exceeded the respective Clarke values for the Earth's crust. The distribution of most elements and their accumulation in the Middle-Late Holocene (from to 5477-4985 to 1241-803 cal yr BP) in the middle of the sediment profile is explained by the high content of mud and clay minerals. Based on the coefficients of radial migration, we established that most of the studied elements were introduced into the sediments during high water levels and floods. The values of palaeomarkers indicate a change in climatic conditions in the Late Pleistocene and Holocene from dry and cold to more humid and warm, and from arid and cold (in the Early Holocene) to modern climatic conditions, respectively.

2/11
Nr opisu: 0000046423
Autorzy: Joanna Mirosław-Grabowska, Edyta Zawisza, Milena Obremska, Joanna Kowalczyk, Łukasz Jan Zbucki, Kazimierz Tobolski.
Tytuł pracy: Human impact recorded in lake environment (Charzykowskie Lake, N Poland) during the last 6,200 years
Tytuł czasopisma:
Szczegóły: 2023, Vol. 73, no. 3, p. 467--478
p-ISSN: 0001-5709

Charakterystyka formalna: artykuł w czasopiśmie polskim
Charakterystyka merytoryczna: artykuł oryginalny naukowy
Charakterystyka wg MNiSW: artykuł w czasopiśmie z IF (wykaz MEiN)
Język publikacji: ENG
Wskaźnik Impact Factor ISI: 1.100
Punktacja ministerstwa: 100.000
Słowa kluczowe ang.: geochemistry ; holocene ; human impact ; lake sediments ; Poland ; subfossil cladocera
https://geojournals.pgi.gov.pl/agp/article/view/33881
DOI: 10.24425/agp.2023.145612
Streszczenie: Based on geochemical and biological investigations of a 6-m-long sediment core, a reconstruction of the environmental conditions in Charzykowskie Lake (northern Poland) is presented. The analyzed sediments consist of fine calcareous detritus gyttja interbedded by lake marl. The results of palynological analysis document the vegetation development around and in the studied lake and confirm the middle and late Holocene age of the sedimentation of the deposits. The identification of 22 taxa of subfossil Cladocera shows the biodiversity of the fauna and reflects the changes in the trophic and water level. The concentrations of various chemical elements suggest the origin of the sediments. Geochemical, including isotope, and biological data, made it possible to reconstruct the environmental conditions, as well as traces of human influence over the last ca. 6,200 years. Four stages of human impact have been documented by the pollen data. The first traces of human groups in the vicinity of Charzykowskie Lake are preserved in sediments from about 4,000 years ago. The human activity is poorly recorded in the Cladocera and in the geochemical compositions of the lake sediments, probably due to the size and depth of the lake and its isolation.

3/11
Nr opisu: 0000041902
Autorzy: Fabian Welc, Jerzy Antoni Nitychoruk, Leszek Marks, Krzysztof Bińka, Anna Rogóż-Matyszczak, Milena Obremska, Abdelfattah Zalat.
Tytuł pracy: 2400 years of climate and human-induced environmental change recorded in sediments of Lake Młynek in northern Poland
Tytuł czasopisma:
Szczegóły: 2021, Vol. 17, issue 3, p. 1181--1198
p-ISSN: 1814-9324
e-ISSN: 1814-9332

Charakterystyka formalna: artykuł w czasopiśmie zagranicznym
Charakterystyka merytoryczna: artykuł oryginalny naukowy
Charakterystyka wg MNiSW: artykuł w czasopiśmie z IF (wykaz MEiN)
Język publikacji: ENG
Wskaźnik Impact Factor ISI: 4.498
Punktacja ministerstwa: 100.000
Słowa kluczowe ang.: climate change ; environmental change ; lake sediments ; holocene ; middle age ; human activity ; Lake Młynek ; Poland
https://cp.copernicus.org/articles/17/1181/2021/
DOI: 10.5194/cp-17-1181-2021
Streszczenie: In the densely forested Warmia and Masuria region (northern Poland) there are many small endorheic lakes characterized by their low sedimentation rate, which makes them excellent archives of Holocene environmental and palaeoclimatic change. Lake Młynek, located near the village of Janiki Wielkie, was selected for multi-faceted palaeoenvironmental research supported with radiocarbon dates. Sediments from this lake also contain unique information about human impact on the environment, because a stronghold has been operating on its northern shore since the early Iron Age to the early Medieval period, giving the opportunity to correlate palaeoenvironmental data with the phases of human activity over the last 2400 years. During the second and third centuries BCE the lake was surrounded by a dense deciduous forest. From the first century BCE to second century CE the forest around the lake was much reduced, which can be associated with the first pre-Roman (La Tene) and Roman occupation phase evidenced by the construction of the stronghold located close to the lake. From the second up to ninth century CE gradual restoration of the forest and a decline in human activity took place, along with lake deepening and the onset of a colder and humid climatic phase which corresponded to the global cooling episode known as the Bond 1 event (1.5 ka BP). The next intensive phase of forest clearing around the lake occurred between the 9th-13th century CE as result of human activity (Middle Age settlement phase of the stronghold). Whilst this period is marked by a warming, the human impact which has transformed the landscape likely overprints any signals of climate-driven environmental changes.
Projekt/grant: 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) : UMO-2016/21/B/ST10/03059

