The age of the subfossil trunk horizon in deposits of the Warta river valley (central Poland) based on ¹⁴C dating

• Autorzy: Dzieduszyńska D. , Peterga-Zganiacz J. , Krąpiec M.
• Języki publikacji: EN

Abstrakty

EN

The present study focuses on investigations carried out in the Late Vistulian succession of the Warta River deposits (central Poland) in which a horizon of subfossil trees was excavated. Preliminary conclusions on time record and past environmental conditions of a forest existence determined from radiocarbon dating, pollen analyses and geological evidence appear promising with view of treering chronologies.

Słowa kluczowe

EN

subfossil forest; peat; pollen analysis; ¹⁴C dating; Allerød; Younger Dryas; Warta River valley; Central Poland

• Wydawca: De Gruyter
• Czasopismo: Geochronometria
• Rocznik: 2011
• Tom: Vol. 38, no. 4
• Strony: 334--340
• Opis fizyczny: Bibliogr. 26 poz., rys., wykr.

Twórcy

autor

Dzieduszyńska D.

autor

Peterga-Zganiacz J.

autor

Krąpiec M.

• Departament of Quaternary Studies, Institute of Earth Science, University of Łódź, Kopcińskiego 31, 90-142 Lodz, Poland,

Bibliografia

• Björck S, Walker M, Cwynar L, Johnsen S, Knudsen K-L, Lowe J, Wohlfarth B and INIIMATE 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 Science 13(4): 283-292, DOI 10.1002/(SICI)1099-1417(199807/08)13:4<283::AID-JQS386>3.0.CO;2-A.
• Bohncke S, Vandenberghe J and Huijzer AS, 1993. Periglacial envi-ronments during the Weichselian Late Glacial in the Mass valley, the Netherlands. Geologie en Mijnbouw 72: 193-210.
• Bronk Ramsey C, 1995. Radiocarbon calibration and analysis of stratigraphy: The OxCal program. Radiocarbon 37(2): 425-430.
• Forysiak J, 2005. Rozwój doliny Warty między Burzeninem i Dobrowem po zlodowaceniu warty (The development of the Warta River Valley between Burzenin and Dobrów in the Late Quaternary period). Acta Geographica Lodziensia 90: 116 pp (in Polish).
• Forysiak J, Miotk-Szpiganowicz G and Petera J, 1999. Geologic setting and palynologic examination of the Vistulian sediments at Koźmin near Turek, central Poland. Geological Quarterly 43(1): 85-98.
• Friedrich M, Kromer B, Spurk M, Hofmann J and Kaiser KF, 1999. Paleo-environment and radiocarbon calibration as derived from Lateglacial/Early Holocene tree-ring chronologies. Quaternary International 61(1): 27-39, DOI 10.1016/S1040-6182(99)00015-4.
• Friedrich M, Remmele S, Kromer B, Hofmann J, Spurk M, Kaiser KF, Orcel Ch and Küppers M, 2004. The 12,460-year Hohenheim oak and pine tree-ring chronology from Central Europe – a unique annual record for radiocarbon calibration and paleoenvironment re-constructions. Radiocarbon 46(3): 1111-1122.
• Goździk JS, 1995. Inwolucje – jeden z typów deformacyjnych (Involution as a type of deformation structures). In: Mycielska–Dowgiałło E, ed., Badania osadów czwartorzędowych. Wyd. Wydziału Geografii i Studiów Regionalnych UW: 249-256 (in Polish).
• Isarin RFB, Renssen H and Vandenberghe J, 1998. The impact of the North Atlantic ocean on the Younger Dryas climate in northwestern and central Europe. Journal of Quaternary Science 13(5): 447-453, DOI 10.1002/(SICI)1099-1417(1998090)13:5<447::AID-JQS402>3.0.CO;2-B.
• Kasse C, 1999. Can involutions be used as palaeotemperature indicators? Biuletyn Peryglacjalny 38: 95-110.
• Klatkowa H, 1996. Symptoms of the permafrost presence in Middle Poland during the last 150 000 years. Biuletyn Peryglacjalny 35: 45-86.
