Late Holocene forest contraction and fragmentation in central Africa

During the warmer Holocene Period, two major climatic crises affected the Central African rainforests. The first crisis, around 4000 cal yr BP, caused the contraction of the forest in favor of savanna expansion at its northern and southern periphery. The second crisis, around 2500 cal yr BP, resulted in major perturbation at the forest core, leading to forest disturbance and fragmentation with a rapid expansion of pioneer-type vegetation, and a marked erosional phase. The major driver of these two climatic crises appears to be rapid sea-surface temperature variations in the equatorial eastern Atlantic, which modified the regional atmospheric circulation. The change between ca. 2500 to 2000 cal yr BP led to a large increase in thunderstorm activity, which explains the phase of forest fragmentation. Ultimately, climatic data obtained recently show that the present-day major rise in thunderstorms and lightning activity in Central Africa could result from some kind of solar influence, and hence the phase of forest fragmentation between ca. 2500 to 2000 cal yr BP may provide a model for the present-day global warming-related environmental changes in this region.

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Main Authors: Maley, Jean, Doumenge, Charles, Giresse, Pierre, Mahé, Gil, Philippon, Nathalie, Hubau, Wannes, Lokonda, Michel O., Tshibamba, Johm M., Chepstow-Lusty, Alex
Format: article biblioteca
Language:eng
Subjects:K01 - Foresterie - Considérations générales, F40 - Écologie végétale, B10 - Géographie, 000 - Autres thèmes, forêt tropicale humide, changement climatique, paléontologie, végétation, savane, histoire naturelle, évolution, couverture végétale, écologie, http://aims.fao.org/aos/agrovoc/c_7976, http://aims.fao.org/aos/agrovoc/c_1666, http://aims.fao.org/aos/agrovoc/c_5509, http://aims.fao.org/aos/agrovoc/c_8176, http://aims.fao.org/aos/agrovoc/c_6825, http://aims.fao.org/aos/agrovoc/c_5088, http://aims.fao.org/aos/agrovoc/c_2745, http://aims.fao.org/aos/agrovoc/c_25409, http://aims.fao.org/aos/agrovoc/c_2467, http://aims.fao.org/aos/agrovoc/c_1432,
Online Access:http://agritrop.cirad.fr/586909/
http://agritrop.cirad.fr/586909/1/Doumenge_C.pdf
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spelling dig-cirad-fr-5869092024-01-29T00:48:12Z http://agritrop.cirad.fr/586909/ http://agritrop.cirad.fr/586909/ Late Holocene forest contraction and fragmentation in central Africa. Maley Jean, Doumenge Charles, Giresse Pierre, Mahé Gil, Philippon Nathalie, Hubau Wannes, Lokonda Michel O., Tshibamba Johm M., Chepstow-Lusty Alex. 2018. Quaternary Research, 89 (1), n.spéc. Tribute to Daniel Livingstone and Paul Colinvaux : 43-59.https://doi.org/10.1017/qua.2017.97 <https://doi.org/10.1017/qua.2017.97> Late Holocene forest contraction and fragmentation in central Africa Maley, Jean Doumenge, Charles Giresse, Pierre Mahé, Gil Philippon, Nathalie Hubau, Wannes Lokonda, Michel O. Tshibamba, Johm M. Chepstow-Lusty, Alex eng 2018 Quaternary Research K01 - Foresterie - Considérations générales F40 - Écologie végétale B10 - Géographie 000 - Autres thèmes forêt tropicale humide changement climatique paléontologie végétation savane histoire naturelle évolution couverture végétale écologie http://aims.fao.org/aos/agrovoc/c_7976 http://aims.fao.org/aos/agrovoc/c_1666 http://aims.fao.org/aos/agrovoc/c_5509 http://aims.fao.org/aos/agrovoc/c_8176 http://aims.fao.org/aos/agrovoc/c_6825 http://aims.fao.org/aos/agrovoc/c_5088 http://aims.fao.org/aos/agrovoc/c_2745 http://aims.fao.org/aos/agrovoc/c_25409 http://aims.fao.org/aos/agrovoc/c_2467 Afrique centrale http://aims.fao.org/aos/agrovoc/c_1432 During the warmer Holocene Period, two major climatic crises affected the Central African rainforests. The first crisis, around 4000 cal yr BP, caused the contraction of the forest in favor of savanna expansion at its northern and southern periphery. The second crisis, around 2500 cal yr BP, resulted in major perturbation at the forest core, leading to forest