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Koobi Fora

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Journal Article
Published: 01 September 2010
Journal of Paleontology (2010) 84 (5): 996–1002.
...Henning Scholz; Matthias Glaubrecht Abstract New field collections allow the study and description of Valvata juliae new species from the Pliocene upper Burgi Member of the Koobi Fora Formation of Kenya. The shell morphology of this species varies from trochospiral to planispiral to open coiled...
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First thumbnail for: A New and Open Coiled Valvata (Gastropoda) from th...
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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 Omo–Turkana Basin. The upper half of the Koobi Fora Formation from just below the KBS Tuff to above...
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First thumbnail for: Precise 40 Ar/ 39 Ar geochronology for the up...
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Journal Article
Published: 01 January 1987
Journal of Paleontology (1987) 61 (1): 130–134.
Journal Article
Published: 01 March 1986
Journal of the Geological Society (1986) 143 (2): 297–310.
... with the biostratigraphic zonations based on vertebrate and molluscan studies. The sedimentary sequence of the Koobi Fora Formation attains an aggregate thickness of 560 m and spans the period from about 4.3 to 0.6 Ma. Detailed correlations have now been established to relate this sequence to other deposits within...
Journal Article
Journal: GSA Bulletin
Published: 01 February 1985
GSA Bulletin (1985) 96 (2): 159–175.
...IAN MCDOUGALL Abstract In the Koobi Fora region, east of Lake Turkana, northern Kenya, there occurs a sequence ∼500 m thick of lacustrine, fluvial, and deltaic sediments that contains abundant vertebrate fossils, including hominids, as well as stone tools. Rhyolitic tuffs within the sedimentary...
Journal Article
Published: 01 June 1982
Journal of Sedimentary Research (1982) 52 (2): 401–414.
...Andrew S. Cohen Abstract A study of fossil mots and root casts from East Turkana, Kenya, has shown them to be useful paleoenvironmental indicators. Fossil root casts were obtained from the Pleistocene, Upper Member of the Koobi Fora Formation, deposited within the East Turkana Embayment of the Lake...
Journal Article
Published: 01 January 1979
Bulletin de la Société Géologique de France (1979) S7-XXI (3): 343–347.
...A. Vincens GeoRef, Copyright 2004, American Geological Institute. 1979 Africa Angiospermae archaeological sites Cenozoic East Africa East African Lakes Gramineae Kenya Koobi Fora Formation Lake Turkana microfossils miospores Monocotyledoneae palynomorphs Plantae Pleistocene...
Image
Boundstones from the Koobi Fora Formation. Laminar bindstone (tufa) (L) growth occurs at the bottom right of the photo. Here, the microbial growth occurs in thin (3 cm) layers. After the introduction of rounded basalt cobbles, the microbial growth continues but becomes more stromatolitic (S).
Published: 01 March 2014
Fig 9 Boundstones from the Koobi Fora Formation. Laminar bindstone (tufa) (L) growth occurs at the bottom right of the photo. Here, the microbial growth occurs in thin (3 cm) layers. After the introduction of rounded basalt cobbles, the microbial growth continues but becomes more stromatolitic (S).
Image
Composite section of the Koobi Fora Formation for the Loiyangalani region, southeast Turkana Basin. Because member boundaries are defined by tuffs, only five of the eight members have been identified just north of Loiyangalani. Modified from Gathogo et al. (2008). The outcrops from the study area belong to the Tulu Bor Member, based on the stratigraphic position of the Kankam Basalt and other marker beds.
Published: 01 March 2014
Fig 5 Composite section of the Koobi Fora Formation for the Loiyangalani region, southeast Turkana Basin. Because member boundaries are defined by tuffs, only five of the eight members have been identified just north of Loiyangalani. Modified from Gathogo et al. (2008) . The outcrops from
Image
Published: 01 March 2014
Table 1 Descriptions of Koobi Fora Facies.
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Composite stratigraphic column for the Koobi Fora Ridge with some key tuff layers, the mollusk (C) and stromatolite (A) marker beds and the samples of the Gabbiella shells and opercula studied herein (column from Feibel, 1999).
Published: 01 January 2013
Figure 2 Composite stratigraphic column for the Koobi Fora Ridge with some key tuff layers, the mollusk (C) and stromatolite (A) marker beds and the samples of the Gabbiella shells and opercula studied herein (column from Feibel, 1999 ).
