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Nachukui Formation

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Stratigraphic columns at localities where Gombe Group basalts have been identified, showing that they are confined to the lowest part of the Pliocene sections (see also Watkins, 1986). The Lonyumun Member of the Koobi Fora and Nachukui formations lies below the Moiti Tuff. Parenthetic numbers following column titles refer to the location numbers on Figure 1. Notes: a – Shungura Formation column after de Heinzelin (1983); b – Koobi Fora Formation column after Brown & Feibel (1991); c – Nachukui Formation column after Harris, Brown & Leakey (1988); d – Lothagam section after McDougall & Feibel (1999).
Published: 01 January 2004
Figure 2. Stratigraphic columns at localities where Gombe Group basalts have been identified, showing that they are confined to the lowest part of the Pliocene sections (see also Watkins, 1986 ). The Lonyumun Member of the Koobi Fora and Nachukui formations lies below the Moiti Tuff
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 Map of the lower Omo Valley of Ethiopia and the northern part of Lake Turkana in Kenya showing the Koobi Fora, Nachukui, and Shungura Formations as light stipple. Numbered points east of the lake refer to palaeontological collection areas. Section names are given for the Shungura and Nachukui Formations. The location of Konso is shown in the inset.
Published: 01 January 2006
Fig. 1.  Map of the lower Omo Valley of Ethiopia and the northern part of Lake Turkana in Kenya showing the Koobi Fora, Nachukui, and Shungura Formations as light stipple. Numbered points east of the lake refer to palaeontological collection areas. Section names are given for the Shungura
Journal Article
Journal: PALAIOS
Published: 01 July 2008
PALAIOS (2008) 23 (7): 452–464.
... of the Nachukui Formation at West Turkana and the Moiti and Lokochot Members of Koobi Fora at East Turkana. It also correlates well with the Mursi Formation and the Basal Member and Member A of the Omo Shungura Formation and the lower portion of the Hadar and Sangantole Formations in the Middle Awash region...
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Journal Article
Published: 01 August 1999
Journal of the Geological Society (1999) 156 (4): 731–745.
... horizon in the overlying Apak Member of the Nachukui Formation, yields an age of 4.22 ± 0.03 Ma; 40 Ar- 39 Ar age spectra on the succeeding Lothagam Basalt indicate an age of 4.20 ± 0.03 Ma for its eruption. Much of the rich faunal assemblage from the Nawata Formation derives from the tightly dated lower...
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FIGURE 2—Map of Lake Turkana area showing NAR1 locality in the Nariokotome Member of the Nachukui Formation
Published: 01 October 2003
FIGURE 2 —Map of Lake Turkana area showing NAR1 locality in the Nariokotome Member of the Nachukui Formation
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 Schematic stratigraphic columns for the formations discussed in the text. Some of the named tuff beds are indicated together with their 40Ar/39Ar ages determined on alkali feldspars from pumice clasts from within the tuff or feldspar crystals collected directly from the tuff. Arithmetic mean ages are given, and the uncertainty quoted is the standard deviation of the population (see Table 1). Correlations of tuffs between sections are shown. The Shungura Formation composite section is after de Heinzelin (1983), the Koobi Fora Formation is essentially that provided by Brown & Feibel (1986), noting a significant hiatus, and that for the Nachukui Formation is derived from Harris et al. (1988a, b) with minor modification. The sequence at Lothagam is from information summarized by Feibel (2003a), and that at Kanapoi is after Leakey et al. (1998) and Feibel (2003b).
Published: 01 March 2008
& Feibel (1986) , noting a significant hiatus, and that for the Nachukui Formation is derived from Harris et al. (1988 a , b ) with minor modification. The sequence at Lothagam is from information summarized by Feibel (2003 a ) , and that at Kanapoi is after Leakey et al . (1998) and Feibel (2003 b ) .
Journal Article
Published: 01 March 2008
Journal of the Geological Society (2008) 165 (2): 549–562.
... & Feibel (1986) , noting a significant hiatus, and that for the Nachukui Formation is derived from Harris et al. (1988 a , b ) with minor modification. The sequence at Lothagam is from information summarized by Feibel (2003 a ) , and that at Kanapoi is after Leakey et al . (1998) and Feibel (2003 b ) . ...
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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
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
Journal Article
Published: 01 January 2006
Journal of the Geological Society (2006) 163 (1): 185–204.
...Fig. 1.  Map of the lower Omo Valley of Ethiopia and the northern part of Lake Turkana in Kenya showing the Koobi Fora, Nachukui, and Shungura Formations as light stipple. Numbered points east of the lake refer to palaeontological collection areas. Section names are given for the Shungura...
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Journal Article
Published: 01 September 2004
Journal of Paleontology (2004) 78 (5): 1024–1027.
