Sorry! De informatie die je zoekt, is enkel beschikbaar in het Engels.
This programme is saved into My study choice.
This programme cannot be saved.
You are not logged in yet to My study choice Portal. Login or create an account to save your programmes.
Something went wrong, try again later.

Speed of ocean circulation explains past climate change in Africa

27 October 2021
Analysis of tiny carbonate fossils and sediment records dating back over 7 million years may hold the key to solving one of the outstanding puzzles of paleoanthropology.

Scientists have identified a new mechanism to account for the drastic aridification in eastern African over the past two million years - with likely implications for evolution and dispersal of our early human ancestors.

In a study published today in Nature, a team led by scientists at Cardiff University propose that starting roughly 2.1 million years ago, changes in the speed of Indian Ocean waters through the Mozambique Channel were synchronized with onset of the east-to-west atmospheric circulation pattern along the Pacific Ocean. This so-called Walker circulation resulted in subsequent changes in the Indian Ocean region causing pronounced dry spells in eastern Africa during glacial periods. The study also found that these increasingly dry and cold spells were punctuated by wetter and warmer periods.

Tiny fossils and foraminifera
For this study, a sediment core was taken from the Mozambique Channel – a 1,600 km-long arm of the western Indian Ocean located between Madagascar and Mozambique. Using tiny fossils of single-celled organisms known as foraminifera, as well as sediments taken from the core, the team reconstructed the flow speed of the ocean’s circulation extending 7 million years into the past.

The team identified two significant points when the speed of the ocean through the channel changed. The first occurred roughly 2.1 million years ago and coincided with the onset of the Pacific Walker Circulation – a phenomenon where easterly trade winds move surface water towards the west. The second change occurred roughly 900,000 years ago and coincided with the onset of intensive ice ages, which would go on to appear in major cycles of roughly 100,000 years.

“The establishment and long-term enhancement of the coupled Pacific and Indian Ocean Walker circulation would have suppressed rainfall in eastern Africa, particularly during ice ages after 2.1 million years ago,” says co-author of the study Professor Ian Hall, from Cardiff University’s School of Earth and Environmental Sciences.

Lead author of the study Dr Jeroen van der Lubbe, from VU Amsterdam and also from Cardiff University’s School of Earth and Environmental Sciences, says: “At first we were we were astonished to find that our detailed reconstruction of ocean flow speed in the Mozambique Channel remained relatively unchanged throughout several major shifts in the Earth’s climate system, such as the development of Northern Hemisphere icesheets, but so clearly reflected the synchronous establishment of the Pacific and Indian Ocean Walker circulation some 2.1 million years ago. Now, we have identified a mechanism, why this is the case."

Climate fluctuations critical factor for hominin evolution
The team say that their results will inform future studies to understand how climate fluctuations may have been a critical factor of hominin evolution and dispersal over the last 2.1 million years. Professor Jose Joordens from Naturalis Biodiversity Center and co-author adds: “Around 2 million years ago, hominin diversity in Africa was high implying a considerable widening of niches and dietary differentiation among several species of our genus Homo. Also, this is when early Homo populations for the first time expanded far beyond Africa. It is still an enigma what caused these events, but we believe that our detailed climate record may hold the key to solve many of the outstanding puzzles in paleoanthropology.”