Late Holocene palaeoenvironmental reconstruction on a peat sequence from northeastern South Africa, using grass phytoliths as main proxy
Contemporary a geographical imbalance of where palaeoclimatological studies have been undertaken exists, where the majority of palaeodata is based on studies from the northernhemisphere. Multiproxy analysis was performed on a peat core from Lydenburg, north-eastern Mpumalanga, covering the last 1.60...
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Format: | Others |
Language: | English |
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Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK)
2013
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Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-91882 |