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Late Holocene forest contraction and fragmentation in central Africa

Quaternary research, 2018-01, Vol.89 (1), p.43-59

2018

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Middle to Late Holocene Paleoclimatic Change and the Early Bantu Expansion in the Rain Forests of Western Central Africa

Current anthropology, 2015-06, Vol.56 (3), p.354-384

2015

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Populations and Climatic Evolution in North Tropical Africa from the End of the Neolithic to the Dawn of the Modern Era

The African archaeological review, 2015-06, Vol.32 (2), p.179-232

2015

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Seasonality change and the third millennium BP rainforest crisis in southern Cameroon (Central Africa)

Quaternary research, 2009-05, Vol.71 (3), p.307-318

2009

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Millennial-scale changes in vegetation records from tropical Africa and South America during the last glacial

Quaternary science reviews, 2010-10, Vol.29 (21), p.2882-2899

2010

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Understanding the 2500 yr BP rainforest crisis in West and Central Africa in the framework of the Late Holocene: Pluridisciplinary analysis and multi-archive reconstruction

Global and planetary change, 2020-09, Vol.192, p.103257, Article 103257

2020

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A Catastrophic Destruction of African Forests about 2,500 Years Ago Still Exerts a Major Influence on Present Vegetation Formations

IDS bulletin (Brighton. 1984), 2002-01, Vol.33 (1), p.13-30

Maley, Jean

2002

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Vegetation dynamics, palaeoenvironments and climatic changes in the forests of western Cameroon during the last 28,000 years B.P

Review of palaeobotany and palynology, 1998, Vol.99 (2), p.157-187

1998

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A focus on the last 1000 years of natural environmental changes in the tropical rainforests of West and Central Africa. Can we detect anthropogenic disturbances?

Global and planetary change, 2023-01, Vol.220, p.103995, Article 103995

2023

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Comment on "Intensifying weathering and land use in Iron Age Central Africa"

Science (American Association for the Advancement of Science), 2012-08, Vol.337 (6098), p.1040; author reply 1040-1040

2012

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Evidence of pollen transport by the Sanaga River on the Cameroon shelf

Comptes Rendus. Géoscience, 2020-01, Vol.352 (1), p.59-72

2020

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Pollen, vegetation change and climate at Lake Barombi Mbo (Cameroon) during the last ca. 33 000 cal yr BP: a numerical approach

Climate of the past, 2012-01, Vol.8 (1), p.59-78

2012

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Comment on “Intensifying Weathering and Land Use in Iron Age Central Africa”

Science (American Association for the Advancement of Science), 2012-08

2012

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African Palaeoclimate and Human Response: A Special Issue of the African Archaeological Review

The African archaeological review, 2015-07, Vol.32 (2), p.167-177

2015

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Comment on “Geochronological arguments for a close relationship between surficial formation profiles and environmental crisis (c. 3000–2000 BP) in Gabon (Central Africa)”, by D. Thiéblemont et al., 2013 [C.R. Geoscience 345, 272–283]

Comptes rendus. Geoscience, 2014-07, Vol.346 (7-8), p.200-202

2014

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INTRODUCTION: African Palaeoclimate and Human Response: A Special Issue of the "African Archaeological Review"

The African archaeological review, 2015-06, Vol.32 (2), p.167-177

2015

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Peuples et évolution climatique en Afrique nord-tropicale, de la fin du Néolithique à l’aube de l’époque moderne

Afriques, 2013-06 (4)

2013

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African palaeoclimate and human response [dossier]

The African archaeological review, 2015, Vol.32 (2), p.167-367

2015

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Vegetation changes during the past 1300 years in western equatorial Africa: a highresolution pollen record from Lake Kamalete, Lope Reserve, Central Gabon

Holocene (Sevenoaks), 2016-07, Vol.15 (7), p.1021-1031

2016

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Lake Chad sedimentation and environments during the late Miocene and Pliocene: New evidence from mineralogy and chemistry of the Bol core sediments

Journal of African earth sciences (1994), 2016-06, Vol.118, p.192-204

2016

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Late-Holocene equatorial environments inferred from deposition processes, carbon isotopes of organic matter, and pollen in three shallow lakes of Gabon, west-central Africa

