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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Angola (1)
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Asia
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Far East
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China
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Jilin China (1)
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Australasia
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New Zealand (1)
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Canada
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Western Canada
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Saskatchewan (1)
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-
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Europe
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Western Europe
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France
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Alpes-de-Haute Provence France (1)
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elements, isotopes
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carbon
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C-13/C-12 (3)
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isotope ratios (3)
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isotopes
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stable isotopes
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C-13/C-12 (3)
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O-18/O-16 (1)
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oxygen
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O-18/O-16 (1)
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fossils
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Invertebrata
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Echinodermata (1)
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Mollusca
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Cephalopoda
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Ammonoidea
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Ammonites (1)
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geologic age
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Cenozoic
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Quaternary
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Holocene (1)
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Pleistocene
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upper Pleistocene (1)
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-
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Tertiary
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Paleogene
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Eocene
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lower Eocene (1)
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Paleocene
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lower Paleocene (1)
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Paleocene-Eocene Thermal Maximum (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Albian (1)
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Upper Cretaceous (1)
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Primary terms
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Africa
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Central Africa
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Angola (1)
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-
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Asia
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Far East
-
China
-
Jilin China (1)
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-
-
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Australasia
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New Zealand (1)
-
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Canada
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Western Canada
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Saskatchewan (1)
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-
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carbon
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C-13/C-12 (3)
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Cenozoic
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Quaternary
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Holocene (1)
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Pleistocene
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upper Pleistocene (1)
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-
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Tertiary
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Paleogene
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Eocene
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lower Eocene (1)
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Paleocene
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lower Paleocene (1)
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Paleocene-Eocene Thermal Maximum (1)
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-
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climate change (1)
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data processing (1)
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Europe
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Western Europe
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France
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Alpes-de-Haute Provence France (1)
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-
-
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geophysical methods (1)
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Invertebrata
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Echinodermata (1)
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Mollusca
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Cephalopoda
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Ammonoidea
-
Ammonites (1)
-
-
-
-
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isotopes
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stable isotopes
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C-13/C-12 (3)
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O-18/O-16 (1)
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-
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Albian (1)
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Upper Cretaceous (1)
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-
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ocean floors (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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paleoecology (1)
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paleogeography (2)
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sedimentary rocks
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clastic rocks
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marl (1)
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sedimentation (1)
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sediments
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clastic sediments
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mud (1)
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peat (1)
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stratigraphy (1)
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rock formations
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Broken River Formation (1)
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sedimentary rocks
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sedimentary rocks
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clastic rocks
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marl (1)
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sediments
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sediments
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clastic sediments
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mud (1)
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peat (1)
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Steady decline in mean annual air temperatures in the first 30 k.y. after the Cretaceous-Paleogene boundary
Terrestrial methane cycle perturbations during the onset of the Paleocene-Eocene Thermal Maximum
Operation of the boreal peatland methane cycle across the past 16 k.y.
Albian ammonites of the Benguela Basin (Angola): a biostratigraphic framework
3D surface-related multiple modeling
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.).