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Atmospheric controls on precipitation isotopes and hydroclimate in high-elevation regions in Eastern Africa since the Last Glacial Maximum
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- Journal Article
- A1
- open access
Anthropogenic alteration of nutrient supply increases the global freshwater carbon sink
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Tracing ancient animal husbandry in tropical Africa using the fossil spore assemblages of coprophilous fungi : a validation study in western Uganda
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- Journal Article
- A1
- open access
Reconstructing East African monsoon variability from grain-size distributions : end-member modeling and source attribution of diatom-rich sediments from Lake Chala
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Water‐isotope ecohydrology of Mount Kilimanjaro
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- Journal Article
- A1
- open access
History of scoria-cone eruptions on the eastern shoulder of the Kenya-Tanzania Rift revealed in the 250-ka sediment record of Lake Chala near Mount Kilimanjaro
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- Journal Article
- A1
- open access
Seasonal variability and sources of in situ brGDGT production in a permanently stratified African crater lake
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Species integrity and origin of Oreochromis hunteri (Pisces: Cichlidae), endemic to crater Lake Chala (Kenya-Tanzania)
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Distinct phases of natural landscape dynamics and intensifying human activity in the central Kenya Rift Valley during the past 1300 years
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Late-Holocene sedimentation and sodium carbonate deposition in hypersaline, alkaline Nasikie Engida, southern Kenya Rift Valley
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Baseline assessment of benthic macroinvertebrate community structure and ecological water quality in Rwenzori rivers (Albertine rift valley, Uganda) using biotic-index tools
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Phytoplankton communities in the crater lakes of western Uganda, and their indicator species in relation to lake trophic status
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Determining patterns of stratification and mixing in tropical crater lakes through intermittent water-column profiling : a case study in western Uganda
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Influence of plant growth form, habitat and season on leaf-wax n-alkane hydrogen-isotopic signatures in equatorial East Africa
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Ecohydrological evolution of Lake Naivasha (central Rift Valley, Kenya) during the past 1650 years, as recorded by ostracod assemblages and stable-isotope geochemistry