4/11
Nr opisu: 0000040406
Autorzy: Krzysztof Bińka, Fabian Welc, Jerzy Antoni Nitychoruk, Dominika Sieradz, Antoni Lewczuk.
Tytuł pracy: Unique finds in palynological spectra : acetolyze resistant vegetative forms of freshwater dinoflagellate based on the Lake Młynek record form Northeastern Poland
Tytuł czasopisma:
Szczegóły: 2020, Vol. 37, no. 2, p. 59--67
p-ISSN: 1641-5558

Charakterystyka formalna: artykuł w czasopiśmie polskim
Charakterystyka merytoryczna: artykuł oryginalny naukowy
Charakterystyka wg MNiSW: artykuł w czasopiśmie bez IF (wykaz MEiN)
Język publikacji: ENG
Punktacja ministerstwa: 70.000
Słowa kluczowe ang.: freshwater dinoflagellate ; microfossil ; human impact ; holocene ; Lake Młynek ; Poland
http://www.studia.quaternaria.pan.pl/pdfs/sq37-2/1_Binka.pdf
DOI: 10.24425/sq.2020.133751
Streszczenie: The freshwater dinoflagellate represent microfossils which are very rarely noted in lake deposits. In Late Holocene sediments of the Lake Młynek, the Iława Lakeland, northern Poland, we identified intense blooms of algae of the genus Palatinus. They occurred primarily in the period of strong human impact during expansion of the Monastic State of the Teutonic Order. The most amazing thing is that samples in which conventional palynological maceration has been used dinoflagellate are represented by armored vegetative forms instead of cysts. During this laboratory processes, especially acetolysis, cellulosic thecae of armored forms should be destructed. This is the second known example of acetolysis resistant thecae of modern dinoflagellate, built by substance other than cellulose. Palatinus blooms were associated probably with the hydrotechnical works made by Teutonic Knights in the catchment, which caused supply and discharge of micronutrients e.g. selenium in the basin.
Projekt/grant: 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) : Narodowe Centrum Nauki, UMO-2016/21/B/ST10/03059

5/11
Nr opisu: 0000038171
Autorzy: Leszek Marks, Fabian Welc, Krystyna Milecka, Abdelfattah Zalat, Chen Zhongyuan, Aleksandra Majecka, Jerzy Antoni Nitychoruk, Aala Salem, Qianli Sun, Marcin Szymanek, Izabela Gałecka, Anna Tołoczko-Pasek.
Tytuł pracy: Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, Egypt
Tytuł czasopisma:
Szczegóły: 2019, Vol. 528, p. 120--132
p-ISSN: 0031-0182

Charakterystyka formalna: artykuł w czasopiśmie zagranicznym
Charakterystyka merytoryczna: artykuł oryginalny naukowy
Charakterystyka wg MNiSW: artykuł w czasopiśmie z IF (wykaz MEiN)
Język publikacji: ENG
Wskaźnik Impact Factor ISI: 2.833
Punktacja ministerstwa: 100.000
Praca recenzowana
Słowa kluczowe ang.: holocene ; atmospheric circulation ; Intertropical Convergence Zone ; palaeowesterlies ; pollen record ; diatoms
Uwaga: Kopia dostępna w Sekcji Bibliometrii.
Inne bazy podające opis:
  • Scopus
  • WoS

    DOI: 10.1016/j.palaeo.2019.04.032
    Streszczenie: During 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.
    Projekt/grant: Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego Egiptu : Narodowe Centrum Nauki, DEC-2012/05/B/ST10/00558

