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Nowe stanowiska interstadialu Pilicy [formacja Chojny] w odkrywce Belchatow.

100%

Krzyszkowski D. , Nita M.

nr 11

788-797

Optical dating of a late quaternary sediment sequence from Sokli, Northern Finland

58%

Alexanderson H. , Eskola K. O. , Helmens K. F.

tom Vol. 32

51-59

Interstadial and non-glacial stadial sediments collected in boreholes from Sokli in northeastern Finland have been dated by optically stimulated luminescence on quartz and feldspar grains. The quartz OSL ages follow stratigraphic order, with one exception, and support the litho- and biostratigraphical correlation with the NW European mainland climate-stratigraphy and the marine oxygen-isotope stages. Feldspar IRSL dates generally overestimate the age, probably due to incomplete bleaching. The data show that during the last glacial cycle north-eastern Finland was not glaciated until MIS 5b, around 90 ka. Interstadial conditions occurred around ∼94 ka (MIS 5c), ∼74-80 ka (MIS 5a) and 42-54 ka (MIS 3). The OSL ages have large standard errors mainly due to small sample sizes, relatively poor luminescence characteristics and uncertainties in dose-rate determinations.

Zmiany klimatu w plejstocenie w świetle danych palinologicznych

58%

Granoszewski W. , Winter H.

tom Vol. 64, nr 1

43--48

The paper presents general climate changes during the last 2.6 Ma in the Northern Hemisphere. Plant formations of warm intervals (interglacials and interstadials) are briefly described. Disappearance of some more climate-sensitive tree taxa as well as climate changes during the Pleistocene in Northern Europe are also portrayed.