Logowanie
Zarejestruj się
Zresetuj hasło
Publikuj i Dystrybuuj
Rozwiązania Wydawnicze
Rozwiązania Dystrybucyjne
Dziedziny
Architektura i projektowanie
Bibliotekoznawstwo i bibliologia
Biznes i ekonomia
Chemia
Chemia przemysłowa
Filozofia
Fizyka
Historia
Informatyka
Inżynieria
Inżynieria materiałowa
Językoznawstwo i semiotyka
Kulturoznawstwo
Literatura
Matematyka
Medycyna
Muzyka
Nauki farmaceutyczne
Nauki klasyczne i starożytne studia bliskowschodnie
Nauki o Ziemi
Nauki o organizmach żywych
Nauki społeczne
Prawo
Sport i rekreacja
Studia judaistyczne
Sztuka
Teologia i religia
Zagadnienia ogólne
Publikacje
Czasopisma
Książki
Materiały konferencyjne
Wydawcy
Blog
Kontakt
Wyszukiwanie
EUR
USD
GBP
Polski
English
Deutsch
Polski
Español
Français
Italiano
Koszyk
Home
Czasopisma
Geochronometria
Tom 44 (2017): Zeszyt 1 (January 2017)
Otwarty dostęp
Reflection of climatic changes during interpleniglacial in the geoecosystems of South-Eastern Poland
Leszek Starkel
Leszek Starkel
,
Danuta J. Michczyńska
Danuta J. Michczyńska
oraz
Piotr Gębica
Piotr Gębica
| 06 paź 2017
Geochronometria
Tom 44 (2017): Zeszyt 1 (January 2017)
O artykule
Poprzedni artykuł
Następny artykuł
Abstrakt
Artykuł
Ilustracje i tabele
Referencje
Autorzy
Artykuły w tym zeszycie
Podgląd
PDF
Zacytuj
Udostępnij
Data publikacji:
06 paź 2017
Zakres stron:
202 - 215
Otrzymano:
01 lip 2016
Przyjęty:
02 mar 2017
DOI:
https://doi.org/10.1515/geochr-2015-0060
Słowa kluczowe
Interpleniglacial
,
frequent climate fluctuations
,
permafrost
,
South-Eastern Poland
© 2016 L. Starkel.
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.
Fig. 1
δ18O of NGRIP profile from Greenland with numbered Greenland Interstadials (after Rasmussen et al., 2014). The stratigraphy of the last Pleistocene glacial stage in Poland is also marked (after Marks et al., 2015), Marine Isotope Stages (MIS) (after Lisiecki and Raymo, 2005) and average timing of interstadials refered to as Hengelo and Denekamp (different authors).
Fig. 2
A — map of Europe with Poland and the investigated area marked (rectangle). B — Palaogeography of the Carpathians and its foreland during the Pleniglacial (after Starkel, 1988): 1 – glaciated area, 2 – arctic desert, 3 – debris covers and active cryoplanation, 4 – tundra-steppe vegetation, 5 – intensive solifluction (areas with higher precipitations), 6 – areas of loess deposition, 7 – directions of intensive deflation, 8 – areas of probable preservation of some tree species, 9 – sites discussed in the present paper: Carpathians: Do – Dobra, Hu – Humniska, Ja – Jamne, Je – Jedlicze, Kr – Krościenko, Ma – Maniowy, So – Sowliny, Uh – Uherce, Wa – Wadowice; Oswiecim Basin: Ka – Kaniów, Pi – Pierściec, Śc – Ściejowice; Vistula and Lower Dunajec valleys: BN – Brzesko Nowe, NH – Nowa Huta, Op – Opatowiec, Sz – Szujec, Wł – Włoszyn; Wisłoka valley: Br – Brzeźnica, Po – Podgrodzie, Wo – Wojsław; Wisłok and San Valleys: GŁ – Główczyna Łańcucka, GN – Grodzisko Nowe, Łą – Łążek, Łu – Łukawiec, WO – Wólka Ogryzkowa, WP – Wólka Pełkińska; Lublin Upland and Roztocze: La – Latyczów.
