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reconstruction based on the pollen profile from Bispingen, Germany, the evaluation of the palaeobotanical and the stable isotope data presented here strongly suggests relatively stable temperature for most ...
gradient across the North Atlantic, leading to lower interglacial will end, which has been a matter of much debate (see, temperatures and precipitation over central Europe. These hydro- for example, refs 1,2 ...
below 12025 vy. The North Atlantic Seaboard Programme (NASP, a working group of IGCP-253) produced the most reliable synthesis of climatic changes during the last Glacialâ Interglacial transition (Lowe ...
regions across the study area, we calculated temperature change velocity from the Last Interglacial (LIG; ~120,000–140,000 years BP) towards the Last Glacial Maximum using the following R packages; raster ...
changes to the consistent Atlantic Meridional Overturning Circulation variability, which modulated North Hemisphere temperatures and displacements of Inter-Tropical Convergence Zone and Walker circulation ...
climate of the Libyan central Sahara is hyperarid and linked to low altitude pressure and winds over North Africa [19]. Scarce meteorological data are available for the Tadrart Acacus massif: the mean ...
the distribution of Q. robur under climatic conditions of the Present, the mid-Holocene [HOL, c. 6000 years before present (YBP)], the Last Glacial Maximum (LGM, c. 22000 YBP) and the Last Interglacial (LIG, c ...
) are to some extent congruent with known pollen records. Unambiguous occurrences of beech pollen from LGM deposits are known from the Sea of Marmara, off the central northern Turkish Black Sea coast, and from ...
from Cameroon (CP 10) and Angola/Congo (CP 11). This could account for the isolation of the Cameroon highlands, as shown by pollen data from the last glacial period in western Central Africa ...
peaks in central Italy by the numerical conversion function between lake mesocosms and temperature [9]. Using carbonate sediments in lakes, we quantitatively reconstructed the early to mid-Holocene ...
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