• Mangerud J, Andersen ST, Berglund BE, Dinner JJ, 1974. Quaternary stratigraphy of Norden, a proposal for terminology and classification. Boreas 3(3): 109-126, DOI 10.1111/j.1502-3885.1974.tb00669.x.
• Michczyńska DJ, Michczyński A, Pazdur A, 2007. Frequency distribution of radiocarbon dates as a tool for reconstructing environmental changes. Radiocarbon 49(2): 799-806.
• Michczyńska DJ, Michczyński A, Pazdur A, Starkel L, 2008. Kalendarzowe wartości granic chronostratygraficznych dla terenu Polski oszacowane na podstawie dużych zbiorów dat 14C (Calendar ages of chronozones for Polish territory evaluated on the base of big sets of 14C dates). Prace Komisji Paleogeografii Czwartorzędu PAU VI: 163-171 (in Polish).
• Nanson GC and Knighton AD, 1996. Anabranching rivers: their cause, character and classification. Earth Surface Processes and Land-forms 21(3): 217-239, DOI 10.1002/(SICI)1096-9837(199603)21:3<217::AID-ESP611>3.0.CO;2-U.
• Petera J, 2002. Vistuliańskie osady dolinne w basenie uniejowskim i ich wymowa paleogeograficzna (Vistulian valley deposits in the Uniejów Basin and their palaeogeographical significance). Acta Geographica Lodziensia 83: 164 pp (in Polish).
• Petera-Zganiacz J, 2007. Osady rzeki plenivistuliańskiej w Koźminie (Deposits of the Plenivistulian river at the Koźmin site). Acta Geo-graphica Lodziensia 93: 43-56 (in Polish).
• Petera-Zganiacz J and Dzieduszyńska D, 2007. Wymowa paleogeograficzna horyzontu kopalnych pni w osadach późnego vistulianu (Palaeogeographical significance of subfossil tree trunks in the Late Vistulian sediments). Acta Geographica Lodziensia 93: 57-66 (in Polish).
• Reimer PJ, Baillie MGL, Bard E, Bayliss A, Blackwell PG, Bronk Ramsey C, Buck CE, Burr GS, Edwards RL, Freidrich M, Grootes PM, Guilderson TP, Hajdas I, Heaton TJ, Hogg AG, Hughen KA, Kaiser KF, Kromer B, McCormac G, Manning SW, Reimer RW, Richards DA, Southon JR, Talamo S, Turney CMS, van der Plicht J and Weyhenmeyer CE, 2009. Intcal09 and Marine09 radiocarbon age calibration curves, 0–50,0000 years cal BP. Radiocarbon 51(4): 1111-1150.
• Renssen H, Isarin RFB, Jacob D, Podzun R and Vandenberghe J, 2001. Simulation of the Younger Dryas climate in Europe using a regional climate model nested in an AGCM: preliminary results. Global and Planetary Change 30(1-2): 41-57, DOI 10.1016/S0921-8181(01)00076-5.
• Spurk M, Kromer B and Peschke P, 1999. Dendrochronologische, palynologische und Radiokarbon-Untersuchungen eines Waldes aus der Jüngeren Tundrezeit (Dendrochronological, palynological and radiocarbon investigations of the Younger Dryas forest). Quartär 49/50: 34-38 (in German).
• Swanson D, Ping ChL and Michaelson GJ, 1999. Diapirism in soils due to thaw of ice – rich material near the permafrost table. Permafrost and Periglacial Processes 10(4): 349-367, DOI 10.1002/(SICI)1099 1530(199910/12)10:4<349::AID-PPP318>3.0.CO;2-N.
• Turkowska K, Petera J, Forysiak J and Miotk-Szpiganowicz G, 2000. Morfogeneza powierzchni Kotliny Kolskiej w okolicach Koźmina (Morphogenesis of the Koło Basin near Koźmin). Acta Geographica Lodziensia 78: 89-134 (in Polish).
• Turkowska K, Forysiak J, Petera J, Miotk-Szpiganowicz G, 2004. A Warta River system during the Younger Dryas in the Koło Basin (Middle Poland). Questiones Geographicae 23: 83-107.
• Vandenberghe J, 1988. Cryoturbations. In: Clark MJ, ed., Advances in Periglacial Geomorphology. Wiley, Chichester: 179-198.
• OxCal, https://c14.arch.ox.ac.uk/oxcal.