disturbance and fragmentation with a rapid expansion of pioneer-type vegetation, and a marked erosional phase. The major driver of these two climatic crises appears to be rapid sea-surface temperature variations in the equatorial eastern Atlantic, which modified the regional atmospheric circulation. The change between ca. 2500 to 2000 cal yr BP led to a large increase in thunderstorm activity, which explains the phase of forest fragmentation. Ultimately, climatic data obtained recently show that the present-day major rise in thunderstorms and lightning activity in Central Africa could result from some kind of solar influence, and hence the phase of forest fragmentation between ca. 2500 to 2000 cal yr BP may provide a model for the present-day global warming-related environmental changes in this region. article info:eu-repo/semantics/article Journal Article info:eu-repo/semantics/publishedVersion http://agritrop.cirad.fr/586909/1/Doumenge_C.pdf text Cirad license info:eu-repo/semantics/restrictedAccess https://agritrop.cirad.fr/mention_legale.html https://doi.org/10.1017/qua.2017.97 10.1017/qua.2017.97 info:eu-repo/semantics/altIdentifier/doi/10.1017/qua.2017.97 info:eu-repo/semantics/altIdentifier/purl/https://doi.org/10.1017/qua.2017.97
institution CIRAD FR
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-cirad-fr
tag biblioteca
region Europa del Oeste
libraryname Biblioteca del CIRAD Francia
language eng
topic K01 - Foresterie - Considérations générales
F40 - Écologie végétale
B10 - Géographie
000 - Autres thèmes
forêt tropicale humide
changement climatique
paléontologie
végétation
savane
histoire naturelle
évolution
couverture végétale
écologie
http://aims.fao.org/aos/agrovoc/c_7976
http://aims.fao.org/aos/agrovoc/c_1666
http://aims.fao.org/aos/agrovoc/c_5509
http://aims.fao.org/aos/agrovoc/c_8176
http://aims.fao.org/aos/agrovoc/c_6825
http://aims.fao.org/aos/agrovoc/c_5088
http://aims.fao.org/aos/agrovoc/c_2745
http://aims.fao.org/aos/agrovoc/c_25409
http://aims.fao.org/aos/agrovoc/c_2467
http://aims.fao.org/aos/agrovoc/c_1432
K01 - Foresterie - Considérations générales
F40 - Écologie végétale
B10 - Géographie
000 - Autres thèmes
forêt tropicale humide
changement climatique
paléontologie
végétation
savane
histoire naturelle
évolution
couverture végétale
écologie
http://aims.fao.org/aos/agrovoc/c_7976
http://aims.fao.org/aos/agrovoc/c_1666
http://aims.fao.org/aos/agrovoc/c_5509
http://aims.fao.org/aos/agrovoc/c_8176
http://aims.fao.org/aos/agrovoc/c_6825
http://aims.fao.org/aos/agrovoc/c_5088
http://aims.fao.org/aos/agrovoc/c_2745
http://aims.fao.org/aos/agrovoc/c_25409
http://aims.fao.org/aos/agrovoc/c_2467
http://aims.fao.org/aos/agrovoc/c_1432
spellingShingle K01 - Foresterie - Considérations générales
F40 - Écologie végétale
B10 - Géographie
000 - Autres thèmes
forêt tropicale humide
changement climatique
paléontologie
végétation
savane
histoire naturelle
évolution
couverture végétale
écologie
http://aims.fao.org/aos/agrovoc/c_7976
http://aims.fao.org/aos/agrovoc/c_1666
http://aims.fao.org/aos/agrovoc/c_5509
http://aims.fao.org/aos/agrovoc/c_8176
http://aims.fao.org/aos/agrovoc/c_6825
http://aims.fao.org/aos/agrovoc/c_5088
http://aims.fao.org/aos/agrovoc/c_2745
http://aims.fao.org/aos/agrovoc/c_25409
http://aims.fao.org/aos/agrovoc/c_2467
http://aims.fao.org/aos/agrovoc/c_1432
K01 - Foresterie - Considérations générales
F40 - Écologie végétale
B10 - Géographie
000 - Autres thèmes
forêt tropicale humide
changement climatique
paléontologie
végétation
savane
histoire naturelle
évolution
couverture végétale
écologie
http://aims.fao.org/aos/agrovoc/c_7976
http://aims.fao.org/aos/agrovoc/c_1666
http://aims.fao.org/aos/agrovoc/c_5509
http://aims.fao.org/aos/agrovoc/c_8176
http://aims.fao.org/aos/agrovoc/c_6825
http://aims.fao.org/aos/agrovoc/c_5088
http://aims.fao.org/aos/agrovoc/c_2745
http://aims.fao.org/aos/agrovoc/c_25409
http://aims.fao.org/aos/agrovoc/c_2467
http://aims.fao.org/aos/agrovoc/c_1432
Maley, Jean
Doumenge, Charles
Giresse, Pierre
Mahé, Gil
Philippon, Nathalie
Hubau, Wannes
Lokonda, Michel O.
