4 results
DMP XV: Palaeohydrology and Palaeoenvironment: Initial Results and Report of 2010 and 2011 Fieldwork
- Nicholas Drake, Mustapha Salem, Simon Armitage, Jan Francke, Mark Hounslow, Osama Hlal, Kevin White, Ahmed El-Hawat
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- Journal:
- Libyan Studies / Volume 42 / 2011
- Published online by Cambridge University Press:
- 24 April 2014, pp. 139-149
- Print publication:
- 2011
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This paper reports the results of fieldwork conducted in the 2010 and 2011 DMP field seasons and of analysis of samples collected during these and previous years. Research has involved 1) studying palaeolake sediment outcrops, 2) using ground penetrating radar (GPR) to determine their extent under the Dahān Ubārī, and 3) coring palaeolakes in order to determine their palaeoenvironmental records. Research on these samples is continuing but some initial findings are discussed in this paper. The most extensive palaeolake sediments are found within the al-Mahruqah Formation and were deposited by a giant lake system that developed in the Fazzān Basin during past humid periods. Stratigraphic analysis of Lake Megafazzān sediments suggests two different sedimentary successions, a lake margin succession distinctive for its lacustrine and palaeosol carbonates, and a clastic-dominated, intensely rootleted, basin-centre succession which has terrestrial intervals (aeolian and palaeosols) as well as in the upper parts lacustrine limestones. Both basin margin and basin centre successions are underlain by fluvial deposits. Magnetostratigraphy suggests that the formation may be as old as the mid-Pliocene. After the Lake Megafazzān phase, smaller palaeolakes developed within the basin during subsequent humid periods. One of the largest is found in the Wādī al-Hayāt in the area between Jarma and Ubārī. Similar deposits further west along the Wādī at progressively higher altitudes are interpreted as small lakes and marshes fed by springs issuing from aquifers at the base of the escarpment, last replenished during the Holocene humid phase. Dating of sediments suggests that this was between c. 11 and c. 8 ka. The Wādī ash-Shāţī palaeolake core also provides a Holocene palaeoclimate record that paints a slightly different picture, indicating lake conditions until around 7 ka, whereupon it started oscillating until around 5.5 ka when sedimentation terminates. The reasons for the differences in these records are discussed.
DMP VIII: Palaeohydrology and palaeoenvironment
- Nicholas Drake, Kevin White, Mustapha Salem, Simon Armitage, Ahmed El-Hawat, Jan Francke, Mark Hounslow, Adrian Parker
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- Journal:
- Libyan Studies / Volume 40 / 2009
- Published online by Cambridge University Press:
- 03 March 2015, pp. 171-178
- Print publication:
- 2009
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The January 2009 fieldwork season conducted geomorphological and palaeoenviromental surveys in as yet unexplored parts of the Lake Megafazzan Basin, as well as continuing research in the Wadi al-Hayat and Ubari Sand Sea. Lake Megafazzan sediments were investigated at two sites on the eastern margin of the basin. At the first site, east of Tamessah, 24 m of stratigraphy was investigated and found to consist of a lacustrine carbonate unit at the base progressing into a fluvial unit and then an upper carbonate unit. The sediments were sampled for magnetostratigraphy and cosmogenic nucleide dating in order to determine their age. Similar studies were undertaken in the vicinity of the Arial Agricultural Project, where 31 m of section were logged and sampled. Here the sediments were quite different, being composed of a deltaic sequence consisting of stacked channels and palaeosols, thought to represent the outflow delta of the palaeolake. Many new Holocene lake sediment deposits were discovered and sampled in the Wadi al-Hayat and the Ubari Sand Sea, including a 5 m section through Jarma Playa that appears to record the last arid-humid cycle. Lake Gabr 'Awn and the moat round Old Jarma were cored in order to gather a detailed picture of recent palaeoenvironmental change. Finally, we implemented a pilot geophysical survey to test the ability of state-of-the-art Ground Penetrating Radar (UltraGPR) technology for detecting and mapping buried palaeolake sediments under the dunes of the Ubari Sand Sea. The UltraGPR was found to be very effective, detecting palaeolake sediments as much as 60 m beneath the surface. Preliminary results suggest such sediments underlie much of the region.
