Twentieth century changes in montane vegetation in the eastern Free State,South Africa, derived from palynology of hyrax dung middens

Citation
Js. Carrion et al., Twentieth century changes in montane vegetation in the eastern Free State,South Africa, derived from palynology of hyrax dung middens, J QUAT SCI, 14(1), 1999, pp. 1-16
Citations number
52
Categorie Soggetti
Earth Sciences
Journal title
JOURNAL OF QUATERNARY SCIENCE
ISSN journal
02678179 → ACNP
Volume
14
Issue
1
Year of publication
1999
Pages
1 - 16
Database
ISI
SICI code
0267-8179(199902)14:1<1:TCCIMV>2.0.ZU;2-M
Abstract
The dating and pollen analysis of a hyrax dung deposit in a mountain rock s helter (Rooiberg Shelter II) are compared with that in a previous study fro m the same mountain range at the rural town Clarens, in South Africa. Calib ration of radiocarbon measurements from the dung deposit provides different possibilities for the age of the sequence. Unlikely dates can be eliminate d on the basis of pollen stratigraphy, comparisons with a previously studie d accumulation from the last 30 yr, artificially increased radiocarbon leve ls in the upper samples as result of nuclear arms testing after 1954, the p resence of historically introduced exotic elements, and the assumption of a relatively constant rate of dung accumulation. According to these consider ations we suggest that the dung started accumulating at the beginning of th e twentieth century. The pollen contents show marked changes in composition , indicating mainly open grass vegetation with fynbos in the first half of this century and woody vegetation in the second half. A first marked increa se of the woody component is estimated to have occurred around 1950, but it only became permanent in the 1960s. The fluctuating pollen sequence can be st be interpreted in terms of the combined effects of rainfall changes, fir e and stock grazing, the latter of which increased together with town expan sion in the area during the course of this century. Considering historical events recorded in the area and the region in general, the results suggest that pollen in hyrax dung is a good recorder of vegetation change. Copyrigh t (C) 1999 John Wiley & Sons, Ltd.