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Omo-Turkana Basin

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Journal Article
Published: 01 March 2012
Journal of the Geological Society (2012) 169 (2): 213–226.
...Ian McDougall; Francis H. Brown; Paulo M. Vasconcelos; Benjamin E. Cohen; David S. Thiede; Michael J. Buchanan Abstract Six tuffaceous beds within the Omo Group of the OmoTurkana Basin have been dated using the 40 Ar/ 39 Ar single crystal total fusion method on anorthoclase, yielding eruption ages...
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Journal Article
Published: 01 March 2008
Journal of the Geological Society (2008) 165 (2): 549–562.
...IAN McDOUGALL; FRANCIS H. BROWN Abstract The OmoTurkana Basin of northern Kenya and southern Ethiopia developed in the northern Kenya Rift about 4.3 Ma ago in the Early Pliocene. Nearly 800 m of sediments, included within the Omo Group, crop out in the basin. Numerous rhyolitic tuffs...
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Distribution and thickness of Omo Group sediments in the Omo–Turkana Basin from interpretation of seismic data and from measured stratigraphic thicknesses. Principal areas of outcrop of the Shungura, Nachukui and Koobi Fora formations are shown with diagonal shading. Inset shows the location of the map area in NE Africa.
Published: 01 March 2012
Fig. 1. Distribution and thickness of Omo Group sediments in the OmoTurkana Basin from interpretation of seismic data and from measured stratigraphic thicknesses. Principal areas of outcrop of the Shungura, Nachukui and Koobi Fora formations are shown with diagonal shading. Inset shows
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The temporal distribution of tuffaceous beds within the Omo–Turkana Basin with number of tuffs plotted in 0.1 Ma intervals. Data from Konso are separate and plotted in front of the Omo–Turkana data; totals are not cumulative; there is overlap between them because some, but not all, tuffs at Konso have been correlated with tuffs in the Omo–Turkana Basin.
Published: 01 March 2012
Fig. 6. The temporal distribution of tuffaceous beds within the OmoTurkana Basin with number of tuffs plotted in 0.1 Ma intervals. Data from Konso are separate and plotted in front of the OmoTurkana data; totals are not cumulative; there is overlap between them because some, but not all, tuffs
Journal Article
Published: 01 January 2006
Journal of the Geological Society (2006) 163 (1): 185–204.
... of tuffs that is derived is consistent with 40 Ar/ 39 Ar ages reported separately, and provides the stratigraphic framework for interpreting those ages. Further, new correlations are established to the Konso Formation in southern Ethiopia. As drainage from the Ethiopian Rift to the OmoTurkana Basin...
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Journal Article
Published: 01 January 2006
Journal of the Geological Society (2006) 163 (1): 205–220.
...Ian McDougall; Francis H. Brown Abstract The Plio-Pleistocene Koobi Fora Formation, about 560 m thick, crops out east of Lake Turkana and is part of the much larger depositional system of the OmoTurkana Basin. The upper half of the Koobi Fora Formation from just below the KBS Tuff to above...
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 Map of part of northern Kenya and southern Ethiopia showing the extent of the Omo–Turkana Basin, including areas of outcrop of some of the named formations. Localities referred to in the text are identified. Inset shows the location of the map in NE Africa. Insets on the main map labelled a, b, c refer to more detailed maps in the Supplementary Publication (see p. 3), which show detailed sample locations.
Published: 01 March 2008
Fig. 1.  Map of part of northern Kenya and southern Ethiopia showing the extent of the OmoTurkana Basin, including areas of outcrop of some of the named formations. Localities referred to in the text are identified. Inset shows the location of the map in NE Africa. Insets on the main map
Image
Composite stratigraphic sections of the main formations in the Omo–Turkana Basin, together with the results of 40Ar/39Ar dating of mainly alkali feldspars from pumice clasts within tuffs (McDougall & Brown 2006, 2008; this study). Ages determined here are shown in bold and in a larger size. The main tuffaceous beds are shown in black, often named, and correlations between the stratigraphic columns are shown by grey lines. The Shungura Formation composite section is after de Heinzelin (1983), the Koobi Fora Formation is mainly from Brown & Feibel (1986), noting a significant hiatus, and that for the Nachukui Formation is derived from Harris et al. (1988) with minor modification. The sequence at Kanapoi, to the east of Loperot, is after Leakey et al. (1998) and Feibel (2003), and the sequence at Kibish to the north of Lake Turkana is after Brown & Fuller (2007). To the left of the stratigraphic columns for the Koobi Fora and Shungura formations are the measured magnetic polarities, where grey shading represents normal polarity and unshaded indicates reversed polarity. Data are from Hillhouse et al. (1986) and Lepre & Kent (2010) for the Koobi Fora Formation and after Brown et al. (1978) and Kidane et al. (2007) for the Shungura Formation. The ages shown for the polarity boundaries are from Gradstein et al. (2004).