DMP III: Pleistocene and Holocene palaeonvironments and prehistoric occupation of Fazzan, Libyan Sahara
- Marta Mirazón Lahr, Robert Foley, Simon Armitage, Huw Barton, Federica Crivellaro, Nicholas Drake, Mark Hounslow, Lisa Maher, David Mattingly, Mustapha Salem, Jay Stock, Kevin White
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- Journal:
- Libyan Studies / Volume 39 / 2008
- Published online by Cambridge University Press:
- 03 March 2015, pp. 263-294
- Print publication:
- 2008
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The palaeoanthropological and geomorphological sub-projects of the Desert Migrations Project (DMP) focus on the Pleistocene and early Holocene environment and prehistory of Fazzan so as to assess the timing and extent of hominin and human movement across the Sahara through time. This paper reports on the findings of the 2008 field season, with a focus on the prehistoric evidence along the northern margin of the Ubari sand sea.
The geomorphological record of the area preserves evidence of at least five past episodes of lake formation. The exact chronology of these, as well as the spatial extent of these lakes, remains the focus of further study.
The archaeological record of hominin and human occupation of Fazzan prior to the establishment of the Garamantian civilisation is extraordinarily rich. Between 2007 and 2008, the DMP palaeoanthropological project surveyed thirty-five localities along the northern margin of the Ubari sand sea, recording a range of assemblages spanning all Palaeolithic industries. Most of the archaeological remains found consisted of stone-tools, while grinding stones were comparatively restricted geographically. Mode 1/Oldowan tools were found at two localities, contrasting with the widespread presence of Mode 2/Acheulean, Mode 3/Middle Stone Age and Mode 5/microlithic artefacts. This indicates that, although hominin presence in the area is probably earlier than previously thought, populations were comparatively sparse until the Middle Pleistocene. Twenty-one localities within the Ubari sand sea, as well as seven south of the Messak Settafet were also surveyed between 2007 and 2008. The detailed study of the lithics from these areas will be carried out next year, but preliminary results stress the different nature of the assemblages found within interdune corridors — very low frequency of cores, no Mode 1 and extremely rare Mode 2 lithics (found at a single locality).
The 2009 field season will focus on obtaining further samples of palaeolake sediments for dating, on the evidence of Mode 1 assemblages south of the Messak, as well as on the refining of the archaeological indicators that may distinguish the different phases of hominin and human occupation of Fazzan during the Later Pleistocene and Holocene.
Desert Migrations: people, environment and culture in the Libyan Sahara
- David Mattingly, Marta Lahr, Simon Armitage, Huw Barton, John Dore, Nick Drake, Robert Foley, Stefania Merlo, Mustapha Salem, Jay Stock, Kevin White, Muftah Ahmed, Franca Cole, Federica Crivellaro, Mireya Gonzalez Rodriguez, Maria Guagnin, Sebastian Jones, Vassil Karloukovski, Victoria Leitch, Lisa Maher, Farès Moussa, Anita Radini, Ian Reeds, Toby Savage, Martin Sterry
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- Journal:
- Libyan Studies / Volume 38 / 2007
- Published online by Cambridge University Press:
- 03 March 2015, pp. 115-156
- Print publication:
- 2007
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The Desert Migrations Project is a new interdisciplinary and multi-dimensional collaborative project between the Society for Libyan Studies and the Department of Antiquities. The geographical focus of the study is the Fazzan region of southwest Libya and in thematic terms we aim to address the theme of migration in the broadest sense, encompassing the movement of people, ideas/knowledge and material culture into and out of Fazzan, along with evidence of shifting climatic and ecological boundaries over time. The report describes the principal sub-strands of the project's first season in January 2007, with some account of research questions, methods employed and some preliminary results. Three main sub-projects are reported on. The first concerns the improved understanding of long-term climatic and environmental changes derived from a detailed palaeoenvironmental study of palaeolake sediments. This geo-science work runs alongside and feeds directly into both archaeological sub-projects, the first relating to prehistoric activity and mobility around and between a series of palaeolakes during wetter climatic cycles; the second to the excavation of burials in the Wadi al-Ajal, exploring the changing relationship between material culture, identity and ethnicity across time, from prehistory to the early Islamic period (the span of the main cemetery zones). In addition, some rock art research and a survey of historic period sites was undertaken in the Wadi ash-Shati and Ubari sand sea.