Late Pleistocene desiccation of Lake Tana, source of the Blue Nile.
Lead Research Organisation:
University of St Andrews
Department Name: Earth and Environmental Sciences
Abstract
Lake Tana, in the highlands of northern Ethiopia, is the source of the Blue Nile, one of the world's great rivers. Surprisingly, very little is known about the age and history of this lake: one estimate from the 1930's is that it was formed 10,000 years ago by a lava dam. Similarly, little is known about the climatic history of the wider region that comprises the Blue Nile headwaters, despite the fact that the Nile has long been recognized as critical to the resources of ancient and modern Egypt. New geophysical and core data, obtained by us in October 2003 and September 2004 with NERC support, show that the lake may be at least 40,000 years old. Our new data also show that the lake dried out at around 16,000 years ago, and almost certainly at apparently regular intervals during the later stages of the last Ice Age. It is possible that the lake dried because of intense droughts lasting one or two hundred years, and that the droughts were caused by disruption of Africa's monsoon climate when iceberg-laden meltwater from North America flooded the North Atlantic - the Heinrich events. In this new PalaeoTana Project, we aim to test these hypotheses by drilling a sediment core, up to 100m in length, from the northern basin of Lake Tana, in about 10m water depth, and about 2km from shore. The core will be scanned at high resolution using X-ray fluorescence, X-ray and colour imagery, geophysical and magnetic core-scanning technology, without damaging the sedimentary components. The resulting datasets will identify past desiccation events, which will be investigated in detail and interpreted by comparison to sediments of the known drying-out event at 16,000 years ago. Dating the sediments by appropriate methods including luminescence, tephrochronology, and Argon-Argon dating will allow precise estimates of the timing and duration of the drought events. The relative timing of these events in comparison with abrupt climatic events in ocean cores (especially Heinrich events), and in other continental records, will allow inferences about the global- scale mechanisms of abrupt climate change. The data can also be used to test climate models, and thus to help judge the accuracy of model-predicted abrupt climate change in the future. A long core record of past climate and environment from this part of Africa would have major significance for understanding both regional environmental change, because of the influence of the Nile on NE Africa and the eastern Mediterranean, and global climate. It will contribute to understanding how future changes in ocean temperature and circulation will affect global climate, especially in the heavily populated monsoon regions of Africa and Asia. It will also have significance for understanding the later stages of human evolution in and dispersal out of Africa, by providing a record of the environmental changes that influenced early human populations and their water, plant and hunting resources.
Organisations
Publications
Schlolaut G
(2018)
An extended and revised Lake Suigetsu varve chronology from ~50 to ~10 ka BP based on detailed sediment micro-facies analyses
in Quaternary Science Reviews
Blinkhorn J
(2018)
The structure of the Middle Stone Age of eastern Africa
in Quaternary Science Reviews
Martin Trauth
(2018)
Abrupt or Gradual? Change Point Analysis of the Late Pleistocene-Holocene Chew Bahir Record from Southern Ethiopia
in Quaternary Research
Gil-Romera G
(2019)
Long-term fire resilience of the Ericaceous Belt, Bale Mountains, Ethiopia.
in Biology letters
Bittner L
(2020)
Revisiting afro-alpine Lake Garba Guracha in the Bale Mountains of Ethiopia: rationale, chronology, geochemistry, and paleoenvironmental implications
in Journal of Paleolimnology
Grove M
(2020)
Neural networks differentiate between Middle and Later Stone Age lithic assemblages in eastern Africa.
in PloS one
Bronk Ramsey C
(2020)
Reanalysis of the Atmospheric Radiocarbon Calibration Record from Lake Suigetsu, Japan
in Radiocarbon
Schaebitz F
(2021)
Hydroclimate changes in eastern Africa over the past 200,000 years may have influenced early human dispersal
in Communications Earth & Environment
Roberts H
(2021)
Using multiple chronometers to establish a long, directly-dated lacustrine record: Constraining >600,000 years of environmental change at Chew Bahir, Ethiopia
in Quaternary Science Reviews
Grove M
(2021)
Testing the Integrity of the Middle and Later Stone Age Cultural Taxonomic Division in Eastern Africa
in Journal of Paleolithic Archaeology
Description | This work revealed that the Northern Ethiopian Highlands have a composite volcanic history that records the development of two temporally distinct flood basalt piles (an older one at +3i Myr and a younger one at ca. 28 Myr) separated by a short-lived episode (<1 Myr) of intense felsic volcanism. The implications are that Lake Tana might be the exhumed cauldera of an enormous explosive volcano (geophysical surveys reveal the Lake to contain >>100m of sedimentary infill). Ongoing work is testing the linkages (or lack thereof) between these volcanic events and the global climatic decline that marks this period in Earth history (the late Eocene through Oligocene). |