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all geography including DSDP/ODP Sites and Legs
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Africa
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Afar Depression (1)
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simians (2)
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Primary terms
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absolute age (6)
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Africa
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East Africa
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Afar Depression (1)
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Ethiopia
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Omo River (1)
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Omo Valley (1)
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Ethiopian Rift (1)
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Kenya (4)
-
Lake Turkana (1)
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Tanzania
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Olduvai Gorge (1)
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-
Turkana Basin (4)
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-
East African Lakes
-
Lake Turkana (1)
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-
East African Rift (2)
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Nile River (1)
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Nubian Shield (1)
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Asia
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Arabian Peninsula
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Arabian Shield (1)
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Indian Peninsula
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India
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Bastar Craton (1)
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Cenozoic
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Koobi Fora Formation (3)
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Omo Group (2)
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Quaternary
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Holocene (1)
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Pleistocene
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lower Pleistocene
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Olduvai Subchron (1)
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Matuyama Chron (1)
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Shungura Formation (3)
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Tertiary
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Neogene
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Pliocene (3)
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upper Cenozoic (1)
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Chordata
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Vertebrata
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Tetrapoda
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Mammalia
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Theria
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Eutheria
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Primates
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Hominidae
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Australopithecinae
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Australopithecus (1)
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Homo
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Homo erectus (1)
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Homo habilis (1)
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Homo sapiens (1)
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simians (2)
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crust (1)
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deformation (1)
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geochemistry (1)
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geochronology (2)
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igneous rocks
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plutonic rocks
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granites
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leucogranite (1)
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ultramafics (1)
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volcanic rocks
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basalts (1)
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glasses
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volcanic glass (1)
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pyroclastics
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pumice (3)
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tuff (3)
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rhyolites (1)
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Indian Ocean (1)
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isotopes
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stable isotopes
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magmas (1)
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metals
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rare earths
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neodymium (1)
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metamorphic rocks (1)
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metamorphism (1)
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oxygen
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O-18/O-16 (1)
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paleoclimatology (2)
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plate tectonics (1)
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Precambrian
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upper Precambrian
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Proterozoic
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Neoproterozoic (1)
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sedimentary rocks
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clastic rocks
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tectonophysics (1)
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sedimentary rocks
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sedimentary rocks
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clastic rocks
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sandstone (1)
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volcaniclastics (1)
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sediments
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volcaniclastics (1)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Konso Formation
Sequence of tuffs between the KBS Tuff and the Chari Tuff in the Turkana Basin, Kenya and Ethiopia Available to Purchase
Chronological distribution of named and correlated tuffs in the five groups... Available to Purchase
( A ) Synthetic stratigraphic logs of the Kibish, Konso, and Herto Bouri fo... Available to Purchase
Map of the lower Omo Valley of Ethiopia and the northern part of Lake Turka... Available to Purchase
Using Radiometric Dating, Magnetostratigraphy, and Tephrostratigraphy to Calibrate Rates of Hominin Evolution in the East African Rift Available to Purchase
40 Ar/ 39 Ar eruption ages of Turkana Basin tuffs: millennial-scale resolution constrains palaeoclimate proxy tuning models and hominin fossil ages Open Access
Precise 40 Ar/ 39 Ar geochronology for the upper Koobi Fora Formation, Turkana Basin, northern Kenya Available to Purchase
New single crystal 40 Ar/ 39 Ar ages improve time scale for deposition of the Omo Group, Omo–Turkana Basin, East Africa Available to Purchase
Petrogenesis and Metallogenic Evolution of Leucogranites from the Paleoproterozoic Malanjkhand Granitoids, Central India Available to Purchase
Geology, geochronology and geodynamic implications of the Cenozoic magmatic province in W and SE Ethiopia Available to Purchase
INTERESTING PAPERS IN OTHER JOURNALS Available to Purchase
Zircon U–Pb ages, δ 18 O and whole-rock Nd isotopic compositions of the Dire Dawa Precambrian basement, eastern Ethiopia: implications for the assembly of Gondwana Available to Purchase
Climatic significance of clay minerals in Cenozoic marine and lacustrine sediments Available to Purchase
Ophiolites in Northeast and East Africa: implications for Proterozoic crustal growth Available to Purchase
Large mammal turnover in Africa and the Levant between 1.0 and 0.5 Ma Available to Purchase
Abstract Faunal change at the Early–Middle Pleistocene boundary in Europe has long been a topic for discussion. However, analyses of large mammal turnover at this time in Africa have been lacking, largely because of the low number of sites dated to this interval. Recent work, particularly in the last 10 years, has resulted in a much larger published sample of sites and we synthesize these data in this paper. In our multivariate (TWINSPAN) analyses of African and Levantine large mammal faunas we found that localities were subdivided by geographic regions, not by age. There were some small-scale changes with the appearance or extinction of particular taxa, but there was no large-scale turnover such as that seen in Europe. The Levant was included as a possible route for faunal interchange with east Africa, but no similarities were found between these areas. It therefore appears that the modern zoogeographic separation of the Levant and north Africa into the Palaearctic region and sub-Saharan Africa into the African region can be traced back to at least the Early–Middle Pleistocene boundary.
Hominins and the Early–Middle Pleistocene transition: evolution, culture and climate in Africa and Europe Available to Purchase
Abstract Some of the more important evidence is reviewed for the archaeology of hominin colonization associated with the Early-Middle Pleistocene transition. This is done by reference to the nature of migration ‘out of Africa’ before the interval of transition, across the transition itself, and then after it. Technologically assisted behaviour may not have been so important in the colonization process, behaviour and biology being the primary factors that led to the success of a migrating species. While climate change and especially shifts in local aridity would have been experienced and possibly remembered by localized hominin groups, the Acheulean behavioural repertoire did not change much across Africa and Europe over a million years of time. It merely adapted to local conditions. The Acheulean was a generalized hand-held processing technology for a generalized hominin.