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Reflection of climatic changes during interpleniglacial in the geoecosystems of South-Eastern Poland

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Warianty tytułu
Konferencja
Conference Proceedings of the 12th International Conference “Methods of Absolute Chronology” May 11-13th, 2016, Gliwice-Paniówki, Poland.
Języki publikacji
EN
Abstrakty
EN
About 70% of the last cold stage was taken by transitional phases of continuous fluctuations of climate and permafrost extension. All this is reflected especially well in slope types and the thickness of slope, fluvial and aeolian deposits. Very distinct and relatively fast changes took place around 33–30 ka BP: the aridification of climate with an ice sheet transgression, expansion of continuous permafrost and the onset of loess deposition. The greatest transformations of slopes and river valleys in the Carpathians and Subcarpathian Basins took place not in the coolest phases but during the Interpleniglacial. The authors exemplified a number of sites in Southern Poland documenting frequent fluctuations of climate and permafrost from that 25–30 ka long period. Calibrated dates of dated episodes correlate well with the δ18O curve from Greenland with frequent warmings. These rapid warmings are reflected in the higher rate of aggradation in valley floors and thick colluvial material deposited over slopes, both combined with a retreat of permafrost. The comparison with the Greenland 18O curve is valuable to establish a comparable chronology of events, even for such a distant area like Central-Eastern Europe.
Wydawca
Czasopismo
Rocznik
Strony
202--215
Opis fizyczny
Bibliogr. 75 poz., rys.
Twórcy
autor
  • Institute of Geography and Spatial Organization, Polish Academy of Sciences, Św. Jana 22, 31-018 Krakow, Poland
  • GADAM Centre of Excellence, Institute of Physics – CSE, Silesian University of Technology, Konarskiego 22B, 44-100 Gliwice
autor
  • University of Information Technology and Management in Rzeszów, Department of Geography, Sucharskiego 2, 35-225 Rzeszów, Poland
Bibliografia
  • 1. Alexandrowicz SW and Jersak J, 1991. Profil lessów w Opatowcu nad Wisłą (Loess profile in Opatowiec on the Vistula River). In: Maruszczak H, Ed., Podstawowe profile lessów w Polsce (Basic loess profiles in Poland). Uniwersytet Marii Curie-Skłodowskiej, Lublin: 91–93.
  • 2. Baulin V, Belopukhova YB and Danilova NS, 1984. Holocene permafrost in the USRR. [In:] Velichko A.A. (ed.), Late Quaternary Environments of the Soviet Union, Univ. of Minnesota Press: 87–94.
  • 3. Birks HH, Gelorini V, Robinson E and Hoek WZ, 2015. Impacts of palaeoclimate change 60 000–8000 years ago on humans and their environments in Europe: Integrating palaeoenvironmental and archaeological data. Quaternary International378: 4–13.
  • 4. Björck S, Walker MJC, Cwynar L, Johnsen SJ, Knudsen K-L, Lowe JJ, Wohlfarth B and INTIMATE Members, 1998. An event stratigraphy for the last termination in the North Atlantic region based on the Greenland Ice Core record: a proposal by the INTIMATE group. Journal of Quaternary Science13: 283–292.
  • 5. Blockley SPE, Lane CS, Hardiman M, Rasmussen SO, Seierstad IK, Steffensen JP, Svensson A, Lotter AF, Turney CSM and Bronk Ramsey C, 2012. Synchronisation of palaeoenvironmental records over the last 60,000 years, and an extended INTIMATE event stratigraphy to 48,000 b2k. Quaternary Science Reviews36: 2–10.
  • 6. Blockley S, Brauer A, Davies S, Hardiman M, Harding P, Lane C, MacLeod A, Matthews I, Pyne-O’Donnell S, Rasmussen SO, Wulf S and Zanchetta G, 2014. Tephrochronology and the extended INTIMATE (INTegration of Ice-core, Marine and TErrestrial records) event stratigraphy 8-128 ka b2k. Quaternary Science Reviews106: 88–100.
  • 7. Bottema S, 1979. Pollen analytical investigations in Thessaly (Greece). Palaeohistoria21: 19–40.
  • 8. Bronk Ramsey C, 2009. Bayesian analysis of radiocarbon dates. Radiocarbon51(1): 337–360.
  • 9. Buraczyński J, 1996. Ewolucja doliny górnego Wieprza na Roztoczu w piętrach Wisly i holocenu. (Evolution of the upper Wieprz River valley in the Roztocze Upland during Vistulian and the Holocene). Annales UMCS Lublin, sec. B 51(8): 117–139.
