Testing the 'megadrought' hypothesis: the timing, cause and impacts of climate change in equatorial Africa (DeepCHALLA-UK)
Lead Research Organisation:
University of Cambridge
Department Name: Geography
Abstract
Over the last 25,000 years, East African climate has responded to changes in the Earth's orbit (mainly precession) that influence long-term variations in monsoonal rainfall and the migration of the intertropical convergence zone. But climate of earlier periods, back to 250,000 years, is less well understood as few continuous high resolution terrestrial records exist. This is a major gap in our understanding of equatorial climate from a region critical to the evolution of our own species. The African megadrought hypothesis states that droughts lasting many thousands of years occurred during the last interglacial (130,000 - 80,000 years ago) across tropical Africa. Evidence from the few sites investigated indicate they were of a severity greater than any droughts of succeeding time periods, and had major implications for evolutionary processes, for example continent wide migrations in Homo sapiens. Such long and intensely dry events in the history of African climate are an unexpected phenomenon, and their precise timing, origin and extent, has yet to be established. We hypothesise that megadroughts arose due to monsoon failure caused by changes in the shape of earth's orbit around the sun (the ~100,000 year eccentricity cycle), amplifying changes in the seasonal distribution of solar radiation (the ~21,000 year precession cycle). In order to fully understand these extreme climatic events, we will explore climate changes in the East African equatorial region spanning two glacial-interglacial cycles (i.e. the last ~250,000 years) giving critical context to the megadroughts and their causes.
The project focuses on the sedimentary record from Lake Challa, a deep lake on the flank of Kilimanjaro. Unlike other studies from East Africa, the easterly position of Lake Challa places it beyond the direct influence of the Atlantic climate system, thus removing this aspect as a possible forcing and allowing us to isolate a record of monsoonal variation. The outstanding potential of these lake sediments to provide a long, sensitive repository of environmental change data has been established by a prior study of the last 25,000 years, that resulted in multi-disciplinary articles in 'Nature' on orbital forcing of climate, 'Science' on the laminated sediments and relation to ENSO, and 'Geology' concerning the seasonality of climate variations and the Kilimanjaro ice core. Additional data sets (published in other journals) confirm that the environmental proxies and dating methods proposed here will deliver a high quality record from this lake. The age of the deeper sediments has been estimated from seismic profiles of the sedimentary layers in the lake; new, absolute dates are required to identify the basal sediment age and rates of subsequent sedimentation. This project will lead in modelling of sediment ages from the new, deep cores through radiocarbon dates, palaeomagnetism to detect the presence of well-dated magnetic reversals and dating of volcanic ash layers through Ar/Ar dating and chemical correlation. Carbon and oxygen isotope data from diatom silica are excellent tools to reveal the megadroughts due to their sensitivity to humid/arid shifts as already demonstrated during the last 25,000 years.
This project is part of an international consortium, partly funded by the International Continental scientific Drilling Program to recover cores from the lake. Our international partners have already gained support from their own national funding councils and will contribute complimentary environmental proxies (e.g. pollen, organic biomarkers) as well as additional dating (Ar/Ar) and, finally, climate modelling (ranging from local hydrology to global climate modelling) used to understand the global significance of our results in terms of forcing factors. We have Kenyan and Tanzanian collaborators, who will also act as conduits to ensure our discoveries help inform ongoing and future conservation needs and development strategies.
The project focuses on the sedimentary record from Lake Challa, a deep lake on the flank of Kilimanjaro. Unlike other studies from East Africa, the easterly position of Lake Challa places it beyond the direct influence of the Atlantic climate system, thus removing this aspect as a possible forcing and allowing us to isolate a record of monsoonal variation. The outstanding potential of these lake sediments to provide a long, sensitive repository of environmental change data has been established by a prior study of the last 25,000 years, that resulted in multi-disciplinary articles in 'Nature' on orbital forcing of climate, 'Science' on the laminated sediments and relation to ENSO, and 'Geology' concerning the seasonality of climate variations and the Kilimanjaro ice core. Additional data sets (published in other journals) confirm that the environmental proxies and dating methods proposed here will deliver a high quality record from this lake. The age of the deeper sediments has been estimated from seismic profiles of the sedimentary layers in the lake; new, absolute dates are required to identify the basal sediment age and rates of subsequent sedimentation. This project will lead in modelling of sediment ages from the new, deep cores through radiocarbon dates, palaeomagnetism to detect the presence of well-dated magnetic reversals and dating of volcanic ash layers through Ar/Ar dating and chemical correlation. Carbon and oxygen isotope data from diatom silica are excellent tools to reveal the megadroughts due to their sensitivity to humid/arid shifts as already demonstrated during the last 25,000 years.