    6/11
    Nr opisu: 0000036404
    Autorzy: Abdelfattah Zalat, Fabian Welc, Jerzy Antoni Nitychoruk, Leszek Marks.
    Tytuł pracy: Climate change, environmental history and Human impact during the Late Holocene inferred from diatom analysis of the Qarun Lake, Faiyoum Oasis, Egypt
    Tytuł całości: W: The 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regions : programme and book of abstracts
    Miejsce wydania: Zagreb
    Wydawca:
    Rok wydania: 2018
    Strony zajęte przez pracę: P. 8
    Charakterystyka formalna: streszczenie zjazdowe międzynarodowe (książka streszczeń)
    Charakterystyka merytoryczna: konferencja naukowa międzynarodowa
    Język publikacji: ENG
    Słowa kluczowe ang.: Qarun Lake ; Egypt ; holocene ; diatom analysis ; climate change
    Projekt/grant: Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego Egiptu : Narodowe Centrum Nauki, DEC-2012/05/B/ST10/00558

    7/11
    Nr opisu: 0000036407
    Autorzy: Leszek Marks, Fabian Welc, Abdelfattah Zalat, Jerzy Antoni Nitychoruk, Zhongyuan Chen, Alaa Salem, Aleksandra Majecka.
    Tytuł pracy: Environmental conditions in late Antiquty in the Faiyum Oasis (Egypt) based on the Lake Qarun sediments studies and geoarcheological research
    Tytuł całości: W: The 5 th Geoarchaeological Conference Late Antiquity and Migration Period in the light of geoarchaeological records from the eastern Mediterranean, eastern Adriatic and adjacent regions : programme and book of abstracts
    Miejsce wydania: Zagreb
    Wydawca:
    Rok wydania: 2018
    Strony zajęte przez pracę: P. 30
    Charakterystyka formalna: streszczenie zjazdowe międzynarodowe (książka streszczeń)
    Charakterystyka merytoryczna: konferencja naukowa międzynarodowa
    Język publikacji: ENG
    Słowa kluczowe ang.: lake sediments ; environmental conditions ; holocene ; Faiyum Oasis ; Egypt
    Uwaga: Kopia dostępna w Sekcji Bibliometrii.
    Projekt/grant: Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego Egiptu : Narodowe Centrum Nauki, DEC-2012/05/B/ST10/00558

    8/11
    Nr opisu: 0000034974
    Autorzy: Leszek Marks, Alaa Salem, Fabian Welc, Jerzy Antoni Nitychoruk, Zhongyuan Chen, Maarten Blaauw, Abdelfattah Zalat, Aleksandra Majecka, Marcin Szymanek, Marta Chodyka, Anna Tołoczko-Pasek, Qianli Sun, Xiaoshuang Zhao, Jun Jiang.
    Tytuł pracy: Holocene lake sediments from the Faiyum Oasis in Egypt: : a record of environmental and climate change
    Tytuł czasopisma:
    Szczegóły: 2018, Vol. 47, Issue 1, p. 62--79
    p-ISSN: 0300-9483
    e-ISSN: 1502-3885

    Charakterystyka formalna: artykuł w czasopiśmie zagranicznym
    Charakterystyka merytoryczna: artykuł oryginalny naukowy
    Charakterystyka wg MNiSW: artykuł w czasopiśmie z IF (wykaz MEiN)
    Język publikacji: ENG
    Wskaźnik Impact Factor ISI: 3.531
    Punktacja ministerstwa: 35.000
    Praca recenzowana
    Słowa kluczowe ang.: holocene ; lake sediments ; Faiyum Oasis ; environmental change ; climate change
    Uwaga: Kopia dostępna w Sekcji Bibliometrii
    http://onlinelibrary.wiley.com/doi/10.1111/bor.12251/abstract
    DOI: 10.1111/bor.12251
    Streszczenie: The 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.
    Projekt/grant: 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) : Narodowe Centrum Nauki, UMO-2016/21/B/ST10/03059
    Projekt/grant: Zastosowanie innowacyjnej metody komputerowej do analizy obrazu okrzemek i zmian paleośrodowiskowychw Holocenie na Pojezierzu Iławskim : Fundusz Grantów na Badania Własne / PSW Biała Podlaska, SNW-51-FG.V.4-1/17

