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NARROW
Format
Article Type
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GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa (1)
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East African Rift (2)
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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Middle Atlas (1)
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-
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Morocco
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Moroccan Atlas Mountains
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Middle Atlas (1)
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-
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Southern Africa
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Botswana (1)
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Kalahari Craton (1)
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South Africa
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Gauteng South Africa (1)
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North-West Province South Africa (1)
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Transvaal region (1)
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Arctic Ocean
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Barents Sea (1)
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Asia
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Far East
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China
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Heilongjiang China
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Daqing Field (1)
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Henan China (1)
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Japan
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Hokkaido (1)
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Honshu
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Hyogo Japan
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Kyushu
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Kumamoto Japan (1)
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Korea
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Taiwan
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Chelungpu Fault (1)
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Taiwanese Central Range (1)
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Himalayas (1)
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Ili Basin (1)
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Indian Peninsula
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India
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Pakistan (1)
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Middle East
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Iran (5)
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Sette-Daban Range (1)
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West Siberia (1)
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Yakutia Russian Federation
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Atlantic Ocean
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Commonwealth of Independent States
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Indian Ocean
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Rocky Mountains
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Pacific Ocean
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polar regions (1)
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South America
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Argentina
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mineral exploration (1)
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elements, isotopes
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C-14 (1)
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hydrogen
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D/H (1)
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isotope ratios (2)
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isotopes
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stable isotopes
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metals
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iron
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nitrogen (1)
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noble gases
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radon
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Rn-222 (2)
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fossils
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Archaea (1)
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bacteria
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coliform bacteria
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Escherichia
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Desulfovibrio (1)
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Geobacter (1)
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Chordata
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Vertebrata
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Pisces
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Osteichthyes
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Teleostei (1)
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Tetrapoda
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Amphibia
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Labyrinthodontia
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Aves
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Mammalia
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Multituberculata (1)
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Primates
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Hominidae
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simians
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Rodentia
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Myomorpha
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Cricetidae
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Microtus (1)
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Metatheria (1)
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Reptilia
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Anapsida
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Testudines
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Cryptodira (1)
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Diapsida
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Archosauria
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dinosaurs
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Ornithischia
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Testudinata (1)
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eukaryotes (2)
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fungi (1)
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Graptolithina
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Hemichordata (2)
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Invertebrata
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Arthropoda
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Mandibulata
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Insecta
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Pterygota
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Neoptera
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Endopterygota
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Hymenoptera (1)
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Lepidoptera (1)
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Trilobitomorpha
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Trilobita (1)
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Brachiopoda (2)
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Bryozoa (2)
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Cnidaria
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Anthozoa
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Scleractinia (2)
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Echinodermata (1)
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Mollusca
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Gastropoda (1)
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Porifera (1)
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Protista
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Foraminifera
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Allogromiina (2)
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Radiolaria (3)
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Vermes
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Annelida (1)
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Metazoa (1)
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microfossils
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problematic microfossils (1)
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palynomorphs
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megaspores (3)
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miospores
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Classopollis (2)
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pollen (33)
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Plantae
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algae
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Chlorophyta
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Charophyta (1)
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Coccolithophoraceae
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Coccolithus (1)
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nannofossils (1)
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Rhodophyta (1)
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Pteridophyta
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Lycopsida (2)
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Spermatophyta
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Angiospermae