This project is part of an international consortium, partly funded by the International Continental scientific Drilling Program to recover cores from the lake. Our international partners have already gained support from their own national funding councils and will contribute complimentary environmental proxies (e.g. pollen, organic biomarkers) as well as additional dating (Ar/Ar) and, finally, climate modelling (ranging from local hydrology to global climate modelling) used to understand the global significance of our results in terms of forcing factors. We have Kenyan and Tanzanian collaborators, who will also act as conduits to ensure our discoveries help inform ongoing and future conservation needs and development strategies.
Planned Impact
The scientific and societal impact of our work will be both significant and diverse. Scientific outputs will be delivered in the very top journals; a credible ambition based on the past history of the team and the high impact of the previous CHALLACEA project on the lake (Nature, Science, Geology). This work is truly discovery-based, as fundamental climate changes which likely impact on our understanding of climate dynamics remain to be discovered in this region during the targeted time intervals. Broader implications for evolutionary processes, biodiversity and hominin dispersal are all expected from the objectives of this proposal.
International impact is ensured through our embedded international network within DeepCHALLA and the offices of the ICDP programme. We will also bring our findings to larger and broader international organisations such as Future Earth. Communications at top international conferences (AGU, EGU etc.) will further accelerate the impact.
As scientists working in developing countries we have a responsibility to communicate and engage with the local communities and national institutions. This has already begun through a two-centred meeting held in Nairobi and Taveta in 2012 hosted by the National Museum of Kenya and the University of Nairobi. This identified local priorities of water resources and capacity building. We will use the DeepCHALLA climate and hydrological modelling framework to deliver information about recent and future climate variability at Town Hall meetings. Secondly, we will work with regional development organisations and co-host a north-south conference in the area, likely Arusha, Tanzania. Thirdly we will build capacity through contributing to MSc programmes in Kenyan and Tanzanian universities, working with existing bilateral exchange programmes and using pathway to impact funds to invite an African PhD student to the UK to learn of the importance and practice of developing scientific impact.
A key tool to communicate our research beyond academia will be the writing of blogs and news stories in conjunction with our universities' media experts and promoted by Twitter, a communication tool that can be targeted at specific journalists. Outlets including regular articles in Climatica (http://climatica.org.uk/), the BGS GeoBlogy and university blog sites are proposed. Engagement with the general public and school children is to be achieved through talks at key popular science events such as the biennial BGS open day and local museum events. We will also use our institutional outreach networks to take an interactive demonstration into schools and museums to help inform the wider public and future generations about environmental change. Funds for developing high quality materials are requested.
International impact is ensured through our embedded international network within DeepCHALLA and the offices of the ICDP programme. We will also bring our findings to larger and broader international organisations such as Future Earth. Communications at top international conferences (AGU, EGU etc.) will further accelerate the impact.
As scientists working in developing countries we have a responsibility to communicate and engage with the local communities and national institutions. This has already begun through a two-centred meeting held in Nairobi and Taveta in 2012 hosted by the National Museum of Kenya and the University of Nairobi. This identified local priorities of water resources and capacity building. We will use the DeepCHALLA climate and hydrological modelling framework to deliver information about recent and future climate variability at Town Hall meetings. Secondly, we will work with regional development organisations and co-host a north-south conference in the area, likely Arusha, Tanzania. Thirdly we will build capacity through contributing to MSc programmes in Kenyan and Tanzanian universities, working with existing bilateral exchange programmes and using pathway to impact funds to invite an African PhD student to the UK to learn of the importance and practice of developing scientific impact.