  • 10. Buraczyński J, 1998. Development of eolian processes during the pleni-and Vistulian the southeastern Poland. Biuletyn Peryglacjalny37: 7–18.
  • 11. Davies SM, Abbott PM, Pearce NJG, Wastegård S and Blockley SPE, 2012. Integrating the INTIMATE records using tephrochronology: rising to the challenge. Quaternary Science Reviews36: 11–27.
  • 12. Dziewański J and Starkel L, 1967. Slope covers on the middle terrace at Zabrodzie upon the San. Geomorphologica Carpatho-Balcanica1: 21–35.
  • 13. Feurdean A, Perşoiu A, Tantau I, Stevens T, Magyari EK, Onac BP, Markovic S, Andric M, Connor S, Farcas S, Gałka M, Gaudeny T, Hoek W, Kolaczek P, Kunes P, Lamentowicz M, Marinova E, Michczyńska DJ, Perşoiu I, Płóciennik M, Słowiński M, Stancikaite M, Sumegi P, Svensson A, Tamas T, Timar A, Tonkov S, Toth M, Veski S, Willis KJ and Zernitskaya V, 2014. Climate variability and associated vegetation response throughout Central and Eastern Europe (CEE) between 60 and 8 ka. Quaternary Science Reviews106: 206–224.
  • 14. Gerlach T, 1990. Ewolucja młodo czwartorzędowych zbiorników jeziornych centralnej części Dołów Jasielsko-Sanockich. (Evolution of the upper Quaternary lake basins in the central part of Jaslo-Sanok Depression). Studia Geomorphologica Carpatho-Balcanica24: 119–160.
  • 15. Gerlach T, Koszarski L, Koperowa W and Koster EA, 1972. Sédiments lacustres postglaciaires dans la dépression de Jaslo - Sanok. (Sediments of postglacial lakes in the Jaslo - Sanok depression). Studia Geomorphologica Carpatho-Balcanica6: 37–62.
  • 16. Gerlach T, Krysowska-Iwaszkiewicz M, Szczepanek K and Pazdur M, 1993. Nowe dane o pokrywie karpackiej odmiany lessów w Humniskach koło Brzozowa. (New data about cover of the Carpathian variety of loess in Humniska near Brzozów). Zeszyty IGiPZ PAN16: 43pp.
  • 17. Gębica P, 1995. Evolution of the Vistula Valley and alluvial fans of the Raba and Uszwica rivers between Uscie Solne and Szczurowa in the Vistulian and Holocene. Geographical Studies IGiPZ PAN, Special Issue8: 31–50.
  • 18. Gębica P, 2004. Przebieg akumulacji rzecznej w górnym vistulianie w Kotlinie Sandomierskiej (The Course of Fluvial Accumulation During the Upper Vistulian in Sandomierz Basin). Prace Geograficzne IGiPZ PAN193: 229 pp (in Polish).
  • 19. Gębica P, Szczepanek K, Pazdur A and Sańko AF, 1998. Vistulian terrace with loess cover in the Vistula river valley near Brzesko (Southern Poland). Biuletyn Peryglacjalny37: 81–93.
  • 20. Gębica P, Starkel L and Michczyńska DJ, 2015. Fluvial history of Sub-Carpathian Basins (Poland) during the last cold stage (60–8 cal ka BP). Quaternary International388: 119–141.
  • 21. Gilot E, Niedziałkowska E, Sobolewska M and Starkel L, 1982. Pleniglacial alluvial fan of the Biała stream at Kaniow near Czechowice (The Oświęcim Basin). Studia Geomorphologica Carpatho-Balcanica15: 115–124.
  • 22. Grichuk VP, 1973. Vegetation. The palaeogeography of Europe during Late Pleistocene, Moscow: 182–219 (in Russian).
  • 23. Harasimiuk M, 1991. Vistulian Glacial Cycle of the fluvial processes development in the valley of the middle Wieprz river (SE Poland). Annales, UMCS Lublin, sec. B, 46(5) 81–109.
  • 24. Jersak J, Sendobry K and Śnieszko Z, 1992. Postwarciańska ewolucja wyżyn lessowych w Polsce (Evolution of less plateau in Poland during the post-Warta period). Prace Naukowe Uniwersytetu Śląskiego1227, Katowice: 195 pp (in Polish).
  • 25. Kiss T, Hernesz P, Sümeghy B, Györgyövics K and Sipos G, 2015. The evolution of the Great Hungarian Plain fluvial system – Fluvial processes in a subsiding area from the beginning of the Weichselian. Quaternary International388: 142–155.
