Late Glacial deglaciation of the Zackenberg area, NE Greenland
The Greenland Ice Sheet (GrIS) is a key component of the global climate system. However, our current understanding of the spatio-temporal oscillations and landscape transformation of the GrIS margins since the last glacial cycle is still incomplete.
Garcia-Oteyza, J. +17 more
openaire +8 more sources
PLANT MACROFOSSIL RECORDS | Late Glacial Multidisciplinary Studies [PDF]
Amplitudes and rates of climate changes and environmental responses were especially high during the Late Glacial (ca. 16 000–11 500 years BP). By applying several methods on the same material (if possible on the same core to avoid correlation problems ...
Birks, H.H. +7 more
core +1 more source
Life hung by a thread: endurance of Antarctic fauna in glacial periods [PDF]
Today, Antarctica exhibits some of the harshest environmental conditions for life on Earth. During the last glacial period, Antarctic terrestrial and marine life was challenged by even more extreme environmental conditions.
Thatje, S. +12 more
core +1 more source
Progress in palynology of the Gelasian–Calabrian Stages in Europe: Ten messages [PDF]
Europe has at present the most extensive network of palynological sites covering the Late Pliocene and the Early Pleistocene or roughly the Gelasian-Calabrian Stages. This paper covers ten points of recent progress in the palynology of this time period:
Leroy, SAG
core +4 more sources
Synoptic climate change as a driver of late Quaternary glaciations in the mid-latitudes of the Southern Hemisphere [PDF]
The relative timing of late Quaternary glacial advances in mid-latitude (40-55° S) mountain belts of the Southern Hemisphere (SH) has become a critical focus in the debate on global climate teleconnections.
H. Rother, J. Shulmeister
doaj
Diverse phenotypes of Late Glacial–Early Holocene downy birch (Betula pubescens Erh.) and the morphology of early Preboreal tree stands in southern Schleswig-Holstein [PDF]
The flexibility in growth of Betula pubescens is taken as example for possible erroneous imaginations of Late Glacial–Early Holocene living conditions.
S. Krüger
doaj +1 more source
Today, the Late Glacial interstadials Bølling and Allerød, originally defined in northern Europe, are often applied as chronozones in different palaeoclimate contexts across the Northern Hemisphere. The scientific community in both palaeoclimate research
Olaf JÖRIS, Esteban ÁLVAREZ FERNÁNDEZ
doaj
This collective project of research, which started in 2009, is dedicated to hunter-gatherers societies in Paris Basin from the fourteenth millenium cal BC until the sixth millenium cal BC, i.e during the Late Glacial and the beginning of the Post Glacial.
Boris Valentin
doaj +1 more source
Carbonate cementation in the late glacial outwash and beach deposits in northern Estonia [PDF]
The sedimentary environments, morphology and formation of carbonate cement in the late glacial glaciofluvial outwash and beach deposits in northern Estonia are discussed.
Maris Rattas, Pille Lomp, Argo Jõeleht
doaj +1 more source
The origin and evolution of small dry valleys in the last-glacial area on the example of the Pomeranian Lake District (Poland) [PDF]
Short dry valleys forming a part of the relief characteristic of the temperate zone occur particularly frequently in areas related to the young-glacial zone.
Marek Majewski, Renata Paluszkiewicz
doaj +1 more source

