FN Archimer Export Format PT J TI Microscopic charcoals in ocean sediments off Africa track past fire intensity from the continent BT AF Haliuc, Aritina Daniau, Anne-Laure Mouillot, Florent Chen, Wentao Leys, Bérangère David, Valérie Hanquiez, Vincent Dennielou, Bernard Schefuß, Enno Bayon, Germain Crosta, Xavier AS 1:1;2:1;3:2;4:2;5:3;6:1;7:1;8:4;9:5;10:4;11:1; FF 1:;2:;3:;4:;5:;6:;7:;8:PDG-REM-GEOOCEAN-ASTRE;9:;10:PDG-REM-GEOOCEAN-ASTRE;11:; C1 University Bordeaux, CNRS, Bordeaux INP, EPOC, UMR 5805, F-33600, Pessac, France UMR CEFE, University Montpellier, CNRS, EPHE, IRD, Univ. Paul Valery Montpellier 3, 1919 route de Mende, 34293, Montpellier, CEDEX 5, France Aix Marseille University, Avignon University, CNRS, IRD, IMBE, Aix Technopole de l’environnement Arbois Méditerranée Avenue Louis Philibert - Batiment Villemin, 13545, Aix-en-Provence, Cedex 4, France University Brest, CNRS, Ifremer, Geo-Ocean, F-29280, Plouzané, France MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, 28359, Bremen, Germany C2 UNIV BORDEAUX, FRANCE UNIV MONTPELLIER, FRANCE UNIV AIX MARSEILLE, FRANCE IFREMER, FRANCE UNIV BREMEN MARUM, GERMANY SI BREST SE PDG-REM-GEOOCEAN-ASTRE UM GEO-OCEAN IN WOS Ifremer UMR DOAJ copubli-france copubli-europe copubli-univ-france IF 7.9 TC 2 UR https://archimer.ifremer.fr/doc/00834/94612/101993.pdf https://archimer.ifremer.fr/doc/00834/94612/101994.pdf https://archimer.ifremer.fr/doc/00834/94612/101995.pdf LA English DT Article CR CONGOLOBE NAUSICAA-IMAGES 2-MD105 ZAIANGO ZAIANGO1 ZAIANGO2 ZAIANGOROV BO Pourquoi pas ? Marion Dufresne L'Atalante AB Fires in Africa account for more than half of global fire-carbon emissions but the long-term evolution of fire activity and its link to global climate change remains elusive. Paleofire records provide descriptive information about fire changes through time, going beyond the range of satellite observations, although fire regime characteristics are challenging to reconstruct. To address this conceptual gap, we report here the abundance and morphometric data for a large set of microscopic charcoal samples (n = 128) recovered from surface ocean sediments offshore Africa. We show that in subtropical Southern Africa, large and intense fires prevailing in open savanna-grassland ecosystems produce a high abundance of small and elongated microcharcoal particles. In contrast, in the forest ecosystems of equatorial and tropical regions of western and central Africa, low-intensity fires dominate, producing low amounts of squared microcharcoal particles. Microcharcoal concentration and morphotype in marine sediment records off Africa are thus indicative of fire regime characteristics. Applied to down-core marine charcoal records, these findings reveal that at orbital time-scale intense and large, open grassland-savanna fires occurred during wet periods in the sub-tropical areas. A strong contribution of fire carbon emissions during periods of precession and summer insolation maxima in the geological record is thus expected. PY 2023 PD APR SO Communications Earth & Environment SN 2662-4435 PU Springer Science and Business Media LLC VL 4 IS 1 UT 000975284100001 DI 10.1038/s43247-023-00800-x ID 94612 ER EF