ERRATUM: Expanded glaciers during a dry and cold Last Glacial Maximum in equatorial East Africa

Abstract

Glaciers on the world's highest tropical mountains are among the most sensitive components of the cryosphere, yet the climatic controls that influence their fluctuations are not fully understood. Here, we present the first 10 Be ages of glacial moraines in Africa and use these to assess the climatic conditions that influenced past tropical glacial extents. We applied 10 Be surface exposure dating to determine the ages of quartz-rich boulders atop moraines in the Rwenzori Mountains (~1°N, 30°E), located on the border of Uganda and the Democratic Republic of Congo. The 10 Be ages document expanded glaciers at ca. 24.9 and 21.5 ka, indicating that glaciers in equatorial East Africa advanced during the global Last Glacial Maximum (LGM; ca. 26-19.5 ka). A comparison of these moraine ages with regional paleoclimate records indicates that Rwenzori glaciers expanded contemporaneously with dry and cold conditions. Recession from the moraines occurred subsequent to ca. 21.5 ka, similar in timing to a rise in air temperature documented in East African lake records. Our results suggest that, on millennial time scales, past fluctuations of Rwenzori glaciers were strongly influenced by air temperature.

Co-variations of climate and silicate weathering in the Nile Basin during the Late Pleistocene

“…8b). Also, temperature in the last glacial tropical Africa was estimated to be about 3-5°C cooler than today (LGM, Kelly et al, 2014;Schefuß et al, 2005). Based on the above, we speculate that a progressive cooling in North-East Africa between ~110 and ~25 kyrs could possibly explain the progressive decrease of the δ 7 Li minima values, in response to gradual changes in soil conditions within the Nile Basin.…”