Published: 01 March 2012
Fig. 3. Composite stratigraphic sections of the main formations in the OmoTurkana Basin, together with the results of 40 Ar/ 39 Ar dating of mainly alkali feldspars from pumice clasts within tuffs ( McDougall & Brown 2006 , 2008 ; this study). Ages determined here are shown in bold
Journal Article
Published: 19 September 2008
Geological Magazine (2009) 146 (1): 34–47.
... in a northeasterly direction. About 4.3 Ma ago, in the Pliocene, the OmoTurkana Basin formed in the northern part of the Kenya Rift in relatively low country between the Kenya and Ethiopia domes, where the sediments of the Omo Group accumulated. The domes are often regarded as related to underlying mantle plumes...
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Journal Article
Published: 01 January 2004
Geological Magazine (2004) 141 (1): 41–53.
...BEREKET HAILEAB; FRANCIS H. BROWN; IAN McDOUGALL; PATRICK N. GATHOGO Abstract A little before 4 Ma ago, deposition of Pliocene and Pleistocene strata described as the Omo Group began in the Turkana and Omo basins of northern Kenya and southern Ethiopia. Soon after, basaltic magma erupted as thin...
FIGURES
Journal Article
Journal: Elements
Published: 01 April 2023
Elements (2023) 19 (2): 75–81.
... our ancestors’ paleobiology. In eastern Africa, the Ngorongoro Volcanic Highlands, Omo-Turkana Basin, and Awash Valley contain many paleontological sites that have produced a comprehensive fossil record of human origins and exhibited the geologic setting of the last six million years. Allia Bay...
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Journal Article
Journal: GSA Bulletin
Published: 01 February 2000
GSA Bulletin (2000) 112 (2): 163–176.
..., 1994 ) ( Figs. 3 and 4 ). The seismically and volcanically active Turkana-Omo rift is to the east of the Lotikipi-Kibish rift, and it branches northward into the North Omo and Usno basins ( Figs. 3 and 4 ). Geological Society of America 2000 Phonolite flows from eruptive centers...
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Locations in Africa with fossils assigned to the genus Australopithecus (1–10; Behrensmeyer and Reed 2013), sites where quantitative paleoclimate data for the Miocene–Pliocene were sourced (A–G, 5 and 7), and the Chiwondo beds of the Karonga Basin in northern Malawi (G) (Lüdecke et al. 2016). 1, Koro Toro (Chad); 2, Northern Awash Basin (Ethiopia); 3, Middle Awash Basin (Ethiopia); 4, Fejej (Ethiopia); 5, Turkana Basin (Omo, Koobi Foora, West Turkana, Kanapoi, and Allia Bay; Kenya); 6, Lothagam (Kenya); 7, Laetoli (Tanzania); 8, Makapansgat (South Africa); 9, Sterkfontein, Gladysvale, and Malapa (South Africa); 10, Taung (South Africa). A, Greater Awash (Ethiopia); B, Baringo Basin (Kenya); C, Kenya Rift (Kenya); D, Nyanza Rift (Kenya); E, Rukwa Rift Basin (Tanzania); F, Langebaanweg (South Africa); 5,Turkana (Kenya); 7, Laetoli (Tanzania). Please refer to supplemental data for complete data set and references. Digital elevation model of Africa modified from the NASA Shuttle Radar Topography Mission Collection.
