Northeast African temperature variability since the Late Pleistocene

作者：Loomis Shannon E^*; Russell James M; Lamb Henry F

来源：Palaeogeography, Palaeoclimatology, Palaeoecology, 2015, 423: 80-90.

DOI：10.1016/j.palaeo.2015.02.005

• Tropical paleoclimate
• East Africa
• GDGT
• Paleotemperature
• Holocene
• Lake Tana

The development and application of lacustrine paleotemperature proxies based on microbial membrane lipid structures, including the TEX86 and branched glycerol dialkyl glycerol tetraether (brGDGT) paleothermometers, have greatly advanced our understanding of the late-glacial and postglacial temperature history of Africa. However, the currently available records are from equatorial and southern hemisphere sites, limiting our understanding of the spatial patterns of temperature change. Here we use the brGDGT paleotemperature proxy to reconstruct Late Pleistocene and Holocene temperatures from Lake Tana, Ethiopia (12 degrees N, 37 degrees E). Following the termination of Heinrich Stadial 1 at similar to 15 ka, lake Tana experienced a 3.7 degrees C oscillation over 1.2 ky. Temperatures then increased abruptly by nearly 7 degrees C between 13.8 and 13.0 ka, followed by a slow warming trend that peaked during the mid Holocene. Temperatures subsequently cooled from similar to 6 ka to similar to 0.4 ka. These data indicate that temperature at Lake Tana was sensitive to climate changes caused by variations in the Atlantic Meridional Overturning Circulation during the Late Pleistocene, as well as to regional hydrodimatic changes and reorganizations of the monsoons. Our record suggests that late-glacial temperature changes in northeast Africa were linked to high-latitude northern hemispheric climate processes, but that subsequent post-glacial temperature variations were strongly influenced by tropical hydrology.

• 出版日期2015-4-1