Temat: interglacials - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Uwagi o plejstoceńskich glacjałach i interglacjałach
Problem of Pleistocene interglacials and glaciations — general remarks.
Autorzy:: Winter, H.
Powiązania:: https://bibliotekanauki.pl/articles/2074473.pdf
Data publikacji:: 2006
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: plejstocen
klimatostratygrafia
palinostratygrafia
interglacjał
lodowacenie
Pleistocene
climatostratigraphy
palinostratigraphy
interglacials
glaciations
Opis:: The paper discusses issues of the distinguishing mono-interglacials (Eemian, Mazovian and Zbojnian ones) and bi-interglacials (Ferdynandovian and Augustovian ones) pollen successions as well as a problem of cooling/glaciation within Ferdynandovian and Augustovian pollen successions. Division of the Ferdynandovian and Augustovian pollen successions into two separated interglacials each (FI and FII, AI and A II, respectivaly) and the glaciation sensu lato (F I/II and A I/II) between these interglacials from the climatostratigraphical point of view is proposed.
Źródło:: Przegląd Geologiczny; 2006, 54, 2; 142-144
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Main climatic changes in the Quaternary of Poland, Belarus and Ukraine
Autorzy:: Lindner, L.
Gozhik, P.
Marciniak, B.
Mars, L.
Yelovicheva, Y.
Powiązania:: https://bibliotekanauki.pl/articles/2058786.pdf
Data publikacji:: 2004
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: Polska
Belarus
Ukraine
Quaternary
glaciations and coolings
interglacials and warmings
loess
palaeosols
Opis:: 26 units are described and correlated, representing the main climatic episodes during the Quaternary in Poland, Belarus and Ukraine. They comprise 13 cool and 13 warm intervals. The four oldest ones are Różcian (Olkhovskian, Siver), Ponurzycian (Grushevskian, Beregovo), Otwockian (Vselubskian, Berezan) and Celestynovian (Yelenynskian, Kryzhaniv); these correspond to Praetiglian, Tiglian, Eburonian and Menapian, respectively of the Early Pleistocene in the Netherlands. In Poland this part of the Quaternary is named the Pre-Glacial or the Pre-Pleistocene. The Mid and Late Quaternary (the glacial epoch in Europe) comprises 11 glaciations or global coolings, namely the Narevian in Poland (Zhlobynskian, Ilyichivsk), the younger pre-Augustovian (Rogachevian 1/2, Shirokino 1/2), Augustovian 1/2 (Rogachevian 2/3, Shirokino 2/3), Nidanian (Narevian in Belarus, Pryazovsk), Sanian 1 (Servetskian, Sula), Ferdynandovian 1/2 (Belovezhian 1/2, Lubny 1/2), Sanian 2 (Berezinian, Tiligul), Liviecian (Orel), Krznanian (Dnieper 1), Odranian+Wartanian (Dnieperian+Sozhian, Dnieper 2 = Tyasmyn), Vistulian (Poozerian, Valday); and 10 interglacials or global warmings: early pre-Augustovian (Rogachevian 1, Shirokino 1), Augustovian 1 (Rogachevian 2, Shirokino 2), Augustovian 2 (Rogachevian 3, Shirokino 3) ,Małopolanian (Korchevian,Martonosha), Ferdynandovian 1 (Belovezhian 1, Lubny 1), Ferdynandovian 2 (Belovezhian 2, Lubny 2), Mazovian (Alexandrian, Zavadivka), Zbójnian (Smolenskian, Potagaylivka), Lubavian (Shklovian, Kaydaky), Eemian (Muravian, Pryluky) and Holocene. All these units are correlated with oxygen isotope stages identified in deep-sea sediments, shown relative to the palaeomagnetic epochs and correlated with main cool and warm stratigraphic units of Western Europe. Particular attention was placed on correlation of glacial and lake deposits, loesses and palaeosols.
Źródło:: Geological Quarterly; 2004, 48, 2; 97--114
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: O podziale klimatostratygraficznym kompleksu środkowopolskiego w plejstocenie Polski
Climatostratigraphic subdivision of the Pleistocene Middle Polish Complex in Poland
Autorzy:: Lindner, L.
Marks, L.
Powiązania:: https://bibliotekanauki.pl/articles/2074906.pdf
Data publikacji:: 2012
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: pleistocen
kompleksu środkowopolski
zlodowacenia
interglacjał
Polska
Pleistocene
Middle Polish Complex
glaciations
interglacials
Polska
Opis:: The term Middle Polish Complex was introduced by the authors in 2007 as an informal superstage of the younger Middle Pleistocene in Poland. It replaced a previous inconsistent term of Middle Polish Glaciations, composed both of glaciations and interglacials. The Middle Polish Complex comprises deposits of 3 glaciations (Liwiecian, Krznanian and Odranian) and 3 interglacials (Mazovian, Zbójnian and Lublinian). Glacial and lake-marshy deposits of the complex correspond with loess sequences and separating palaeosols. Their common superposition in Poland and recorded palaeomagnetic episodes Emperor, Chegan, Jamaica and Blake of the Brunhes epoch verify a chronology of climatic changes and climatostratigraphic subdivision of the complex. Mutual relation of climate changes and their reference to glacial-interglacial and loessy-palaeosol cycles in neighbouring countries support usefulness to more specified correlations. Successive interglacials and glaciations of the Middle Polish Complex correspond to rhythmic global climate changes reflected by oxygen isotope stages in deep-sea boreholes (MIS11-6)
Źródło:: Przegląd Geologiczny; 2012, 60, 1; 36-45
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:: Czynniki zmian klimatycznych w środkowym i górnym plejstocenie : ich zapis geologiczny w osadach Oceanu Południowego oraz rdzeniach lodowych
Climate change indicators in middle and late Pleistocene as reflected in sediments of Southern Ocean and ice core records
Autorzy:: Kotrys, B.
Powiązania:: https://bibliotekanauki.pl/articles/2075570.pdf
Data publikacji:: 2016
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: plejstocen
Ocean Południowy
morskie stadium izotopowe
temperatura powierzchni morza
glacjał
interglacjał
Pleistocene
Southern Ocean
Marine Isotope Stage
sea surface temperature
glacials
interglacials
Opis:: Climate changes during the Pleistocene were driven by large-scale orbital perturbations as well as by internal feedbacks on the Earth. One of the main roles in climate modelling is played by the Southern Ocean that is a great source of sea ice, carbon dioxide, dissolved silica and nutrients. Numerous sediment and ice records derived from the Southern Ocean and Antarctica document high-resolution climatic changes that allow us a better understanding of global climate evolution. Consistently with the global climatic trend, several sea surface temperature (SST) records of the Southern Ocean are marked by a distinct shift from low to high glacial/interglacial variability around Termination V (T V), called the Mid-Brunhes Event (MBE). Prior to T V, the Southern Ocean’s SST displays lower values and low variability. It points to a distinct expansion of the Southern Ocean cold water masses and positional changes of hydrographical fronts during most of the lower Middle Pleistocene, which started in the Pliocene. Beside large climatic changes, several abrupt distinct warming and cooling phases have been recognized. Some of them (MIS 22–19, MIS 11 and MIS 5) show similarities to MIS 1, which could be used for future climate predictions. In this paper we would like to present the middle and late Pleistocene climatic mechanisms in the Southern Ocean, and to show SST changes in relation to the hydrographic frontal movement, sea ice development and CO2 oscillations.
Źródło:: Przegląd Geologiczny; 2016, 64, 1; 35--42
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

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