  • 26. Klimaszewski M, 1971. The effect of solifluction processes on the development of mountain slopes in the Beskidy (Flysch Carpathians). Folia Quaternaria38: 3–18.
  • 27. Klimaszewski M, Szafer W, Szafran B and Urbański J, 1939. Flora dryasowa w Krościenku nad Dunajcem. (Dryas flora from Krościenko on the Dunajec River). Biuletyn Państwowego Instytutu Geologicznego24.
  • 28. Klimek K and Starkel L (eds.), 1980. Vertical zonality in the Southern Khangai Mountains (Mongolia). Prace Geograficzne IGiPZ PAN136: 1–107.
  • 29. Kowalkowski A and Starkel L, 1984. Altitudinal belts of geomorphic processes in the Southern Khangai Mts.(Mongolia).Studia Geomorphologica Carpatho-Balcanica18: 95–115.
  • 30. Krysowska-Iwaszkiewicz M and Wójcik A, 1990. Wyniki badań późnoplejstoceńskich stokowych pokryw gliniastych w Jedliczach (Doły Jasielsko-Sanockie). (Results of research of the Late Pleistocene loamy slope cover at Jedlicze, Jasło-Sanok Depression). Studia Geomorphologica Carpatho-Balcanica24: 63–85.
  • 31. Lisiecki LE and Raymo ME, 2005. A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records.Paleoceanography20: PA1003.
  • 32. Lowe JJ, Hoek W and INTIMATE Group, 2001. Inter-regional correlation of palaeoclimatic records for the Last Glacial-Interglacial Transition: a protocol for improved precision recommended by the INTIMATE project group. Quaternary Science Reviews20: 1175–1187.
  • 33. Lowe JJ, Rasmussen SO, Bjorck S, Hoek WZ, Steffensen JP, Walker MJC and Yu ZC, 2008. Synchronisation of palaeoenvironmental events in the North Atlantic region during the Last Termination: a revised protocol recommended by the INTIMATE group. Quaternary Science Reviews27: 6–17.
  • 34. Łanczont M, 1995. Warunki paleogeograficzne akumulacji oraz stratygraficzne zróżnicowanie utworów lessowych we wschodniej części Pogórza Karpackiego. (Paleogeographical conditions of accumulation and stratigraphical differentiation of loess deposits in the eastern part of Carpathian Foothills). Wydział Nauki i Nauk o Ziemi UMCS. Rozprawy habilitacyjne: 50pp.
  • 35. Łanczont M and Wojtanowicz J, 2012. Znaczenie badań lessu w paleogeografii. (Importance of the loess research in paleogeography). [In:] M. Łanczont M and Wojtanowicz J, Eds., Z zastosowań geografii. Wyd. UMCS Lublin: 111pp.
  • 36. Mamakowa K, 1968. Flora z interstadiału Paudorf w Łążku koło Zaklikowa. (Flora of the Paudorf Interstadial at Łążek near Zaklików). Acta Paleobotanica9(1): 29–44.
  • 37. Mamakowa K and Gębica P, 2015. Pollen Analysis of a peaty mud Simple from the Dunajec River alluvial fan (Sandomierz Basin, Poland in the context of its morphological position, radiocarbon dating and comparison with nighbouring sites.Acta Palaeobotanica55(1): 93–96.
  • 38. Mamakowa K and Starkel L, 1974. New data about the profile of Young-Quaternary deposits at Brźeznica in Wisłoka valley, Sandomierz Basin. Studia Geomorphologica Carpatho-Balcanica8: 47–59.
  • 39. Mamakowa K and Środoń A, 1977. O pleniglacjalnej florze z Nowej Huty i osadach czwartorzędu doliny Wisły pod Krakowem. Roczniki Polskiego Tow. Geol47(4): 485–511.
  • 40. Mamakowa K, Starkel L, Boratyn J and Brud S, 1997. Stratigraphy of the Vistulian alluvial fills in the Wisłoka valley north of Dębica. Studia Geoomorphologica Carpatho-Balcanica31: 83–99.
  • 41. Marks L, Gałżzka D and Woronko B, 2015. Climate, environment and stratigraphy of the last Pleistocene glacial stage in Poland. Quaternary International.
  • 42. Maruszczak H, 1980. Stratigraphy and chronology of the Vistulian loesses in Poland. Quaternary Studies in Poland2: 57–76.
  • 43. Niedziałkowska E and Szczepanek K, 1993–1994. Utwory pyłowe vistuliańskiego stożka Wisły w Kotlinie Oświęcimskiej (Dust sediments of the Vistula river Vistulian fan in Oświęcim Basin). Studia Geomorphologica Carpatho-Balcanica27–28: 29–44 (in Polish).
