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• W2071297564 abstract "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 14 C yr BP for DUMU core revealed increased Montane forest indicative of relatively moist conditions. Periods 3000–2000 and 2000–1000 14 C yr BP, DUMU core demonstrated increased submontane and lowland forests. Period 1000–200 14 C yr BP, DUMU core signified increased coprophilous fungi while DRM and MBML cores signified fluctuating herbaceous pollen spectra (wet-dry episodes). Period 200 14 C 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." @default.
• W2071297564 created "2016-06-24" @default.
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• W2071297564 date "2014-05-29" @default.
• W2071297564 modified "2023-10-16" @default.
• W2071297564 title "Vegetation Response to Climate Change and Human Impacts in the Usambara Mountains" @default.
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• W2071297564 doi "https://doi.org/10.1155/2014/240510" @default.
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