Image
Figure3—1–19. Valvata juliae sp. nov., upper Burgi Member, Koobi Fora Formation. 1–3, RGM 550.171, KF06SG-20. 1, apertural view; 2, umbilical view; 3, protoconch.; 4, RUP P 9200, apertural view; 5, RGM 550.178, KF06SG-18, apertural view; 6, RGM 550.172, KF06SG-20, apertural view; 7, MCZ 190857, apertural view; 8–9, RGM 550.179, KF06SG-18; 8, apertural view; 9, apical view; 10, RGM 550.176, KF06SG-20, apertural view; 11, RGM 550.177, KF06SG-20, lateral view; 12–13, RGM 550.173, KF06SG-20: 12, apertural view; 13, apical view; 14–15, RGM 550.174, KF06SG-20; 14, apertural view; 15, apical view; 16–19, RGM 550.175, KF06SG-20: 16, apertural view; 17, apical view; 18, 19, protoconch.; 20–22, Valvata niloticaJickeli, 1874, MCZ 190859, Ethiopia: 20, apertural view; 21, 22, protoconch. A scale is given for all protoconch figures separately. The scale for all other images is in the lower left corner of the figure.
Published: 01 September 2010
Figure 3 —1–19. Valvata juliae sp. nov., upper Burgi Member, Koobi Fora Formation. 1–3 , RGM 550.171, KF06SG-20. 1 , apertural view; 2 , umbilical view; 3 , protoconch.; 4 , RUP P 9200, apertural view; 5 , RGM 550.178, KF06SG-18, apertural view; 6 , RGM 550.172, KF06SG-20, apertural view
Image
 Stratigraphic relations of tuffs of Group 4, from the Koobi Fora Tuff up to and including the Lokapetamoi Tuff. The section labelled Stern, Area 131 is from Stern (1993). Others are from field notes of F.H.B.
Published: 01 January 2006
Fig. 6.  Stratigraphic relations of tuffs of Group 4, from the Koobi Fora Tuff up to and including the Lokapetamoi Tuff. The section labelled Stern, Area 131 is from Stern (1993) . Others are from field notes of F.H.B.
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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
Journal Article
Published: 01 March 2012
Journal of the Geological Society (2012) 169 (2): 213–226.
.... The new age data on feldspars from the pumice clasts range from 4.02 ± 0.04 Ma for the Naibar Tuff of the Koobi Fora Formation to 1.53 ± 0.02 Ma for Tuff K of the Shungura Formation. The Orange Tuff in the KBS Member of the Koobi Fora Formation was dated at 1.76 ± 0.03 Ma, providing good control...
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First thumbnail for: New single crystal 40 Ar/ 39 Ar ages improve time ...
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Journal Article
Published: 01 January 2006
Journal of the Geological Society (2006) 163 (1): 185–204.
...Fig. 6.  Stratigraphic relations of tuffs of Group 4, from the Koobi Fora Tuff up to and including the Lokapetamoi Tuff. The section labelled Stern, Area 131 is from Stern (1993) . Others are from field notes of F.H.B. ...
FIGURES
First thumbnail for: Sequence of tuffs between the KBS Tuff and the Cha...
Second thumbnail for: Sequence of tuffs between the KBS Tuff and the Cha...
Third thumbnail for: Sequence of tuffs between the KBS Tuff and the Cha...
Journal Article
Published: 01 January 2013
Journal of Paleontology (2013) 87 (1): 84–90.
...Figure 2 Composite stratigraphic column for the Koobi Fora Ridge with some key tuff layers, the mollusk (C) and stromatolite (A) marker beds and the samples of the Gabbiella shells and opercula studied herein (column from Feibel, 1999 ). ...
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First thumbnail for: Shell and Operculum Taphonomy of the Bithyniid Gas...
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Journal Article
Published: 01 August 1980
Journal of the Geological Society (1980) 137 (4): 431–441.
...L. E. Frostick; I. Reid Abstract An analysis of the Koobi Fora Plateau Gravel, N Kenya, reveals clear-cut but contradictory patterns of sedimentary sorting. Basalt particles form the major constituent and decrease in diameter downstream at a rate of 3 mm km -1 , while feldspar is virtually...
Journal Article
Journal: Elements
Published: 01 April 2023
Elements (2023) 19 (2): 75–81.
...–Pleistocene localities in eastern Africa, Tanzania (Oldupai * (Olduvai) Gorge and Laetoli), Kenya (Allia Bay, Kanapoi, and Koobi Fora), and Ethiopia (Hadar, Woranso-Mille, and Dikika) over the past 75 years of research. E-mail: [email protected] E-mail: [email protected] E...
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First thumbnail for: The Dawn of Humanity: What Can Paleoanthropologist...
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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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First thumbnail for: SUIDS, ELEPHANTOIDS, PALEOCHRONOLOGY, AND PALEOECO...
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