  • 44. Pazdur A, Bluszcz A and Gębica P, 2006. Wyniki datowań OSL i 14C osadów vistulianu w profilach Łukawiec i Dżbrówki (dolina Wisłoka) (Results of OSL and 14C datings of the vistulian sediments in Łukawiec and Dżbrówka profiles (Wisłok valley)). Prace Komisji Paleogeografii Czwartorzędu Polskiej Akademii UmiejętnościIV: 27–29 (in Polish).
  • 45. Rasmussen SO, Bigler M, Blockley SPE, Blunier T, Buchardt SL, Clausen HB, Cvijanovic I, Dahl-Jensen D, Johnsen SJ, Fischer H, Gkinis V, Guillevic M, Hoek WZ, Lowe JJ, Pedro J, Popp T, Seierstad IK, Steffensen JP, Svensson AM, Vallelonga P, Vinther BM, Walker MJC, Wheatley JJ and Winstrup M, 2014. A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records: refining and extending the INTIMATE event stratigraphy. Quaternary Science Reviews106: 14–27.
  • 46. Reimer PJ, Bard E, Bayliss A, Beck JW, Blackwell PG, Bronk Ramsey C, Grootes PM, Guilderson TP, Haflidason H, Hajdas I, Hatt C, Heaton TJ, Hoffmann DL, Hogg AG, Hughen KA, Kaiser KF, Kromer B, Manning SW, Niu M, Reimer RW, Richards DA, Scott EM, Southon JR, Staff RA, Turney CSM, van der Plicht J, 2013. IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP. Radiocarbon55(4): 1869–1887.
  • 47. Rutkowski J, 1993. Objaśnienia do Szczegółowej Mapy Geologicznej Polski 1:50 000, arkusz Kraków (Explanation of the Detailed Geological Map of Polish 1:50 000 sheet Krakow). Państwowy Instytut Geologiczny, Warszawa: 1–46 (in Polish).
  • 48. Sobolewska M, Starkel L and Środoń A, 1964. Late-Pleistocene deposits with fossil flora at Wadowice (West Carpathians).Folia Quaternaria7: 1–16 (in Polish).
  • 49. Sokołowski T, 1995. Development of the lower reach of the Dunajec river in the Vistulian and Holocene. [In:] Starkel L., (Ed.), Evolution of the Vistula River Valley. Geographical Studies, Special Issue 8: 51–71.
  • 50. Sokołowski T and Wasylikowa K, 1984. Utwory czwartorzędowe den dolin Wisły i Wilgi w rejonie Ludwinowa. (Quaternary deposits of the valley floors of the Vistula and Wilga Rivers in the vicinity of Ludwinów) [In:] Materiały sympozjum: Holocen okolic Krakowa, wrzesień 1984, Wyd. AGH, Kraków: 29–34.
  • 51. Starkel L, 1960. Periglacial covers in the Beskid Wyspowy (Carpathians). Biuletyn Peryglacjalny8.
  • 52. Starkel L, 1965. Rozwój rzeźby polskiej części Karpat Wschodnich. (The relief evolution of Polish part of Eastern Carpathians). Prace Instytutu Geografii PAN50.
  • 53. Starkel L, 1977. The paleogeography of Middle and East Europe during the Last cold Stage and West-European comparison. Philosophical Transactions of the Royal SocietyB280.
  • 54. Starkel L, 1988. Palaeogeography of the periglacial zone in Poland during the maximum advance of the Vistulian ice sheet. Geographia Polonica55: 151–163.
  • 55. Starkel L, 1995a. New data on the late Vistulian and Holocene evolution of the Wisłoka valley near Debica. Geographical Studies IGiPZ PAN, Special Issue8: 73–90.
  • 56. Starkel L, 1995b. Evolution of the Carpathian valleys and the Forecarpathian basins in the Vistulian and Holocene. Studia Geomorphologica Carpatho-Balcanica29: 5–40.
  • 57. Starkel L, 1995c. Palaeohydrology of the temperate zone. [In:] Gregory KJ, Starkel L and Baker VR, Eds., Global Continental Palaeohydrology J. Wiley & Sons: 233–257.
  • 58. Starkel L, (ed.), 1981. The evolution of the Wisloka valley near Dębica during the Late Glacial and Holocene. Folia Quaternaria53 91 pp.
  • 59. Starkel L and Kowalkowski A, (eds.), 1980. Environment of the Sant Valley (Southern Khangai Mountains). Prace Geograficzne IGiPZ PAN137: 1–87.
