TY - JOUR A1 - Wichura, Henry A1 - Bousquet, Romain A1 - Oberhänsli, Roland A1 - Strecker, Manfred A1 - Trauth, Martin H. T1 - Evidence for middleUocene uplift of the East African Plateau N2 - Cenozoic uplift of the East African Plateau has been associated with fundamental climatic and environmental changes in East Africa and adjacent regions. While this influence is widely accepted, the timing and the magnitude of plateau uplift have remained unclear. This uncertainty stems from the lack of datable, geomorphically meaningful reference horizons that could record surface uplift. Here, we document the existence of significant relief along the East African Plateau prior to rifting, as inferred from modeling the emplacement history of one of the longest terrestrial lava flows, the similar to 300-km-long Yatta phonolite flow in Kenya. This 13.5 Ma lava flow originated on the present-day eastern Kenya Rift flank, and utilized a riverbed that once routed runoff from the eastern rim of the plateau. Combining an empirical viscosity model with subsequent cooling and using the Yatta lava flow geometry and underlying paleotopography (slope angle), we found that the prerift slope was at least 0.2 degrees, suggesting that the lava flow originated at a minimum elevation of 1400 m. Hence, high paleotopography in the Kenya Rift region must have existed by at least 13.5 Ma. We infer from this that middle Miocene uplift occurred, which coincides with the two-step expansion of grasslands, as well as important radiation and speciation events in tropical Africa. Y1 - 2010 UR - http://geology.gsapubs.org/ U6 - https://doi.org/10.1130/G31022.1 SN - 0091-7613 ER - TY - JOUR A1 - Weinelt, Mara A1 - Kuhnt, Wolfgang A1 - Sarnthein-Lotichius, Johann Michael A1 - Altenbach, Alexander V. A1 - Costello, O. A1 - Erlenkeuser, Helmut A1 - Mathiessen, J. A1 - Pflaumann, Uwe A1 - Simstich, J. A1 - Struck, J. A1 - Thies, A. A1 - Trauth, Martin H. A1 - Vogelsang, E. T1 - Paleoceanographic proxies in the northern North Atlantic Y1 - 2001 SN - 3-540-67231-1 ER - TY - JOUR A1 - Walter, Marius J. A1 - Trauth, Martin H. T1 - A MATLAB based orientation analysis of Acheulean handaxe accumulations in Olorgesailie and Kariandusi, Kenya Rift JF - Journal of human evolution N2 - The Pleistocene archeological record in East Africa has revealed unusual accumulations of Acheulean handaxes at prehistoric sites. In particular, there has been intensive debate concerning whether the artifact accumulation at the Middle Pleistocene Olorgesailie (Southern Kenya Rift) and Kariandusi (Central Kenya Rift) sites were a result of fluvial reworking or of in situ deposition by hominids. We used a two-step approach to test the hypothesis of fluvial reworking. Firstly, the behavior of handaxes in water currents was investigated in a current flume and the flow threshold required to reorientate the handaxes was determined. The results of these experiments suggested that, in relatively high energy and non-steady flow conditions, handaxes will reorientate themselves perpendicular to the current direction. Secondly, an automated image analysis routine was developed and applied to archeological plans from three Acheulean sites, two at Olorgesailie and one at Kariandusi, in order to determine the orientations of the handaxes. A Rayleigh test was then applied to the orientation data to test for a preferred orientation. The results revealed that the handaxes at the Upper Kariandusi Site and the Olorgesailie Main Site Mid Trench had a preferential orientation, suggesting reworking by a paleocurrent. The handaxes from the Olorgesailie Main Site H/6A, however, appeared to be randomly oriented and in situ deposition by the producers therefore remains a possibility. KW - Excavation plan KW - Artifact KW - Flume channel KW - Shape detection KW - Rayleigh test Y1 - 2013 U6 - https://doi.org/10.1016/j.jhevol.2013.02.011 SN - 0047-2484 VL - 64 IS - 6 SP - 569 EP - 581 PB - Elsevier CY - London ER - TY - JOUR A1 - Tronicke, Jens A1 - Trauth, Martin H. T1 - Classroom-sized geophysical experiments BT - magnetic surveying using modern smartphone devices JF - European Journal of Physics N2 - Modern mobile devices (i.e. smartphones and tablet computers) are widespread, everyday tools, which are equipped with a variety of sensors including three-axis magnetometers. Here, we investigate the feasibility and the potential of using such mobile devices to mimic geophysical experiments in the classroom in a table-top