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Vegetation response to climate change and human impacts in the Usambara Mountains
York Institute for Ecosystem, UK.
York Institute for Ecosystem, UK.
Department of Archaeology, University of York, King's Manor, York, UK.ORCID iD: 0000-0002-9936-1310
2014 (English)In: ISRN Forestry, ISSN 2090-892X, 240510Article in journal (Other academic) Published
Abstract [en]

The East and West Usambara Mountain blocks are unique based on three characteristics. Firstly, they are connected blocks; secondly, they have an oceanic-influenced climate; and thirdly, the rain seasons are not easily discernible due to their close proximity to the Indian Ocean and Equator. Sediment cores were collected from peat bogs in Derema (DRM) and Mbomole (MBML) in East Usambara and from Madumu (DUMU) in West Usambara. The multiproxy record provides an understanding on climate and vegetation changes during the last 5000 years. DRM and MBML cores result in radiocarbon ages and age-depth curve which showed hiatus at 20 cm and 61 cm and huge inversion for DUMU core at 57 cm. Period 5000–4000 14C yr BP for DUMU core revealed increased Montane forest indicative of relatively moist conditions. Periods 3000–2000 and 2000–1000 14C yr BP, DUMU core demonstrated increased submontane and lowland forests. Period 1000–200 14C yr BP, DUMU core signified increased coprophilous fungi while DRM and MBML cores signified fluctuating herbaceous pollen spectra (wet-dry episodes). Period 200 14C yr BP to present, all cores demonstrated stable recovery of forest types especially dominance of submontane forests. Abundant coprophilous fungi indicated increased human impacts including forest fires, cultivation, and grazing.

Place, publisher, year, edition, pages
International Scholarly Research Notices , 2014. 240510
Keyword [en]
Climate change; Historical ecology; Palaeoecology; Usambara Mountains
National Category
Environmental Sciences
Research subject
Earth Science with specialization in Environmental Analysis; Archaeology
URN: urn:nbn:se:uu:diva-270395DOI: 10.1155/2014/240510OAI: diva2:889713
Available from: 2015-12-28 Created: 2015-12-28 Last updated: 2016-01-12Bibliographically approved

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