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...

Full description

Bibliographic Details
Main Author: Sjöström, Jenny
Format: Others
Language:English
Published: Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK) 2013
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-91882
id ndltd-UPSALLA1-oai-DiVA.org-su-91882
record_format oai_dc
spelling ndltd-UPSALLA1-oai-DiVA.org-su-918822018-01-12T05:11:30ZLate Holocene palaeoenvironmental reconstruction on a peat sequence from northeastern South Africa, using grass phytoliths as main proxyengSjöström, JennyStockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK)2013Late HoloceneSouth AfricaPalaeoenvironmental reconstructionPhytolithBokoniPhysical GeographyNaturgeografiContemporary 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 1.600 years. Proxy focus was put on fossil grassphytoliths. A general drying trend can be noted from AD 400 to 1000, followed by moremesic conditions around AD 1200. The increasingly mesic conditions were interrupted by asignificantly drier period between c. AD 1250 to 1350. This part of the Lydenburg sequenceoccurs in the end of a climate event termed “Medieval warm period” (MWP), suggested tohave been warmer and variable but mostly wetter in southern Africa. The results are in lineregarding the increased temperature and suggested variability. However, in contrast withearlier findings, significantly drier conditions seem to have prevailed at the Lydenburg fenat the end of “MWP” as interpreted by multiple proxies. Following AD 1400 increasinglymesic conditions was recorded as interpreted by several of the analysed proxies. Morepalaeoenvironmental studies needs to be performed in the area in order to elaborate on thedriving factors of palaeoenvironmental change in the region, as well as to establish if thesignals from the Lydenburg fen record local or regional changes. The results support earlierphytolith studies suggesting that small rondels should be excluded from phytolithassemblages in tropical and sub-tropical areas in Africa. People, Land, and Time in Africa (PLATINA)Bokoni project. This MA thesis is part of a transdisciplinary project involving scholars from Sweden and South Africa aiming to understand traces of pre-colonial terraces found in north-easter Mpumalanga, South Africa.Student thesisinfo:eu-repo/semantics/bachelorThesistexthttp://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-91882application/pdfinfo:eu-repo/semantics/openAccess
collection NDLTD
language English
format Others
sources NDLTD
topic Late Holocene
South Africa
Palaeoenvironmental reconstruction
Phytolith
Bokoni
Physical Geography
Naturgeografi
spellingShingle Late Holocene
South Africa
Palaeoenvironmental reconstruction
Phytolith
Bokoni
Physical Geography
Naturgeografi
Sjöström, Jenny
Late Holocene palaeoenvironmental reconstruction on a peat sequence from northeastern South Africa, using grass phytoliths as main proxy
description 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 1.600 years. Proxy focus was put on fossil grassphytoliths. A general drying trend can be noted from AD 400 to 1000, followed by moremesic conditions around AD 1200. The increasingly mesic conditions were interrupted by asignificantly drier period between c. AD 1250 to 1350. This part of the Lydenburg sequenceoccurs in the end of a climate event termed “Medieval warm period” (MWP), suggested tohave been warmer and variable but mostly wetter in southern Africa. The results are in lineregarding the increased temperature and suggested variability. However, in contrast withearlier findings, significantly drier conditions seem to have prevailed at the Lydenburg fenat the end of “MWP” as interpreted by multiple proxies. Following AD 1400 increasinglymesic conditions was recorded as interpreted by several of the analysed proxies. Morepalaeoenvironmental studies needs to be performed in the area in order to elaborate on thedriving factors of palaeoenvironmental change in the region, as well as to establish if thesignals from the Lydenburg fen record local or regional changes. The results support earlierphytolith studies suggesting that small rondels should be excluded from phytolithassemblages in tropical and sub-tropical areas in Africa. === People, Land, and Time in Africa (PLATINA) === Bokoni project. This MA thesis is part of a transdisciplinary project involving scholars from Sweden and South Africa aiming to understand traces of pre-colonial terraces found in north-easter Mpumalanga, South Africa.
author Sjöström, Jenny
author_facet Sjöström, Jenny
author_sort Sjöström, Jenny
title Late Holocene palaeoenvironmental reconstruction on a peat sequence from northeastern South Africa, using grass phytoliths as main proxy
title_short Late Holocene palaeoenvironmental reconstruction on a peat sequence from northeastern South Africa, using grass phytoliths as main proxy
title_full Late Holocene palaeoenvironmental reconstruction on a peat sequence from northeastern South Africa, using grass phytoliths as main proxy
title_fullStr Late Holocene palaeoenvironmental reconstruction on a peat sequence from northeastern South Africa, using grass phytoliths as main proxy
title_full_unstemmed Late Holocene palaeoenvironmental reconstruction on a peat sequence from northeastern South Africa, using grass phytoliths as main proxy
title_sort late holocene palaeoenvironmental reconstruction on a peat sequence from northeastern south africa, using grass phytoliths as main proxy
publisher Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK)
publishDate 2013
url http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-91882
work_keys_str_mv AT sjostromjenny lateholocenepalaeoenvironmentalreconstructiononapeatsequencefromnortheasternsouthafricausinggrassphytolithsasmainproxy
_version_ 1718606099275317248