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Compositae (1)
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Gymnospermae
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Coniferales
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Pinaceae
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problematic fossils
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problematic microfossils (1)
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prokaryotes (3)
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geochronology methods
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geologic age
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Tertiary
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Neogene
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upper Miocene
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Pliocene
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middle Pliocene (1)
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upper Pliocene (2)
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Green River Formation (2)
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lower Paleocene
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upper Cenozoic (1)
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Mesozoic
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Upper Cretaceous
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Jurassic
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Paleozoic
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Permian
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Silurian (1)
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Precambrian
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Brockman Iron Formation (1)
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upper Precambrian
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Primary terms
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absolute age (2)
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Africa
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East Africa (1)
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East African Rift (2)
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North Africa
-
Atlas Mountains
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Moroccan Atlas Mountains
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Middle Atlas (1)
-
-
-
Morocco
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Moroccan Atlas Mountains
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Middle Atlas (1)
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-
-
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Southern Africa
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Botswana (1)
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Kalahari Craton (1)
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South Africa
-
Gauteng South Africa (1)
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North-West Province South Africa (1)
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Transvaal region (1)
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-
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Arctic Ocean
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Barents Sea (1)
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asbestos deposits (1)
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Asia
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Far East
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China
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Heilongjiang China
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Daqing Field (1)
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Henan China (1)
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Hunan China (1)
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Jilin China (1)
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Liaoning China (1)
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North China Plain (1)
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Ordos Basin (1)
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Shanxi China (1)
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Xinjiang China (1)
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Japan
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Hokkaido (1)
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Honshu
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Hyogo Japan
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Kobe Japan (1)
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Kanto Plain (1)
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Osaka Japan (1)
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Kyushu
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Kumamoto Japan (1)
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Korea
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Chelungpu Fault (1)
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Himalayas (1)
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Pakistan (1)
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Middle East
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Sette-Daban Range (1)
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atmosphere (1)
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Cenozoic
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Quaternary
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Pleistocene
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Mindel (1)
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Tertiary
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Neogene
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Miocene
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middle Miocene (2)
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Pebas Formation (1)
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Pontian (1)
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Pliocene
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middle Pliocene (1)
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upper Pliocene (2)
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-
Paleogene
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Eocene
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Green River Formation (2)
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lower Eocene (1)
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Paleocene
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lower Paleocene
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K-T boundary (1)
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Wasatch Formation (1)
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upper Cenozoic (1)
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ceramic materials (1)
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Chordata
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Vertebrata
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Pisces
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Osteichthyes
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Actinopterygii
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Teleostei (1)
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-
-
-
Tetrapoda
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Amphibia
-
Labyrinthodontia
-
Temnospondyli (1)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
chromosomal
Chromosomal mechanisms in the evolution of artiodactyls Free
Chromosomal DNA, DNA double helix, genes. The top part of this figure gives... Available to Purchase
Scheme of GA updating. (a) The chromosome, composed of 37 seismic attribute... Available to Purchase
A–C: Optical microscope images of a cell in sclerenchyma ring of a fossil r... Open Access
Symbionts of Marginopora vertebralis var. rossi from the Heron Island-W... Available to Purchase
Schematic example of the concatenation of model parameter bit strings into ... Available to Purchase
Example of a two-point crossover acting on the chromosome of two parents to... Available to Purchase
Illustration of regeneration mechanisms. Numbers correspond to electrode nu... Available to Purchase
Chromosome characteristics of 13 taxa of Lonicera . (1) Lonicera maackii... Available to Purchase
Backscattered electron images of pseudotachylyte vein. (A) Chromosome-shape... Open Access
An example that shows (a) a Prefix Gene Expression Programming (PGEP) struc... Available to Purchase
Comparative pollen morphology of the genus Iberis L. (Brassicaceae) in Turkey and its taxonomic implications Available to Purchase
Clustering maps of 13 taxa of Lonicera : (1) clustering map of pollen char... Available to Purchase
Were climatic changes a driving force in hominid evolution? Available to Purchase
Abstract A comparison of externalist and internalist approaches in hominid evolution shows that the externalist approach, with its claim that climate was responsible for the appearance of bipedalism and hominization, now seems to be ruled out by the biological, palaeogeographical, palaeontological and palaeoclimatic data on which it was based. Biological data support the embryonic origin of cranio-facial contraction, which determined the increase in cranial capacity and the shift in the position of the foramen magnum implying bipedalism. In the internalist approach, developmental biology appears as the driving force of hominid evolution, although climate exerts a significant influence and was involved in the following ways: (1) in the prior establishment of ecological niches that allowed the common ancestor to become differentiated into three subspecies; (2) by dividing up the area of distribution of species, resulting in the present-day subspecies of gorillas and chimpanzees; (3) by facilitating relative fluctuations of the geographical areas of distribution of the various species, particularly the spread of australopithecines across the African savanna from north (Chad, Ethiopia) to south (South Africa); (4) by determining adaptive geographical differentiations among Homo erectus and Homo sapiens (pigmentation, haemoglobin, etc.).