Vegetation response to the "African Humid Period" termination in Central Cameroon (7° N) – new pollen insight from Lake Mbalang

A new pollen sequence from the Lake Mbalang (7°19´ N, 13°44´ E, 1110 m a.s.l.) located on the eastern Adamawa plateau, in Central Cameroon, is presented in this paper to analyze the Holocene African Humid Period (AHP) termination and related vegetation changes at 7° N in tropical Africa, completing...

Full description

Bibliographic Details
Main Authors: M. Servant, ECOFIT Mbalang collaborators, A. Vincens, G. Buchet
Format: Article
Language:English
Published: Copernicus Publications 2010-05-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/6/281/2010/cp-6-281-2010.pdf
_version_ 1811312814650818560
author M. Servant
ECOFIT Mbalang collaborators
A. Vincens
G. Buchet
author_facet M. Servant
ECOFIT Mbalang collaborators
A. Vincens
G. Buchet
author_sort M. Servant
collection DOAJ
description A new pollen sequence from the Lake Mbalang (7°19´ N, 13°44´ E, 1110 m a.s.l.) located on the eastern Adamawa plateau, in Central Cameroon, is presented in this paper to analyze the Holocene African Humid Period (AHP) termination and related vegetation changes at 7° N in tropical Africa, completing an important transect for exploring shifts in the northern margin of the African Monsoon. This sequence, spanning the last 7000 cal yr BP, shows that the vegetation response to this transitional climatic period was marked by significant successional changes within the broad context of long-term aridification. Semi-deciduous/sub-montane forest retreat in this area is initially registered as early as ca. 6100 cal yr BP and modern savannah was definitely established at ca. 3000 cal yr BP and stabilized at ca. 2400 cal yr BP; but a slight forest regeneration episode is observed between ca. 5200 and ca. 4200 cal yr BP. In this area with modern high rainfall, increasing in the length of the dry season during the AHP termination linked to a contraction of the northern margin of the Intertropical Convergence Zone (ITCZ) from ca. 6100 cal yr BP onward, probably associated with decreasing in cloud cover and/or fog frequency, has primarily controlled vegetation dynamics and above all the disappearance of the forested environment on the Adamawa plateau. Compared to previous studies undertaken in northern tropical and Central Africa, this work clearly shows that the response of vegetation to transitional periods between climatic extremes such as the AHP termination might be different in timing, mode and amplitude according to the regional climate of the study sites, but also according to the stability of vegetation before and during these climatic transitions.
first_indexed 2024-04-13T10:43:15Z
format Article
id doaj.art-164b0c73b4884a10bd3a2aec61914f58
institution Directory Open Access Journal
issn 1814-9324
1814-9332
language English
last_indexed 2024-04-13T10:43:15Z
publishDate 2010-05-01
publisher Copernicus Publications
record_format Article
series Climate of the Past
spelling doaj.art-164b0c73b4884a10bd3a2aec61914f582022-12-22T02:49:52ZengCopernicus PublicationsClimate of the Past1814-93241814-93322010-05-016328129410.5194/cp-6-281-2010Vegetation response to the "African Humid Period" termination in Central Cameroon (7° N) – new pollen insight from Lake MbalangM. ServantECOFIT Mbalang collaboratorsA. VincensG. BuchetA new pollen sequence from the Lake Mbalang (7°19´ N, 13°44´ E, 1110 m a.s.l.) located on the eastern Adamawa plateau, in Central Cameroon, is presented in this paper to analyze the Holocene African Humid Period (AHP) termination and related vegetation changes at 7° N in tropical Africa, completing an important transect for exploring shifts in the northern margin of the African Monsoon. This sequence, spanning the last 7000 cal yr BP, shows that the vegetation response to this transitional climatic period was marked by significant successional changes within the broad context of long-term aridification. Semi-deciduous/sub-montane forest retreat in this area is initially registered as early as ca. 6100 cal yr BP and modern savannah was definitely established at ca. 3000 cal yr BP and stabilized at ca. 2400 cal yr BP; but a slight forest regeneration episode is observed between ca. 5200 and ca. 4200 cal yr BP. In this area with modern high rainfall, increasing in the length of the dry season during the AHP termination linked to a contraction of the northern margin of the Intertropical Convergence Zone (ITCZ) from ca. 6100 cal yr BP onward, probably associated with decreasing in cloud cover and/or fog frequency, has primarily controlled vegetation dynamics and above all the disappearance of the forested environment on the Adamawa plateau. Compared to previous studies undertaken in northern tropical and Central Africa, this work clearly shows that the response of vegetation to transitional periods between climatic extremes such as the AHP termination might be different in timing, mode and amplitude according to the regional climate of the study sites, but also according to the stability of vegetation before and during these climatic transitions.http://www.clim-past.net/6/281/2010/cp-6-281-2010.pdf
spellingShingle M. Servant
ECOFIT Mbalang collaborators
A. Vincens
G. Buchet
Vegetation response to the "African Humid Period" termination in Central Cameroon (7° N) – new pollen insight from Lake Mbalang
Climate of the Past
title Vegetation response to the "African Humid Period" termination in Central Cameroon (7° N) – new pollen insight from Lake Mbalang
title_full Vegetation response to the "African Humid Period" termination in Central Cameroon (7° N) – new pollen insight from Lake Mbalang
title_fullStr Vegetation response to the "African Humid Period" termination in Central Cameroon (7° N) – new pollen insight from Lake Mbalang
title_full_unstemmed Vegetation response to the "African Humid Period" termination in Central Cameroon (7° N) – new pollen insight from Lake Mbalang
title_short Vegetation response to the "African Humid Period" termination in Central Cameroon (7° N) – new pollen insight from Lake Mbalang
title_sort vegetation response to the african humid period termination in central cameroon 7° n new pollen insight from lake mbalang
url http://www.clim-past.net/6/281/2010/cp-6-281-2010.pdf
work_keys_str_mv AT mservant vegetationresponsetotheafricanhumidperiodterminationincentralcameroon7nnewpolleninsightfromlakembalang
AT ecofitmbalangcollaborators vegetationresponsetotheafricanhumidperiodterminationincentralcameroon7nnewpolleninsightfromlakembalang
AT avincens vegetationresponsetotheafricanhumidperiodterminationincentralcameroon7nnewpolleninsightfromlakembalang
AT gbuchet vegetationresponsetotheafricanhumidperiodterminationincentralcameroon7nnewpolleninsightfromlakembalang