setup. We focus on magnetic surveying and present a basic setup of a table-top experiment for collecting three-component magnetic data across well-defined source bodies and structures. Our results demonstrate that the quality of the recorded data is sufficient to address a number of important basic concepts in the magnetic method. The shown examples cover the analysis of magnetic data recorded across different kinds of dipole sources, thus illustrating the complexity of magnetic anomalies. In addition, we analyze the horizontal resolution capabilities using a pair of dipole sources placed at different horizontal distances to each other. Furthermore, we demonstrate that magnetic data recorded with a mobile device can even be used to introduce filtering, transformation, and inversion approaches as they are typically used when processing magnetic data sets recorded for real-world field applications. Thus, we conclude that such table-top experiments represent an easy-to-implement experimental procedure (as student exercise or classroom demonstration) and can provide first hands-on experience in the basic principles of magnetic surveying including the fundamentals of data acquisition, analysis and processing, as well as data evaluation and interpretation. KW - geophysics KW - magnetic surveying KW - table-top experiment Y1 - 2018 U6 - https://doi.org/10.1088/1361-6404/aaad5b SN - 0143-0807 SN - 1361-6404 VL - 39 IS - 3 PB - IOP Publ. Ltd. CY - Bristol ER - TY - JOUR A1 - Trauth, Martin H. A1 - Strecker, Manfred T1 - Formation of landslide-dammed lakes during a wet period between 40,000 - 25,000 yr B.P. in northwestern Argentina Y1 - 1999 ER - TY - JOUR A1 - Trauth, Martin H. A1 - Strecker, Manfred T1 - Late Pleistocene Lake-Level Fluctuations in the Naivasha Basin, Kenia Y1 - 1996 ER - TY - JOUR A1 - Trauth, Martin H. A1 - Sarnthein, Michael A1 - Arnold, Maurice T1 - Bioturbational mixing depth and carbon flux at the seafloor Y1 - 1997 ER - TY - JOUR A1 - Trauth, Martin H. A1 - Maslin, Mark A. A1 - Deino, Alan A1 - Strecker, Manfred T1 - Late Cenozoic Moisture History of East Africa N2 - Lake sediments in 10 Ethiopian, Kenyan, and Tanzanian rift basins suggest that there were three humid periods at 2.7 to 2.5 million years ago (Ma), 1.9 to 1.7 Ma, and 1.1 to 0.9 Ma, superimposed on the longer-term aridification of East Africa. These humid periods correlate with increased aridity in northwest and northeast Africa and with substantial global climate transitions. These episodes could have had important impacts on the speciation and dispersal of mammals and hominins, because a number of key events, such as the origin of the genus Homo and the evolution of the species Homo erectus, took place in this region during that time. Y1 - 2005 UR - http://dx.doi.org/10.1126/science.1112964 ER - TY - JOUR A1 - Trauth, Martin H. A1 - Maslin, Mark A. A1 - Deino, Alan L. A1 - Strecker, Manfred A1 - Bergner, Andreas G. N. A1 - Dühnforth, Miriam T1 - High- and low-latitude forcing of Plio-Pleistocene African climate and human evolution N2 - The late Cenozoic climate of East Africa is punctuated by episodes of short, alternating periods of extreme wetness and aridity, superimposed on a regime of subdued moisture availability exhibiting a long-term drying trend. These periods of extreme climate variability appear to correlate with maxima in the 400-thousand-year (kyr) component of the Earth's eccentricity cycle. Prior to 2.7 Ma the wet phases appear every 400 kyrs, whereas after 2.7 Ma, the wet phases appear every 800 kyrs, with periods of precessional-forced extreme climate variability at 2.7-2.5 Ma, 1.9-1.7 Ma, and 1.1-0.9 Ma before present. The last three major lake phases occur at the times of major global climatic transitions, such as the onset of Northern Hemisphere Glaciation (2.7-2.5 Ma), intensification of the Walker Circulation (1.9-1.7 Ma), and the Mid-Pleistocene Revolution (1.0-0.7 Ma). High-latitude forcing is required to compress the Intertropical Convergence Zone so that East Africa becomes locally sensitive to precessional forcing, resulting in rapid shifts from wet to dry conditions. These periods of extreme climate variability may have provided a catalyst for evolutionary change and driven key speciation and dispersal events amongst mammals and hominins in East Africa. (C) 2007 Elsevier Ltd. All rights reserved. Y1 - 2008 U6 - https://doi.org/10.1016/j.jhevol.2006.12.009 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 -