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Displaying results 1 - 8 of 8Click/tap on any title to see full details of the record
2022. Holocene environmental change along the central Namib Desert escarpment derived from hyrax and owl dung. Review of Palaeobotany and Palynology 305 104746
2018. Pollen in fossil hyrax dung from Marine Isotope Stages 2 and 3 reveals past environments in Namibia. Quaternary International (464) 260-272
Website link:https://doi.org/10.1016/j.quaint.2017.06.054
2016. Evidence of vegetation change in Late Quaternary deposits of the Namib Desert and boundary region. Quaternary International 404 (B) 186
2015. The potential of palynology in fossil bat-dung from Arnhem Cave, Namibia. Transactions of the Royal Society of South Africa
70 (2) 109-115
Downloadable files:
| Attachment | Size |
|---|---|
| The potential of palynology in fossil bat-dung from Arnhem Cave.pdf | 456.26 KB |
2009. A record of rapid Holocene climate change preserved in hyrax middens from southwestern Africa. Geology 37 (8) 703-706
Website link:http://geology.gsapubs.org/content/37/8/703.abstract
2007. Late Holocene environmental change in the northwestern Namib Desert margin: New fossil pollen evidence from hyrax middens. Palaeogeography, Palaeoclimatology, Palaeoecology
249 (1 - 2) 1 - 17
Downloadable files:
| Attachment | Size |
|---|---|
| Late Holocene environmental change in the northwestern Namib Desert margin_Hyrax_2007.pdf | 1.28 MB |
2004. Fossil hyrax dung and evidence of Late Pleistocene and Holocene vegetation types in the Namib Desert. Journal of Quaternary Science 19 (8) 829-832
2003. Persistent millennial-scale climatic variability over the past 25,000 years in Southern Africa. Quaternary Science Reviews 22 (21 - 22) 2311 - 2326
Website link:http://hdl.handle.net/10204/1422