A key tool to communicate our research beyond academia will be the writing of blogs and news stories in conjunction with our universities' media experts and promoted by Twitter, a communication tool that can be targeted at specific journalists. Outlets including regular articles in Climatica (http://climatica.org.uk/), the BGS GeoBlogy and university blog sites are proposed. Engagement with the general public and school children is to be achieved through talks at key popular science events such as the biennial BGS open day and local museum events. We will also use our institutional outreach networks to take an interactive demonstration into schools and museums to help inform the wider public and future generations about environmental change. Funds for developing high quality materials are requested.
Publications
Martin-Jones C
(2024)
The >250-kyr Lake Chala record: A tephrostratotype correlating archaeological, palaeoenvironmental and volcanic sequences across eastern Africa
in Quaternary Science Reviews
Martin-Jones C
(2019)
History of scoria-cone eruptions on the eastern shoulder of the Kenya-Tanzania Rift revealed in the 250-ka sediment record of Lake Chala near Mount Kilimanjaro
in Journal of Quaternary Science
Di Chiara A
(2024)
A Lake Record of Geomagnetic Secular Variations for the Last 23 ka From Lake Chala: Toward a Composite Directional Lake Record of the Earth's Magnetic Field for Equatorial East Africa
in Geochemistry, Geophysics, Geosystems
Baxter AJ
(2023)
Reversed Holocene temperature-moisture relationship in the Horn of Africa.
in Nature
Description | We have generated a high quality palaeoclimate proxy record (stable isotope data) for the DeepChalla core spanning ~250 ky, which provides an understanding of the lake formation, evolution and response to climate change; compilation of a tephra-based explosive volcanic eruption history from regional volcanoes (one paper published, one in prep). |
Exploitation Route | The Co-I team, in collaboration with project partners will continue to analyse and publish the data. The final absolutely dated continuous and high-resolution tropical palaeoclimate record will become a benchmark for academic palaeoclimate and archaeological studies in Eastern Africa. Volcanologists will use the tephra record to improve understanding of volcanic histories, which will feed into hazard assessment. Two courses will be put on in Tanzania and Kenya for masters students (knowledge-exchange) based around the research we have carried out at Lake Chala, in April 2022. This event has been pushed back from 2020 because of COVID and lies beyond our already extended funding window, so the UK team will not be able to participate in person. |
Sectors | Education Environment Culture Heritage Museums and Collections |
Description | Explosive Volcanism in the Kenyan Rift: A Tephrostratigraphic Perspective |
Amount | £39,822 (GBP) |
Funding ID | 2314467 |
Organisation | Natural Environment Research Council |
Sector | Public |
Country | United Kingdom |
Start | 09/2019 |
End | 09/2023 |
Description | Improved Dating of Modern Human Evolution in the Middle - Late Pleistocene, East Africa. |
Amount | £67,000 (GBP) |
Organisation | Natural Environment Research Council |
Department | National Environmental Isotope Facility (NEIF) |
Sector | Public |
Country | United Kingdom |
Start | 08/2019 |
Description | Reconstructing the impact of the Youngest Toba Tuff volcanic eruption by geochemical analysis in Lake Chala |
Amount | £7,350 (GBP) |
Organisation | Natural Environment Research Council |
Department | NERC Isotope Geosciences Laboratory |
Sector | Academic/University |
Country | United Kingdom |
Start | 06/2023 |
End | 10/2023 |
Title | Lake Chala (Kenya/Tanzania) chronology and isotope data, 0 - >250 kyr BP (DeepCHALLA project) (NERC Grant NE/P011969/1) |
Description | This dataset presents tephra layers, Ar-dates, age-model & stable isotope data from the >250 kyr-long Lake Chala sediment record, Kenya/Tanzania. The file is split into six tables: (1) metadata on the 30 tephra layers (29 visible tephra layers, one cryptotephra) studied to date, including sample and core codes, summary characteristics and ages; (2) summary of Ar-dating results on ten of the Lake Chala tephra layers; (3) the DCH_TephraAge Bayesian age model, which combines tephra, 210Pb and 14C age-estimates for the length of the core; (4) Raw single-grain WDS-EPMA results for all tephra layers studied in the DeepCHALLA sediment record; and (5) secondary standard data; (6) unpublished Diatom ?18O (‰ VSMOW), Bulk organic ?13C (‰), %C and