TY - JOUR A1 - Foerster, Verena A1 - Asrat, Asfawossen A1 - Ramsey, Christopher Bronk A1 - Brown, Erik T. A1 - Chapot, Melissa S. A1 - Deino, Alan A1 - Düsing, Walter A1 - Grove, Matthew A1 - Hahn, Annette A1 - Junginger, Annett A1 - Kaboth-Bahr, Stefanie A1 - Lane, Christine S. A1 - Opitz, Stephan A1 - Noren, Anders A1 - Roberts, Helen M. A1 - Stockhecke, Mona A1 - Tiedemann, Ralph A1 - Vidal, Celine M. A1 - Vogelsang, Ralf A1 - Cohen, Andrew S. A1 - Lamb, Henry F. A1 - Schaebitz, Frank A1 - Trauth, Martin H. T1 - Pleistocene climate variability in eastern Africa influenced hominin evolution JF - Nature geoscience N2 - Despite more than half a century of hominin fossil discoveries in eastern Africa, the regional environmental context of hominin evolution and dispersal is not well established due to the lack of continuous palaeoenvironmental records from one of the proven habitats of early human populations, particularly for the Pleistocene epoch. Here we present a 620,000-year environmental record from Chew Bahir, southern Ethiopia, which is proximal to key fossil sites. Our record documents the potential influence of different episodes of climatic variability on hominin biological and cultural transformation. The appearance of high anatomical diversity in hominin groups coincides with long-lasting and relatively stable humid conditions from similar to 620,000 to 275,000 years bp (episodes 1-6), interrupted by several abrupt and extreme hydroclimate perturbations. A pattern of pronounced climatic cyclicity transformed habitats during episodes 7-9 (similar to 275,000-60,000 years bp), a crucial phase encompassing the gradual transition from Acheulean to Middle Stone Age technologies, the emergence of Homo sapiens in eastern Africa and key human social and cultural innovations. Those accumulative innovations plus the alignment of humid pulses between northeastern Africa and the eastern Mediterranean during high-frequency climate oscillations of episodes 10-12 (similar to 60,000-10,000 years bp) could have facilitated the global dispersal of H. sapiens. KW - Evolutionary ecology KW - Limnology KW - Palaeoclimate Y1 - 2022 U6 - https://doi.org/10.1038/s41561-022-01032-y SN - 1752-0894 SN - 1752-0908 VL - 15 IS - 10 SP - 805 EP - 811 PB - Nature Publ. Group CY - London ER - TY - JOUR A1 - Trauth, Martin H. A1 - Maslin, Mark A. A1 - Deino, Alan L. A1 - Junginger, Annett A1 - Lesoloyia, Moses A1 - Odada, Eric O. A1 - Olago, Daniel O. A1 - Olaka, Lydia A. A1 - Strecker, Manfred A1 - Tiedemann, Ralph T1 - Human evolution in a variable environment : the amplifier lakes of Eastern Africa N2 - The development of rise Cenozoic East African Rift System (EARS) profoundly re-shaped the landscape and significantly increased the amplitude of short-term environmental response to climate variation. In particular, the development of amplifier lakes in rift basins after three million years ago significantly contributed to this exceptional sensitivity of East Africa to climate change compared to elsewhere on the African continent. Amplifier lakes are characterized by tectonically-formed graben morphologies in combination with an extreme contrast between high precipitation in the elevated parts of the catchment and high evaporation in the lake area. Such amplifier lakes respond rapidly to moderate, precessional-forced climate shifts, and as they do so apply dramatic environmental pressure to the biosphere. Rift basins, when either extremely dry or lake-filled, form important barriers for migration, mixing and competition of different populations of animals and hominins. Amplifier lakes link long-term, high-amplitude tectonic processes and short-term environmental fluctuations. East Africa may have become the place where early humans evolved as a consequence of this strong link between different time scales. (C) 2010 Elsevier Ltd. All rights reserved. Y1 - 2010 UR - http://www.sciencedirect.com/science/journal/02773791 U6 - https://doi.org/10.1016/j.quascirev.2010.07.007 SN - 0277-3791 ER - TY - JOUR A1 - Stoof-Leichsenring, Kathleen Rosemarie A1 - Junginger, Annett A1 - Olaka, Lydia A. A1 - Tiedemann, Ralph A1 - Trauth, Martin H. T1 - Environmental variability in Lake Naivasha, Kenya, over the last two centuries JF - Journal of paleolimnolog N2 - Lake Naivasha, Kenya, is one of a number of freshwater lakes in the East African Rift System. Since the beginning of the twentieth century, it has experienced greater anthropogenic influence as a result of increasingly intensive farming of coffee, tea, flowers, and other horticultural crops within its catchment. The water-level history of Lake Naivasha over the past 200 years was derived from a combination of instrumental records and sediment data. In this study, we analysed diatoms in a lake sediment core to infer past lacustrine conductivity and total phosphorus concentrations. We also measured total nitrogen and carbon concentrations in the sediments. Core chronology was established by (210)Pb dating and covered a similar to 186-year history of natural (climatic) and human-induced environmental changes. Three stratigraphic zones in the core were identified using diatom assemblages. There was a change from littoral/epiphytic diatoms such as Gomphonema gracile and Cymbella muelleri, which occurred during a prolonged dry period from ca. 1820 to 1896 AD, through a transition period, to the present planktonic Aulacoseira sp. that favors nutrient-rich waters. This marked change in the diatom assemblage was caused by climate change, and later a strong anthropogenic overprint on the lake system. Increases in sediment accumulation rates since 1928, from 0.01 to 0.08 g cm(-2) year(-1) correlate with an increase in diatom-inferred total phosphorus concentrations since the beginning of the twentieth century. The increase in phosphorus accumulation suggests increasing eutrophication of freshwater Lake Naivasha. This study identified two major periods in the lake's history: (1) the period from 1820 to 1950 AD, during which the lake was affected mainly by natural climate variations, and (2) the period since 1950, during which the effects of anthropogenic activity overprinted those of natural climate variation. KW - Lake sediments KW - Diatoms KW - Conductivity KW - Lake Naivasha KW - Human impact KW - Eutrophication Y1 - 2011 U6 - https://doi.org/10.1007/s10933-011-9502-4 SN - 0921-2728 VL - 45 IS - 3 SP - 353 EP - 367 PB - Springer CY - Dordrecht ER -