... of sandstones, mudstones, and tephras in facies interpreted as fluvial. Most of the fossils come from this formation. The Late Miocene–Early Pliocene Nachukui Formation consists of sandstones, mudstones, claystones, diatomites, and coquinas. This formation has an older fluvial phase and a younger lacustrine...
Journal Article
Published: 01 January 2006
Journal of the Geological Society (2006) 163 (1): 205–220.
... Turkana, Kenya, showing the Koobi Fora, Nachukui and Shungura Formations as shaded areas. Numbered points east of Lake Turkana indicate palaeontological collection areas. Localities and section names are given for the Nachukui and Shungura Formations. In this contribution we present 40 Ar/ 39 Ar...
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Journal Article
Published: 01 January 2004
Geological Magazine (2004) 141 (1): 41–53.
...Figure 2. Stratigraphic columns at localities where Gombe Group basalts have been identified, showing that they are confined to the lowest part of the Pliocene sections (see also Watkins, 1986 ). The Lonyumun Member of the Koobi Fora and Nachukui formations lies below the Moiti Tuff...
FIGURES
Image
 Map of the lower Omo Valley, Ethiopia, and the northern part of Lake Turkana, Kenya, showing the Koobi Fora, Nachukui and Shungura Formations as shaded areas. Numbered points east of Lake Turkana indicate palaeontological collection areas. Localities and section names are given for the Nachukui and Shungura Formations.
Published: 01 January 2006
Fig. 1.  Map of the lower Omo Valley, Ethiopia, and the northern part of Lake Turkana, Kenya, showing the Koobi Fora, Nachukui and Shungura Formations as shaded areas. Numbered points east of Lake Turkana indicate palaeontological collection areas. Localities and section names are given
Journal Article
Published: 01 November 2000
Journal of Paleontology (2000) 74 (6): 1173–1180.
.... This paper is a first step towards this goal. The specimens are housed in the National Museums of Kenya, Nairobi and bear their catalog numbers (prefixed KNM). Nachukui Formation, Omo Group. Late Pliocene (ca. 3.58–3.2 Ma) of South Turkwel, Turkana Basin, northern Kenya. Figure 1...
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Journal Article
Published: 01 March 2012
Journal of the Geological Society (2012) 169 (2): 213–226.
... 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...
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(a) Regional geological map of the Turkana Basin showing the contemporaneous Koobi Fora, Nachukui and Shungura formations. Sample localities shown as closed red circles. (b) Simplified stratigraphic section of the Koobi Fora and Shungura formations. Ages in red text are from this study. Source: map and stratigraphic section both modified after McDougall and Brown (2006).
Published: 15 June 2023
Fig. 1. ( a ) Regional geological map of the Turkana Basin showing the contemporaneous Koobi Fora, Nachukui and Shungura formations. Sample localities shown as closed red circles. ( b ) Simplified stratigraphic section of the Koobi Fora and Shungura formations. Ages in red text are from
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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 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
Journal Article
Journal: PALAIOS
Published: 01 October 2003
PALAIOS (2003) 18 (4-5): 445–453.
...FIGURE 2 —Map of Lake Turkana area showing NAR1 locality in the Nariokotome Member of the Nachukui Formation ...
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Lake Turkana, Kenya. Note the abundant faults that result from extension across the basin. The coeval Plio-Pleistocene deposits (Shungura, Nachukui, and Koobi Fora formations) are shown. Three volcanic provinces occur in the lake, forming North, Central, and South islands (abbreviated NI, CI, and SI, respectively). The black box highlights the study area near the village of Loiyangalani. Modified after McDougall and Brown (2008) and Dunkelman et al. (1988).
Published: 01 March 2014
Fig 2 Lake Turkana, Kenya. Note the abundant faults that result from extension across the basin. The coeval Plio-Pleistocene deposits (Shungura, Nachukui, and Koobi Fora formations) are shown. Three volcanic provinces occur in the lake, forming North, Central, and South islands (abbreviated NI
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 Generalized stratigraphic columns for the Nachukui, Koobi Fora and Shungura Formations from the level of the KBS Tuff ( H-2) to the Silbo Tuff. Named tuffs, discussed in the text, are shown in the stratigraphic columns in black. Secure correlations between sections are indicated. The age of each dated tuffaceous horizon is shown, based upon pooled single-crystal analyses. The age is given as the arithmetic mean and standard deviation of the population. Width of the unfilled stratigraphic column indicates the dominant detrital sediment, with widest to narrowest representing sand, silt and clay, respectively. A dashed line indicates the absence of sediment in the section.
Published: 01 January 2006
Fig. 3.  Generalized stratigraphic columns for the Nachukui, Koobi Fora and Shungura Formations from the level of the KBS Tuff ( H-2) to the Silbo Tuff. Named tuffs, discussed in the text, are shown in the stratigraphic columns in black. Secure correlations between sections are indicated. The age