Journal of paleolimnology, 2009-02, Vol.41 (2), p.369-392

2009

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Corrigendum to “Diatom, phytolith, and pollen records from a 10Be/9Be dated lacustrine succession in the Chad basin: Insight on the Miocene–Pliocene paleoenvironmental changes in Central Africa” [PALAEO: 430 (2015) 85–103]

Palaeogeography, palaeoclimatology, palaeoecology, 2016-01, Vol.442, p.128-128

2016

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Climatic instability in west equatorial Africa during the Mid- and Late Holocene

Quaternary international, 2006-06, Vol.150 (1), p.71-81

2006

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Last Glacial Maximum lacustrine and fluviatile Formations in the Tibesti and other Saharan mountains, and large-scale climatic teleconnections linked to the activity of the Subtropical Jet Stream

Global and planetary change, 2000-11, Vol.26 (1), p.121-136

Maley, Jean

2000

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Reconstruction of Megalake Chad using Shuttle Radar Topographic Mission data

Palaeogeography, palaeoclimatology, palaeoecology, 2006-09, Vol.239 (1), p.16-27

2006

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Late Holocene forest contraction and fragmentation in central Africa

Middle to Late Holocene Paleoclimatic Change and the Early Bantu Expansion in the Rain Forests of Western Central Africa

Populations and Climatic Evolution in North Tropical Africa from the End of the Neolithic to the Dawn of the Modern Era

Seasonality change and the third millennium BP rainforest crisis in southern Cameroon (Central Africa)

Millennial-scale changes in vegetation records from tropical Africa and South America during the last glacial

Understanding the 2500 yr BP rainforest crisis in West and Central Africa in the framework of the Late Holocene: Pluridisciplinary analysis and multi-archive reconstruction

A Catastrophic Destruction of African Forests about 2,500 Years Ago Still Exerts a Major Influence on Present Vegetation Formations

Vegetation dynamics, palaeoenvironments and climatic changes in the forests of western Cameroon during the last 28,000 years B.P

A focus on the last 1000 years of natural environmental changes in the tropical rainforests of West and Central Africa. Can we detect anthropogenic disturbances?

Comment on "Intensifying weathering and land use in Iron Age Central Africa"

Evidence of pollen transport by the Sanaga River on the Cameroon shelf

Pollen, vegetation change and climate at Lake Barombi Mbo (Cameroon) during the last ca. 33 000 cal yr BP: a numerical approach

Comment on “Intensifying Weathering and Land Use in Iron Age Central Africa”

African Palaeoclimate and Human Response: A Special Issue of the African Archaeological Review

Comment on “Geochronological arguments for a close relationship between surficial formation profiles and environmental crisis (c. 3000–2000 BP) in Gabon (Central Africa)”, by D. Thiéblemont et al., 2013 [C.R. Geoscience 345, 272–283]

INTRODUCTION: African Palaeoclimate and Human Response: A Special Issue of the "African Archaeological Review"

Peuples et évolution climatique en Afrique nord-tropicale, de la fin du Néolithique à l’aube de l’époque moderne

African palaeoclimate and human response [dossier]

Vegetation changes during the past 1300 years in western equatorial Africa: a highresolution pollen record from Lake Kamalete, Lope Reserve, Central Gabon

Lake Chad sedimentation and environments during the late Miocene and Pliocene: New evidence from mineralogy and chemistry of the Bol core sediments

Late-Holocene equatorial environments inferred from deposition processes, carbon isotopes of organic matter, and pollen in three shallow lakes of Gabon, west-central Africa

Corrigendum to “Diatom, phytolith, and pollen records from a 10Be/9Be dated lacustrine succession in the Chad basin: Insight on the Miocene–Pliocene paleoenvironmental changes in Central Africa” [PALAEO: 430 (2015) 85–103]

Climatic instability in west equatorial Africa during the Mid- and Late Holocene

Last Glacial Maximum lacustrine and fluviatile Formations in the Tibesti and other Saharan mountains, and large-scale climatic teleconnections linked to the activity of the Subtropical Jet Stream

Reconstruction of Megalake Chad using Shuttle Radar Topographic Mission data

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