Timing of peat initiation across the central Congo Basin

Abstract The central Congo Basin contains the world’s most extensive tropical peatland complex, spanning 16.7 million hectares. Until now, radiocarbon dating of basal peats has been limited to 14 samples with poor spatial coverage, and suggested that peat typically initiated during the Holocene. We present 38 new basal dates, improving spatial coverage across the region. Some of the new basal dates are much older than any previous dates, indicating that peat initiated in the central Congo Basin at multiple locations in the Late Pleistocene. Our oldest basal date is 42 300 (41 200–43 800) calibrated years before present, making this one of the world’s oldest extant tropical peatlands, and twice as old as previously believed. The temporal distribution of basal dates suggests that changing climatic wetness has played a role in peat initiation in the region; numerous basal dates correspond with climatically wet phases, whilst few basal dates correspond with dry phases such as the Last Glacial Maximum (LGM). Today we find the central Congo Basin peatlands on wide interfluves between rivers, and on floodplains (mostly of the dendritic left-bank tributaries of the Congo River). We find the oldest basal dates on the floodplains of these left-bank tributaries, indicating a surprisingly high degree of channel stability over many millennia. This contrasts with, for example, peatlands on Amazonian floodplains, which are typically just a few thousand years old. The persistence of peat in the central Congo Basin since before the LGM, likely the most climatically dry period during the last 42 000 yr in this region, suggests that these areas may have played an important biogeographical role as forest refugia during glacial-interglacial cycles.

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Publication Details

Journal
Environmental Research Letters
Published
2025-06-27
DOI
https://doi.org/10.1088/1748-9326/ade905
Citations
6
Primary Topic
Geological formations and processes
Type
article
Field-Weighted Citation Impact
10.02
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article

Timing of peat initiation across the central Congo Basin

Chris Kiahtipes, Yannick E. Bocko, Nicholas T. Girkin, Pierre Bola et al.
6 citations
Environmental Research Letters
Geological formations and processes
10.02
article

Timing of peat initiation across the central Congo Basin

Chris Kiahtipes, Yannick E. Bocko, Nicholas T. Girkin, Pierre Bola, Greta C. Dargie, Corneille E. N. Ewango, Suspense A. Ifo, Enno Schefuß, Raphaël M. Tshimanga, Arnoud Boom, Andy J. Baird, Bart Crezee, Edward T. A. Mitchard, Paul J. Morris, George E. Biddulph, Ralph R Schneider, Simon L. Lewis, Brice Milongo, Donna Hawthorne, Joseph Kanyama, Yannick Garcin, Mark A. Trigg, Pauline Gulliver, Susan Page, Dylan M. Young, Ian T. Lawson, Déo R. V. Boukono, Lisa F. Louvouandou, Jodrhy P. Milandou Matoko, Gloire J. Kibongui, Sofie Sjoegersten, Ovide Emba Botuli
article en
6 citations

Abstract

Abstract The central Congo Basin contains the world’s most extensive tropical peatland complex, spanning 16.7 million hectares. Until now, radiocarbon dating of basal peats has been limited to 14 samples with poor spatial coverage, and suggested that peat typically initiated during the Holocene. We present 38 new basal dates, improving spatial coverage across the region. Some of the new basal dates are much older than any previous dates, indicating that peat initiated in the central Congo Basin at multiple locations in the Late Pleistocene. Our oldest basal date is 42 300 (41 200–43 800) calibrated years before present, making this one of the world’s oldest extant tropical peatlands, and twice as old as previously believed. The temporal distribution of basal dates suggests that changing climatic wetness has played a role in peat initiation in the region; numerous basal dates correspond with climatically wet phases, whilst few basal dates correspond with dry phases such as the Last Glacial Maximum (LGM). Today we find the central Congo Basin peatlands on wide interfluves between rivers, and on floodplains (mostly of the dendritic left-bank tributaries of the Congo River). We find the oldest basal dates on the floodplains of these left-bank tributaries, indicating a surprisingly high degree of channel stability over many millennia. This contrasts with, for example, peatlands on Amazonian floodplains, which are typically just a few thousand years old. The persistence of peat in the central Congo Basin since before the LGM, likely the most climatically dry period during the last 42 000 yr in this region, suggests that these areas may have played an important biogeographical role as forest refugia during glacial-interglacial cycles.

Environmental Research LettersVol. 20(8)
Centre National de la Recherche Scientifique (FR), University of Leeds (GB), University of Nottingham (GB), University of Leicester (GB), University of St Andrews (GB), University of Bremen (DE), Aix-Marseille Université (FR), University of South Florida (US), Department of Space (IN), Christian-Albrechts-Universität zu Kiel (DE), University of Kinshasa (CD), Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement (FR), Centre de Recherche et d’Enseignement de Géosciences de l’Environnement (FR), Université Pédagogique Nationale (CD), University of Mbandaka (CD), Scottish Universities Environmental Research Centre (GB), Institut de Recherche pour le Développement (FR), University College London (GB), Université de Kisangani (CD), Marien Ngouabi University (CG)
Openalex Percentile: Top 1%
Geological formations and processes
10.02
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