Late Pleistocene and Holocene Afromontane vegetation and headwater wetland dynamics within the Eastern Mau Forest, Kenya
(2021) In Journal of Quaternary Science 36(2). p.239-254- Abstract
The Mau Forest Complex is Kenya's largest fragment of Afromontane forest, providing critical ecosystem services, and has been subject to intense land use changes since colonial times. It forms the upper catchment of rivers that drain into major drainage networks, thus supporting the livelihoods of millions of Kenyans and providing important wildlife areas. We present the results of a sedimentological and palynological analysis of a Late Pleistocene–Holocene sediment record of Afromontane forest change from Nyabuiyabui wetland in the Eastern Mau Forest, a highland region that has received limited geological characterization and palaeoecological study. Sedimentology, pollen, charcoal, X-ray fluorescence and radiocarbon data record... (More)
The Mau Forest Complex is Kenya's largest fragment of Afromontane forest, providing critical ecosystem services, and has been subject to intense land use changes since colonial times. It forms the upper catchment of rivers that drain into major drainage networks, thus supporting the livelihoods of millions of Kenyans and providing important wildlife areas. We present the results of a sedimentological and palynological analysis of a Late Pleistocene–Holocene sediment record of Afromontane forest change from Nyabuiyabui wetland in the Eastern Mau Forest, a highland region that has received limited geological characterization and palaeoecological study. Sedimentology, pollen, charcoal, X-ray fluorescence and radiocarbon data record environmental and ecosystem change over the last ~16 000 cal a bp. The pollen record suggests Afromontane forests characterized the end of the Late Pleistocene to the Holocene with dominant taxa changing from Apodytes, Celtis, Dracaena, Hagenia and Podocarpus to Cordia, Croton, Ficus, Juniperus and Olea. The Late Holocene is characterized by a more open Afromontane forest with increased grass and herbaceous cover. Continuous Poaceae, Cyperaceae and Juncaceae vegetation currently cover the wetland and the water level has been decreasing over the recent past. Intensive agroforestry since the 1920s has reduced Afromontane forest cover as introduced taxa have increased (Pinus, Cupressus and Eucalyptus).
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- author
- Githumbi, Esther N. LU ; Courtney Mustaphi, Colin J. and Marchant, Rob
- organization
- publishing date
- 2021-01-11
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- afromontane vegetation, Mau Forest, pollen, tropical wetlands, water towers
- in
- Journal of Quaternary Science
- volume
- 36
- issue
- 2
- pages
- 239 - 254
- publisher
- John Wiley & Sons Inc.
- external identifiers
-
- scopus:85099309283
- ISSN
- 0267-8179
- DOI
- 10.1002/jqs.3267
- language
- English
- LU publication?
- yes
- id
- 8a8f432f-7cc1-4ecb-804e-fa168fbac15b
- date added to LUP
- 2021-01-25 12:05:15
- date last changed
- 2022-04-26 23:56:03
@article{8a8f432f-7cc1-4ecb-804e-fa168fbac15b,
abstract = {{<p>The Mau Forest Complex is Kenya's largest fragment of Afromontane forest, providing critical ecosystem services, and has been subject to intense land use changes since colonial times. It forms the upper catchment of rivers that drain into major drainage networks, thus supporting the livelihoods of millions of Kenyans and providing important wildlife areas. We present the results of a sedimentological and palynological analysis of a Late Pleistocene–Holocene sediment record of Afromontane forest change from Nyabuiyabui wetland in the Eastern Mau Forest, a highland region that has received limited geological characterization and palaeoecological study. Sedimentology, pollen, charcoal, X-ray fluorescence and radiocarbon data record environmental and ecosystem change over the last ~16 000 cal a bp. The pollen record suggests Afromontane forests characterized the end of the Late Pleistocene to the Holocene with dominant taxa changing from Apodytes, Celtis, Dracaena, Hagenia and Podocarpus to Cordia, Croton, Ficus, Juniperus and Olea. The Late Holocene is characterized by a more open Afromontane forest with increased grass and herbaceous cover. Continuous Poaceae, Cyperaceae and Juncaceae vegetation currently cover the wetland and the water level has been decreasing over the recent past. Intensive agroforestry since the 1920s has reduced Afromontane forest cover as introduced taxa have increased (Pinus, Cupressus and Eucalyptus).</p>}},
author = {{Githumbi, Esther N. and Courtney Mustaphi, Colin J. and Marchant, Rob}},
issn = {{0267-8179}},
keywords = {{afromontane vegetation; Mau Forest; pollen; tropical wetlands; water towers}},
language = {{eng}},
month = {{01}},
number = {{2}},
pages = {{239--254}},
publisher = {{John Wiley & Sons Inc.}},
series = {{Journal of Quaternary Science}},
title = {{Late Pleistocene and Holocene Afromontane vegetation and headwater wetland dynamics within the Eastern Mau Forest, Kenya}},
url = {{http://dx.doi.org/10.1002/jqs.3267}},
doi = {{10.1002/jqs.3267}},
volume = {{36}},
year = {{2021}},
}