Scandinavian pattern and temperature changes shape European summer droughts over the past millennium. [PDF]
Xue H +5 more
europepmc +1 more source
Dynamical paleoclimatology generalized theory of global climate change
Saltzman, Barry 1931-
core
Holocene shoreline displacement and the impact of the Storegga tsunami on Hinnøya, northern Norway
The Holocene relative sea‐level (RSL) history of Norway's largest island, Hinnøya, has been investigated in detail, using sediment records from 25 isolation basins. The sediments were analysed for macrofossil and phytoplankton content, which served as the basis for identifying marine–lacustrine transitions, that is isolation contacts. Terrestrial plant
Anders Romundset +5 more
wiley +1 more source
Contrasting marine and terrestrial responses of South Asian summer monsoon system caused by hemispheric insolation. [PDF]
Wen Q +13 more
europepmc +1 more source
Józefów site is a case study which provides a detailed record of environmental and climate changes and confirms the main traces of the landscape morphogenesis of the Late Pleistocene established in central‐eastern Europe. This study presents a multiproxy reconstruction of palaeoenvironment under variable climatic conditions from the retreat of the ...
Aleksandra Majecka +11 more
wiley +1 more source
Baobab isotope records and rainfall forcing in Southwest Madagascar over the last 700 years. [PDF]
Razanatsoa E +4 more
europepmc +1 more source
To assess how the eastern part of the Limfjord system has changed over the Holocene, relative to the wider Limfjord and western Baltic region, a sedimentary succession spanning c. 9600–150 cal. a BP was collected from Nibe Bredning, near Sebbersund, from a shallow coastal inlet along the eastern connection between the Limfjord and the Kattegat (north ...
Gabriella M. Weiss +5 more
wiley +1 more source
Agent-based simulations reveal the possibility of multiple rapid northern routes for the second Neanderthal dispersal from Western to Eastern Eurasia. [PDF]
Coco E, Iovita R.
europepmc +1 more source
Palaeoglaciations in the Polar and Subpolar Ural Mountains
The Ural Mountains form a major physiographic boundary between the East European Plain and West Siberia, both repeatedly glaciated during the Pleistocene by the Barents–Kara ice sheet. Although the present‐day topography reflects significant glacial modification, the extent, chronology and interaction of mountain glaciers with the Barents–Kara ice ...
Bartosz Kurjanski +6 more
wiley +1 more source
Clay minerals evidences for cold-warm fluctuations in the Early Silurian. [PDF]
Zhang Z +5 more
europepmc +1 more source