  • 60. Starkel L, Gębica P, Kalicki T, Ludwikowska M, Niedzialkowska E, 1999. Chronostratygrafia aluwiów i form fluwialnych w południowej Polsce. [In:] Pazdur A., Bluszcz A., Stankowski W and Starkel L, Eds., Geochronologia górnego czwartorzędu Polski w świetle datowania radiowęglowego i luminescencyjnego. Wind J. Wojewoda, Wroclaw: 133–155.
  • 61. Starkel L, Soja R and Michczyńska DJ, 2006. Past hydrological events reflected in Holocene history of Polish Rivers.Catena66: 24–33.
  • 62. Starkel L, Gębica P and Superson J, 2007. Last Glacial-Interglacial cycle in the evolution of river valleys in southern and central Poland. Quaternary Science Reviews26: 2924–2936.
  • 63. Starkel L, Michczyńska DJ, Gębica P, Kiss T, Panin A and Persoiu I, 2015. Climatic fluctuations reflected in the evolution of fluvial systems of Central-Eastern Europe (60–8 ka cal BP). Quaternary International388: 97–118.
  • 64. Superson J, 1996. Funkcjonowanie systemu fluwialnego wyżynnej części dorzecza Wieprza w zlodowaceniu Wisły. (The activity of fluvial system in the upland part of the Wieprz river catchment during Vistulian). Wydział Biologii i Nauk o Ziemi UMCS, Rozprawy habilitacyjne53: 280pp.
  • 65. Superson J and Zagórski P, 2003. The development of periglacial sedimentation in the Wolica valley (SE Poland) during the Weichselian upper pleniglacial. Landform Annalysis4: 17–37.
  • 66. Superson J, Gębica P and Brzezińska-Wójcik T, 2010. The origin of deformation structures in periglacial fluvial sediments of the Wisłok valley, southeast Poland. Permafrost and Periglacial Processes21: 301–314.
  • 67. Szumański A, 1986. Postglacjalna ewolucja i mechanizm transformacji dna doliny Dolnego Sanu (Post-glacial evolution and transformation mechanism of valley floor of the Lower San River). Zeszyty Naukowe AGH, Geologia12(1): 5–92 (in Polish).
  • 68. Środoń A, 1968. O roślinności interstadialu Paudorf w Karpatach Zachodnich. (About vegetation of the Paudorf Interstadial in the Western Carpathians). Acta Palaebotanica9: 1–27.
  • 69. Vandenberghe J, 1992. Periglacial Phenomena and Pleistocene Environmental Conditions in the Netherlands - An Overview. Permafrost and Periglacial Processes3: 363–374.
  • 70. Vandenberghe J, French HM, Gorbunov A, Marchenko S, Velichko AA, Jin H, Cui Z, Zhang T and Wan X, 2014. The last Permafrost Maximum (LPM) map of the Northern Hemisphere: permafrost extent and mean annual air temperatures, 25–17 ka BP. Boreas43: 652–666.
  • 71. Wojtanowicz J, 1996. An age of the inicial phase of the Lateglacial intercontinental dunes and problems of the Plenivistulian dunes in S-E Poland in the light of TL datings. [In:] Szczypek T., Ed., Współczesne oraz kopalne zjawiska I formy eoliczne. Uniw. Śląski, Sosnowiec: 157–169.
  • 72. Wojtanowicz J, 1999. Problem of occurrence and age (TL) of inland Plenivistulian dunes in Poland (on the example of Sandomierz Basin). In: Schirmer W, Ed., Dunes and fossil soils. GeoArchae-oRhein3: 43–53.
  • 73. Wójcik A, Malata T and Szczepanek K, 1999. Stanowisko Grodzisko Nowe. Problem wieku plejstoceńskich teras piaszczystych w dolinie Sanu przy ujsciu Wisłoka. (Grodzisko Nowe site. The problem of age of the Pleistocene sandy terraces in San valley near inlet of Wislok river). [In:] VI Konferencja stratygrafii plejstocenu Polski “Czwartorzęd wschodniej części Kotliny Sandomierskiej”, Czudec, 31VIII-4IX 1999, PIG, Kraków: 115–117.
  • 74. Zagwijn WH, 1974. The Pliocene-Pleistocene boundary in western and southern Europe. Boreas3: 75–97.
  • 75. Zieliński P, Sokołowski RJ, Fedorowicz S and Zaleski I, 2014. Periglacial structures within fluvio-aeolian successions of the end of the Last Glaciation – examples from SE Poland and NW Ukraine. Boreas43: 712–721.
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-4f2feefd-f0e5-44d5-ac30-51c5a90836b6
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