Fig. 3
Fluvial and slope deposits from the last cold stage at Wadowice: 1. bedrock, 2. loess, 3. deluvial loams, 4. soliflucion loams (clayly) with debris, 5. as above – sandy, 6. talus debris, 7. peat from Br⊘rup (series d), 8. fluvial sands, 9. fluvial gravels, 10. rocky landslide from Interpleniglacial (series h), (after Starkel [In:] Sobolewska et al., 1964).
Fig. 4
Interpleniglacial slope deposits at Dobra (Klimaszewski, 1971; Środoń, 1968) and Krościenko (Klimaszewski et al., 1939) in Polish flysch Carpathians: 1. fluvial gravels, 2. solifluction with debris, 3. solifluction dominant clay, 4. coarse debris, 5. silt and clay, 6. organic remains, 7. rare organic remains, 8. sediment members, 9. main sediments units, 10. bedrock.
Fig. 5
Selected dates from Carpathians. Calibrated 14C dates from selected localities in Poland are marked by horizontal bars representing intervals of 68.2% confidence.
Fig. 6
A geomorphological map ot the Fore-Carpathian Basins (after Gębica et al., 2015, partly modified). 1 – margin of the Carpathians, 2 – Carpathian foothills, 3 – Uplands, 4 – Fore-Carpathian plateaus, 5 – main escarpments, 6 – Vistulian terraces and alluvial fans, 7 – Holocene valley floors (floodplains), 8 – loess cover on the terraces and plateaus, 9 – fields of drift-sand and dunes (inactive), 10 – geological cross sections, A – Wisfoka valley, B – Oświęcim Basin, C – Vistula and Lower Dunajec valleys, D – Wisfok and San valleys.
Fig. 7
Synthetic cross-section of valley floors of Carpathian river at their outlet from the Carpathians. a – channel facies of alluvia, older than Interpleniglacial, b – channel facies of alluvia-younger (from Interpleniglacial – to Holocene), c – overbank and palaeochannel fill facies, d – slope colluvia 1 – peat, 2 – loess, 3 – sand dunes.
Fig. 8
Selected dates from Subcarpathian Basins. Calibrated 14C dates from selected localities in Poland are marked by horizontal bars representing intervals of 68.2% confidence.
Fig. 9
A. Longitudinal profile of Wisioka river valley (after Gębica et al., 2015): 1 – Middle Pleniglacial terrace (level I), 2 – Upper Pleniglacial terrace (II), 3 – Late Vistulian terrace (III), 4 – Holocene terrace (IV), 5 – river channel, 6 – rock surface (strath), 7 – dunes. B. Model of alluvial fan incision marked by the cutting of Interpleniglacial cover in the close fore-mountain area. The younger (Upper Pleniglacial) fan was inserted in the northern part ot Sandomierz Basin (after Gębica et al 2015).
Fig. 10
Alluvia in Wieprz valley at Latyczów (after Harasimiuk, 1991). 1 – sand with gravel, 2 – sand, 3 – silty sand, 4 – mud, 5 – loess, 6 – fossil soil, 7 – ice wedges, 8 – involutions, 9 – small deformations, s – recent (Holocene) soil, f – floodplain deposits, l – natural levees deposits, ss – soil sediments.
Fig. 11
Type and intensity of processes during the Vistulian in C-E Europe in relation to the δ18O curve from Greenland (schematic reconstruction): A. Intensity of denudation on mountain slopes, B. Tendency to aggradation and to erosion in mountain valleys, C. Tendency to agradation and erosion in submontaneous basins, D. δ8O curve from Greenland. Main stratigraphic units 1–5, w – phases of intensive aeolian activity.
Podgląd