Diatom d13C (‰) measurements for the full length of the core (given on a composite depth scale). These chronological data (Tables 1-5) are central to the reconstruction of palaeoclimate from a multi-proxy analyses of the Lake Chala sediment sequence and are included in publications by Baxter et al. (2023) and Martin-Jones et al. (2020, in review), for which references are given in the appropriate files. Stable isotope data (produced by Barker and Leng) remains unpublished at the time of upload. The data was generated by Catherine Martin-Jones, Christine Lane, Maarten Blaauw, Darren Mark, Melanie Leng and Phil Barker between 2017-2022. Much of the tephra data is published and references are provided. |
Type Of Material | Database/Collection of data |
Year Produced | 2023 |
Provided To Others? | Yes |
Impact | N/A |
URL | http://data.bgs.ac.uk/id/dataHolding/13608096 |
Description | DeepCHALLA: two glacial-interglacial cycles (ca. 250,000 years) of climate and ecosystem dynamics on the East African equator |
Organisation | International Continental Scientific Drilling Program |
Sector | Charity/Non Profit |
PI Contribution | Myself and research team members Barker, Blaauw and Leng are collaborators on the wider DeepCHALLA ICDP-funded project, which is led by PI Dirk Verschuren at Ghent University. We contribute our expertise and data to this wider project. Specifically, our NERC grant research will underpin the chronology for the full lacustrine core sequence from Lake Challa, with a focus on understanding the processes operating at the time of the Megadroughts in East Africa. |
Collaborator Contribution | ICDP provided part-funding, infrastructure and expertise to facilitate the coring of Lake Challa in 2016, which is the focus of the NERC project. The funding was not directly received by UK project partners. |
Impact | Publication and impact outcomes to follow. |
Start Year | 2014 |
Description | AFQUA workshop: Creating Chronologies |
Form Of Engagement Activity | Participation in an activity, workshop or similar |
Part Of Official Scheme? | No |
Geographic Reach | International |
Primary Audience | Postgraduate students |
Results and Impact | This one-day workshop delivered at the National Museum of Kenya, Nairobi, concentrated on interpreting dated sediment cores in order to create reliable chronologies. After discussing the theory, hands-on computer sessions were held to work with software dedicated to age-depth modelling. Dr Maarten Blaauw, coI on DeepChalla, is the author of several age-depth modelling software packages, and delivered this workshop. The workshop was attended by students and early-to-mid career researchers from Kenya, South Africa, the US, and Europe. Based on short presentations during the workshop, a set of 5 free radiocarbon dates was awarded by the 14CHRONO Centre, Queen's University Belfast to one of the Kenyan participants, in order to help producing more robust chronologies for her records. The teaching material developed for this workshop was subsequently used elsewhere by Dr Blaauw, including at a chronology workshop delivered at the National University of Mexico (UNAM). |
Year(s) Of Engagement Activity | 2018 |
URL | https://docs.wixstatic.com/ugd/70ce02_bba772d0d06f4df6ae77eb6c46018955.pdf |
Description | AFQUA workshop: Understanding environmental risk and hazards using lake sediments |
Form Of Engagement Activity | Participation in an activity, workshop or similar |
Part Of Official Scheme? | No |
Geographic Reach | International |
Primary Audience | Postgraduate students |
Results and Impact | DeepChalla Project PDRAs, Dr Heather Moorhouse and Dr Catherine Martin-Jones, prepared and gave a one day workshop on "Understanding environmental risk and hazards using lake sediments" - using material and expertise closely related to the DeepChalla project. The workshop was held at the National Museum of Kenya, following the African Quaternary Association's second congress meeting, and intended as a trial capacity-building event, in respect to the DeepCHALLA projects associated ODA award. The workshop was attended by early career researchers from Kenya and Europe. We do not know of subsequent impacts of the event on attendees, but have now refined materials and begun planning for a subsequent future capacity-building workshop. Dr Martin-Jones (PDRA) and Prof Lane (PI) have since used some of the content with A-Level students at a University of Cambridge Geography taster day. |
Year(s) Of Engagement Activity | 2018 |
URL | https://docs.wixstatic.com/ugd/70ce02_bba772d0d06f4df6ae77eb6c46018955.pdf |