about
A synthesis of the theories and concepts of early human evolutionNonlinear detection of paleoclimate-variability transitions possibly related to human evolutionMolecular profiling of diatom assemblages in tropical lake sediments using taxon-specific PCR and Denaturing High-Performance Liquid Chromatography (PCR-DHPLC).Hidden diversity in diatoms of Kenyan Lake Naivasha: a genetic approach detects temporal variation.High- and low-latitude forcing of Plio-Pleistocene East African climate and human evolution.A MATLAB based orientation analysis of Acheulean handaxe accumulations in Olorgesailie and Kariandusi, Kenya Rift.Late Cenozoic moisture history of East Africa.Episodes of environmental stability versus instability in Late Cenozoic lake records of Eastern Africa.Tephrochronologic Constraints on Temporal Distribution of Large Landslides in Northwest Argentina.Human evolution in a variable environment: the amplifier lakes of Eastern AfricaThe effects of solar irradiation changes on the migration of the Congo Air Boundary and water levels of paleo-Lake Suguta, Northern Kenya Rift, during the African Humid Period (15–5ka BP)Climate change and mass movements in the NW Argentine AndesModelling vegetation change during Late Cenozoic uplift of the East African plateausMultiple landslide clusters record Quaternary climate changes in the northwestern Argentine AndesHydrological modelling of a Pleistocene landslide-dammed lake in the Santa Maria Basin, NW ArgentinaEvidence for middle Miocene uplift of the East African PlateauThree and half million year history of moisture availability of South West Africa: Evidence from ODP site 1085 biomarker recordsClimatic change recorded in the sediments of the Chew Bahir basin, southern Ethiopia, during the last 45,000 yearsEnvironmental variability in Lake Naivasha, Kenya, over the last two centuriesThe sensitivity of East African rift lakes to climate fluctuationsReply to the comment on “Environmental change and human occupation of southern Ethiopia and northern Kenya during the last 20,000 years. Quaternary Science Reviews 129: 333–340”Environmental change and human occupation of southern Ethiopia and northern Kenya during the last 20,000 yearsMATLAB® Recipes for Earth SciencesSemi-automated detection of annual laminae (varves) in lake sediments using a fuzzy logic algorithmA new probabilistic technique to build an age model for complex stratigraphic sequencesEast African climate pulses and early human evolutionHydrological constraints of paleo-Lake Suguta in the Northern Kenya Rift during the African Humid Period (15–5kaBP)Mapping changing shorelines in the Malombe and Chiuta lakes of Malawi—environmental effects of recent climatic variationsTURBO2: A MATLAB simulation to study the effects of bioturbation on paleoceanographic time seriesRemotely-sensed evapotranspiration estimates for an improved hydrological modeling of the early Holocene mega-lake Suguta, northern Kenya RiftThe Mid-Miocene East African Plateau: a pre-rift topographic model inferred from the emplacement of the phonolitic Yatta lava flow, KenyaImage ProcessingStatistics on Directional DataHistorical genetics on a sediment core from a Kenyan lake: intraspecific genotype turnover in a tropical rotifer is related to past environmental changesMATLAB® Recipes for Earth SciencesComment on “Diatomaceous sediments and environmental change in the Pleistocene Olorgesailie Formation, southern Kenya Rift” by R.B. Owen, R. Potts, A.K. Behrensmeyer and P. Ditchfield [Palaeogeography, Palaeoclimatology, Palaeoecology 269 (2008)Late Pleistocene–Holocene rise and collapse of Lake Suguta, northern Kenya RiftTrends, rhythms and events in Plio-Pleistocene African climateMATLAB® Recipes for Earth SciencesEarly Holocene water budget of the Nakuru-Elmenteita basin, Central Kenya Rift
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Martin H. Trauth
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Martin H. Trauth
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