Tshibamba, Johm M.
Chepstow-Lusty, Alex
Late Holocene forest contraction and fragmentation in central Africa
description During the warmer Holocene Period, two major climatic crises affected the Central African rainforests. The first crisis, around 4000 cal yr BP, caused the contraction of the forest in favor of savanna expansion at its northern and southern periphery. The second crisis, around 2500 cal yr BP, resulted in major perturbation at the forest core, leading to forest disturbance and fragmentation with a rapid expansion of pioneer-type vegetation, and a marked erosional phase. The major driver of these two climatic crises appears to be rapid sea-surface temperature variations in the equatorial eastern Atlantic, which modified the regional atmospheric circulation. The change between ca. 2500 to 2000 cal yr BP led to a large increase in thunderstorm activity, which explains the phase of forest fragmentation. Ultimately, climatic data obtained recently show that the present-day major rise in thunderstorms and lightning activity in Central Africa could result from some kind of solar influence, and hence the phase of forest fragmentation between ca. 2500 to 2000 cal yr BP may provide a model for the present-day global warming-related environmental changes in this region.
format article
topic_facet K01 - Foresterie - Considérations générales
F40 - Écologie végétale
B10 - Géographie
000 - Autres thèmes
forêt tropicale humide
changement climatique
paléontologie
végétation
savane
histoire naturelle
évolution
couverture végétale
écologie
http://aims.fao.org/aos/agrovoc/c_7976
http://aims.fao.org/aos/agrovoc/c_1666
http://aims.fao.org/aos/agrovoc/c_5509
http://aims.fao.org/aos/agrovoc/c_8176
http://aims.fao.org/aos/agrovoc/c_6825
http://aims.fao.org/aos/agrovoc/c_5088
http://aims.fao.org/aos/agrovoc/c_2745
http://aims.fao.org/aos/agrovoc/c_25409
http://aims.fao.org/aos/agrovoc/c_2467
http://aims.fao.org/aos/agrovoc/c_1432
author Maley, Jean
Doumenge, Charles
Giresse, Pierre
Mahé, Gil
Philippon, Nathalie
Hubau, Wannes
Lokonda, Michel O.
Tshibamba, Johm M.
Chepstow-Lusty, Alex
author_facet Maley, Jean
Doumenge, Charles
Giresse, Pierre
Mahé, Gil
Philippon, Nathalie
Hubau, Wannes
Lokonda, Michel O.
Tshibamba, Johm M.
Chepstow-Lusty, Alex
author_sort Maley, Jean
title Late Holocene forest contraction and fragmentation in central Africa
title_short Late Holocene forest contraction and fragmentation in central Africa
title_full Late Holocene forest contraction and fragmentation in central Africa
title_fullStr Late Holocene forest contraction and fragmentation in central Africa
title_full_unstemmed Late Holocene forest contraction and fragmentation in central Africa
title_sort late holocene forest contraction and fragmentation in central africa
url http://agritrop.cirad.fr/586909/
http://agritrop.cirad.fr/586909/1/Doumenge_C.pdf
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