[HTML][HTML] Deglaciation of fennoscandia
To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the
form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we …
form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we …
The Last Interglacial–Glacial cycle (MIS 5–2) re-examined based on long proxy records from central and northern Europe
KF Helmens - Quaternary Science Reviews, 2014 - Elsevier
Current multi-proxy studies on a long sediment sequence preserved at Sokli (N Finland), ie
in the central area of Fennoscandian glaciations, are drastically changing classic ideas of …
in the central area of Fennoscandian glaciations, are drastically changing classic ideas of …
The development of the Baltic Sea Basin during the last 130 ka
During the Eemian interglacial 130–115 ka BP, the hydrology of the Baltic Sea was
significantly different from the Holocene. A pathway between the Baltic basin and the …
significantly different from the Holocene. A pathway between the Baltic basin and the …
A compilation of Western European terrestrial records 60–8 ka BP: towards an understanding of latitudinal climatic gradients
Terrestrial records of past climatic conditions, such as lake sediments and speleothems,
provide data of great importance for understanding environmental changes. However, unlike …
provide data of great importance for understanding environmental changes. However, unlike …
Pleistocene glaciations in Lithuania
R Guobytė, J Satkūnas - Developments in quaternary sciences, 2011 - Elsevier
Lithuania is a classical region covered with the sedimentary deposits of the six glacial and
eight ice-free stages. The oldest in Lithuania Quaternary sediments of pre-ice basins were …
eight ice-free stages. The oldest in Lithuania Quaternary sediments of pre-ice basins were …
Proxy comparison in ancient peat sediments: pollen, macrofossil and plant DNA
We compared DNA, pollen and macrofossil data obtained from Weichselian interstadial (age
more than 40 kyr) and Holocene (maximum age 8400 cal yr BP) peat sediments from …
more than 40 kyr) and Holocene (maximum age 8400 cal yr BP) peat sediments from …
Extent and chronology of Quaternary glaciation
J Ehlers, P Gibbard - Episodes, 2008 - indianjournalofcomputerscience …
In a recent INQUA project the extent of Pleistocene glaciations has been digitally mapped
and the chronology of events reviewed. The onset of the present Ice Age in both …
and the chronology of events reviewed. The onset of the present Ice Age in both …
Marine isotope stage 4 (71–57 ka) on the Western European margin: insights to the drainage and dynamics of the Western European Ice Sheet
Abstract Marine Isotope Stage (MIS) 4 (ca. 71–57 ka; within the Middle Weichselian
Substage) is considered a significant Pleistocene glaciation, but it remains poorly …
Substage) is considered a significant Pleistocene glaciation, but it remains poorly …
The marine δ18O record overestimates continental ice volume during Marine Isotope Stage 3
There is disagreement in the Quaternary research community in how much of the marine δ
18 O signal is driven by change in ice volume. Here, we examine this topic by bringing …
18 O signal is driven by change in ice volume. Here, we examine this topic by bringing …
The glaciation of Finland
P Johansson, JP Lunkka, P Sarala - Developments in quaternary sciences, 2011 - Elsevier
Abstract Middle Pleistocene Glaciations. In Lapland and western Finland there are sites
where till or glaciofluvial deposits underlie Eemian organic sediments. Many of them are …
where till or glaciofluvial deposits underlie Eemian organic sediments. Many of them are …