Studies of glaciotectonized sub-till lacustrine deposits in Lønstrup Klint and Lodbjerg Klint, northern Jylland, Denmark, show the presence of plant and ani-mal remains from the Middle Weichselian "mammoth steppe". Radiocarbon dates on picked-out plant fragments yield ages around 30 ka BP, and a macrofossil plant assemblage in the lake sediments indicates that uplands were covered by an open, tree-less vegetation with herbs and scattered shrubs. Mean July temperatures were probably at least 6°C lower than at present. The datings suggest a change from marine to glacio-lacustrine environments in Vendsyssel slightly before 30 ka BP. Glacial thrusting and subsequent deposition of the youngest till in the region was connected with the ...
Studies of vegetation history bring a new incentive to our understanding of plant survival and migra...
This paper presents the first unambiguous terrestrial palaeoecological record for the late glacial “...
Cryoturbated organic beds and channel fills, intercalated with sandy and gravelly fluvial units, hav...
cs A new and fundamental outline of the Late Pleistocene geological history in SE Denmark is obtaine...
Eastern Denmark was an important region for the early immigration of humans into southern Scandinavi...
Plant macrofossil remains have been analysed from two raised peat bogs in northern Germany and Denma...
A 2 m thick laminated lacustrine deposit of silt and clay recovered from the high-latitudinal site a...
Late Weichselian litho-, bio-, and chronostratigraphy (i4C and varves) in southeastern Sweden provid...
Lithostratigraphy and chronostratigraphy of samples from 18 deep boreholes in Vendsyssel have result...
The North Sea is a large, shallow epicontinental sea dominated by a sandy bottom that reflects a hig...
Late Weichselian litho-, bio-, and chronostratigraphy (14C and varves) in southeastern Sweden provid...
The Quaternary sedimentary succession in Vendsyssel, northern Denmark, contains a unique, high-resol...
The site Pilgrimstad in central Sweden has often been cited as a key locality for discussions of ice...
During the early part of the Allerød period, from c. 13 600 to 13 330 years BP, unstable soils with ...
The site Pilgrimstad in central Sweden has often been cited as a key locality for discussions of ice...
Studies of vegetation history bring a new incentive to our understanding of plant survival and migra...
This paper presents the first unambiguous terrestrial palaeoecological record for the late glacial “...
Cryoturbated organic beds and channel fills, intercalated with sandy and gravelly fluvial units, hav...
cs A new and fundamental outline of the Late Pleistocene geological history in SE Denmark is obtaine...
Eastern Denmark was an important region for the early immigration of humans into southern Scandinavi...
Plant macrofossil remains have been analysed from two raised peat bogs in northern Germany and Denma...
A 2 m thick laminated lacustrine deposit of silt and clay recovered from the high-latitudinal site a...
Late Weichselian litho-, bio-, and chronostratigraphy (i4C and varves) in southeastern Sweden provid...
Lithostratigraphy and chronostratigraphy of samples from 18 deep boreholes in Vendsyssel have result...
The North Sea is a large, shallow epicontinental sea dominated by a sandy bottom that reflects a hig...
Late Weichselian litho-, bio-, and chronostratigraphy (14C and varves) in southeastern Sweden provid...
The Quaternary sedimentary succession in Vendsyssel, northern Denmark, contains a unique, high-resol...
The site Pilgrimstad in central Sweden has often been cited as a key locality for discussions of ice...
During the early part of the Allerød period, from c. 13 600 to 13 330 years BP, unstable soils with ...
The site Pilgrimstad in central Sweden has often been cited as a key locality for discussions of ice...
Studies of vegetation history bring a new incentive to our understanding of plant survival and migra...
This paper presents the first unambiguous terrestrial palaeoecological record for the late glacial “...
Cryoturbated organic beds and channel fills, intercalated with sandy and gravelly fluvial units, hav...