    9/11
    Nr opisu: 0000033785
    Autorzy: Abdelfattah A. Zalat, Leszek Marks, Fabian Welc, Alaa Salem, Jerzy Antoni Nitychoruk, Zhongyuan Chen, Aleksandra Majecka, Marcin Szymanek, Marta Chodyka, Anna Tołoczko-Pasek, Qianli Sun, Xiaoshuang Zhao, Jun Jiang.
    Tytuł pracy: Diatom Stratigraphy of FA-1 Core, Qarun Lake, Records of Holocene Environmental and Climatic Change in Faiyum Oasis, Egypt
    Tytuł czasopisma:
    Szczegóły: 2017, Vol. 34, no. 1, p. 61--69
    p-ISSN: 1641-5558

    Charakterystyka formalna: artykuł w czasopiśmie polskim
    Charakterystyka merytoryczna: artykuł oryginalny naukowy
    Charakterystyka wg MNiSW: artykuł w czasopiśmie bez IF (wykaz MEiN)
    Język publikacji: ENG
    Punktacja ministerstwa: 14.000
    Słowa kluczowe: holocen ; środowisko ; zmiany klimatu ; jezioro Karun ; okrzemki ; oaza Fajum ; Egipt
    Słowa kluczowe ang.: holocene ; environment ; climate change ; Qarun Lake ; diatoms ; Faiyum Oasis ; Egypt
    Uwaga: Kopia dostepna w Sekcji Bibliometrii
    Inne bazy podające opis:
  • BazTech
  • Scopus
  • Emerging Sources Citation Index (Web of Science Core Collection)
  • DOAJ
  • Zoological Rekord
  • IC Journals Master List

    http://www.studia.quaternaria.pan.pl/pdfs/sq34-1/5_Zalat.pdf
    DOI: 10.1515/squa-017-0005
    Streszczenie: This 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.
    Projekt/grant: Opracowanie nowych algorytmów analizy obrazu z wykorzystaniem sztucznych sieci komputerowych : działalność statutowa WNET PSW, 2017-WNET/KNT/ZI/1

    10/11
    Nr opisu: 0000031845
    Autorzy: Leszek Marks, Alaa Salem, Fabian Welc, Jerzy Antoni Nitychoruk, Chen Zhongyuan, Abdelfattah Zalat, Aleksandra Majecka, Marta Chodyka, Marcin Szymanek, Anna Tołoczko-Pasek.
    Tytuł pracy: Preliminary report on unique laminated holocene sediments from the Qarun Lake in Egypt
    Tytuł czasopisma:
    Szczegóły: 2016, Vol. 33, no. 1, p. 35--46
    p-ISSN: 1641-5558
    e-ISSN: 2300-0384

    Charakterystyka formalna: artykuł w czasopiśmie polskim
    Charakterystyka merytoryczna: artykuł oryginalny naukowy
    Charakterystyka wg MNiSW: artykuł w czasopiśmie bez IF (wykaz MEiN)
    Język publikacji: ENG
    Punktacja ministerstwa: 14.000
    Praca recenzowana
    Słowa kluczowe: holocen ; osady jeziorne ; osady laminowane ; jezioro Karun ; Fajum ; Egipt
    Słowa kluczowe ang.: holocene ; laminated sediments ; Qarun Lake ; Faiyum Oasis ; Egypt
    Uwaga: Kopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki.
    http://www.studia.quaternaria.pan.pl/pdfs/sq33-1/s_035_046_opt.pdf
    DOI: 10.1515/squa-2016-0004
    Streszczenie: The 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.
    Projekt/grant: Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego Egiptu : Narodowe Centrum Nauki, DEC-2012/05/B/ST10/00558

    11/11
    Nr opisu: 0000029517
    Autorzy: Fabian Welc, Jerzy Antoni Nitychoruk, Zhongyuan Chen, Marta Chodyka, Aleksandra Majecka.
    Tytuł pracy: Holocene climate change in notheastern Africa and its impact on ancient Egyptian civilisation
    Tytuł czasopisma:
    Szczegóły: 2014, nr 21(2), s. 16
    Charakterystyka formalna: varia: list, wywiad, komentarz, biogram, wspomnienie
    Charakterystyka merytoryczna: komunikat o wynikach badań
    Język publikacji: ENG
    Liczba arkuszy: 0,1
    Słowa kluczowe: zmiany klimatyczne ; Afryka Północna ; holocen ; starożytny Egipt
    Słowa kluczowe ang.: climate change ; notheastern Africa ; ancient egyptian civilisation ; holocene
    Uwaga: Kopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki PSW
    Projekt/grant: Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego Egiptu : Narodowe Centrum Nauki, DEC-2012/05/B/ST10/00558

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