Results 71 to 80 of about 1,748,474 (195)
The deglaciation of the mountains of Mexico and Central America
The last deglaciation is an interval of marked changes in the climate system. The records of glaciation of tropical mountains offer unique opportunities to assess the timing of changes and the sensitivity of tropical climates to global and regional ...
L. Vázquez-Selem, M.S. Lachniet
doaj +1 more source
Dual ancestries and ecologies of the Late Glacial Palaeolithic in Britain. [PDF]
Charlton S +19 more
europepmc +1 more source
New lithological, palinological and chronological data obtained through the study of bottom sediments from four small lake depressions on the Pomor Coast, Onega Bay, White Sea are presented.
Vasili Kolka +2 more
doaj +1 more source
Application data base paleogeographic Kola peninsula «Q-KOLA» in paleolimnological research
The paleogeographic database “Q-KOLA” was created to systematize, statistically analyze and visualize information about the history of the natural ecosystems of the Kola Peninsula in the Late Glacial and Holocene. The database can be used in limnological
Ivan Grekov, Dmitry Subetto
doaj +1 more source
Summer paleohydrology during the Late Glacial and Early Holocene based on δ2H and δ18O from Bichlersee, Bavaria. [PDF]
Prochnow M +10 more
europepmc +1 more source
River response to late quaternary environmental change in Corsica [PDF]
Mediterranean river systems are particularly sensitive to environmental change and often provide good archives to reconstruct fluvial histories. This study investigates river response to environmental change in two steep land river catchments in Corsica.
Hewitt, Suzanne
core +3 more sources
A Continuous Centennial Late Glacial-Early Holocene (15-10 cal kyr BP) Palynological Record from the Iberian Pyrenees and Regional Comparisons. [PDF]
Rull V +4 more
europepmc +1 more source
Late-Glacial Cwm Glaciers In Wales [PDF]
Abstract The evidence for the existence of small glaciers in the cwms of the Caernarvonshire mountains during the Late-glacial Period is presented, and by an analysis of their distribution some of the factors responsible for their formation are deduced. These were primarily protection from insolation, drifting of snow into the cirques
openaire +1 more source
An examination of the Geochemical properties of late devensian glacigenic sediments in Eastern England [PDF]
Onshore advance of the North Sea lobe of the Late Devensian British Ice Sheet the last glaciation resulted in the deposition of thick multiple till sequences along the coasts of east Yorkshire and north Lincolnshire.
Boston, Clare M.
core