Published: 16 June 2023
. 2016 ). 1, Koro Toro (Chad); 2, Northern Awash Basin (Ethiopia); 3, Middle Awash Basin (Ethiopia); 4, Fejej (Ethiopia); 5, Turkana Basin (Omo, Koobi Foora, West Turkana, Kanapoi, and Allia Bay; Kenya); 6, Lothagam (Kenya); 7, Laetoli (Tanzania); 8, Makapansgat (South Africa); 9, Sterkfontein
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Figure 8. True-scale cross sections (A) F–F′ across the Chew Bahir basin and (B) G–G′ across the Omo basin (Fig. 4). Numbers above figure refer to dated samples (Tables 1 and 2). Data from beneath Lake Turkana are from Dunkelman et al. (1989), and depth estimates are from gravity interpretations (Ebinger and Ibrahim, 1994).
Published: 01 February 2000
Figure 8. True-scale cross sections (A) F–F′ across the Chew Bahir basin and (B) G–G′ across the Omo basin (Fig. 4) . Numbers above figure refer to dated samples ( Tables 1 and 2 ). Data from beneath Lake Turkana are from Dunkelman et al. (1989) , and depth estimates are from gravity
Journal Article
Published: 15 June 2023
Journal of the Geological Society (2023) 180 (4): jgs2022-171.
.... 2006 ). A number of Turkana Basin tuffs contain pumice clasts that host feldspar (typically anorthoclase) crystals, which are the primary target for 40 Ar/ 39 Ar geochronology. Ages are available for c. 40 Omo Group tuffs, ranging from 4.23 ± 0.01 (2 σ ) Ma (unnamed tuff, Apak Member...
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Journal Article
Journal: Elements
Published: 01 April 2023
Elements (2023) 19 (2): 82–87.
... sequences that enable the evaluation of climatic influences on hominin evolution ( F ig . 3 ). During the Plio–Pleistocene, magmatism and faulting migrated eastward to the basins of the Omo-Turkana Rift, the current locus of subsidence and magmatism. A phase of magmatism and faulting at 3–2 Ma along...
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Journal Article
Published: 01 January 2013
Journal of Paleontology (2013) 87 (1): 84–90.
... it existed primarily as a fluvially-dominated rift basin. During relatively short time intervals, rift lakes formed in the basin, including the most recent, modern Lake Turkana, which is fed primarily by the Omo River draining from the Ethiopian Highlands to the south. The Omo River is hypothesized...
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Journal Article
Published: 16 June 2023
Journal of Sedimentary Research (2023) 93 (5): 309–326.
.... 2016 ). 1, Koro Toro (Chad); 2, Northern Awash Basin (Ethiopia); 3, Middle Awash Basin (Ethiopia); 4, Fejej (Ethiopia); 5, Turkana Basin (Omo, Koobi Foora, West Turkana, Kanapoi, and Allia Bay; Kenya); 6, Lothagam (Kenya); 7, Laetoli (Tanzania); 8, Makapansgat (South Africa); 9, Sterkfontein...
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Journal Article
Journal: PALAIOS
Published: 01 July 2008
PALAIOS (2008) 23 (7): 452–464.
... Kenya:Los Angeles County Natural History Musuem Contributions in Science , 498 . 9 – 20 . Feibel , C.S. , Brown , F.H. , and McDougall , I. , 1989 , Stratigraphic context of fossil hominids from the Omo Group deposits, Northern Turkana Basin, Kenya and Ethiopia : American Journal...
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Figure 3. Neogene environmental changes in Kenya compared with cooling histories of rift flanks and late Cenozoic geologic history. A: Abundance of taxa indicative of grassland ecosystems in lower Omo sequence (northern Turkana Basin) after Bobe and Behrensmeyer (2004). Black lines indicate occurrence of Australopithecus, Paranthropus, and Homo in Turkana Basin. B: Stable carbon isotope compositions of paleosoil carbonates from East Africa fossil localities after Cerling (1992), reflecting dominant type of vegetation. Gray shaded areas show isotopic ranges characteristic for pure C3 vegetation (mainly trees and shrubs) and for pure C4 vegetation (predominantly tropical grasses). C: Cooling histories of rift flanks, as deduced from AHe data from Ndoto Mountains (dark gray) and Cherangani Hills (white). D: Time line for main geological events associated with development of southern Kenya rift system (after Smith, 1994; Pickford, 1994).
Published: 01 May 2007
Figure 3. Neogene environmental changes in Kenya compared with cooling histories of rift flanks and late Cenozoic geologic history. A: Abundance of taxa indicative of grassland ecosystems in lower Omo sequence (northern Turkana Basin) after Bobe and Behrensmeyer (2004) . Black lines indicate