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Grain-size end-members of sediment core GeoB8323-2
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(Table S1) Al, Cr, and Ni element concentrations of sediment core GeoB20610-2
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(Table S1) Al, Cr, and Ni element concentrations of sediment core GeoB20616-1
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Alkenone analysis of sediment core GeoB8323-2
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Inorganic geochemical down-core data from discrete XRF measurements of sedime...
This record allows a high-resolution continental climatic reconstruction for the past ca. 100,000 yrs for the Delagoa Bight. Climate sensitive proxies, like the elemental... -
Pollen and spores of sites GeoB8331 and GeoB8323, Namaqualand Mudbelt, Holoce...
To better understand Holocene vegetation and hydrological changes in South Africa, we analyzed pollen and microcharcoal records of two marine sites GeoB8331 and GeoB8323 from... -
Radiocarbon dating, carbon and nitrogen content, sediment accumulation rate a...
A 30.5 m sediment core was recovered from the coastal lake Eilandvlei (EV13), which represents a unique high-resolution record of environmental change for southern Africa. For... -
Geochemical, mineralogical, stable isotope, geochronological and grain size d...
South African coastal lake sediments provide an excellent opportunity to investigate environmental changes such as sea level and climate variability during the Holocene period.... -
Age determination and distribution of Holocene foraminifera and ostracoda in ...
Distribution of Holocene Foraminifera and Ostracoda in a 30 m long core from Eilandvlei, a coastal lake in the Wilderness, South Africa, covering the last 8900 years. Supplement... -
Holocene ostracod distribution and salinity transfer function of sediment cor...
in preparation Supplement to: Meschner, Stephanie; Frenzel, Peter (in prep.): Late Holocene water balance changes in Groenvlei, a Southern Cape coastal lake in South Africa. -
Recent brackish water Ostracoda and Foraminifera 2013-2014, South Africa
Distribution data and accompanying environmental data for Ostracoda and Foraminifera from surface sediment samples from the Wilderness area and Knysna estuary in South Africa... -
n-Alkanes and compound-specific isotopes in the Orange River system
The summer rainfall zone (SRZ) in the South African interior experienced pronounced hydrological and vegetation changes during the Holocene inferred to be driven mainly by... -
Organic-walled dinoflagellate cyst analysis of sediment core GeoB8331-4 and f...
Atmospheric and oceanographic interactions between the Atlantic and Indian Oceans influence upwelling in the southern Benguela upwelling system. In order to obtain a better... -
Holocene investigations of sediments from Eilandvlei
This study investigates Holocene sediments from Eilandvlei, a coastal lake located within the Wilderness embayment at the southern Cape coast of South Africa. The evolution of... -
Element concentrations in surface sediment samples from the Delagoa Bight (so...
The discrimination of sediment provenance from specific source regions is a crucial prerequisite for the paleoclimatic interpretation of terrigenous sediment archives. The... -
Late Holocene alkenone-derived sea-surface temperature data and grain size en...
Southwest Africa is an important region for paleo-climatic studies, being influenced by both tropical and temperate climate systems and thus reflecting the interplay of variable... -
Raw X-ray fluorescence (XRF) scannings and radiocarbon age of sediment cores ...
Variations in the sediment input to the Namaqualand mudbelt during the Holocene are assessed using an integrative terrestrial to marine, source to sink approach. Geochemical and... -
Raw X-ray fluorescence (XRF) scannings of sediment coreGeoB8331-4
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Raw X-ray fluorescence (XRF) scannings of sediment core GeoB8323-2
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Linking catchment hydrology and ocean circulation in Late Holocene southernmo...
Due to the high sensitivity of southern Africa to climate change, a reliable understanding of its hydrological system is crucial. Recent studies of the regional climatic system...
