Journal
SCIENCE
Volume 326, Issue 5949, Pages -Publisher
AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/science.1175817
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Funding
- NSF [8210897, 9318698, 9512534, 9632389, 9910344, 0321893]
- Institute of Geophysics and Planetary Physics of the University of California at Los Alamos National Laboratory (LANL)
- Philip and Elaina Hampton Fund for Faculty International Initiatives at Miami University
- Direct For Social, Behav & Economic Scie [8210897, 0321893, 9512534, 9318698] Funding Source: National Science Foundation
- Division Of Behavioral and Cognitive Sci [9318698, 9512534, 0321893, 8210897] Funding Source: National Science Foundation
- Division Of Behavioral and Cognitive Sci
- Direct For Social, Behav & Economic Scie [9910344, 9632389] Funding Source: National Science Foundation
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Sediments containing Ardipithecus ramidus were deposited 4.4 million years ago on an alluvial floodplain in Ethiopia's western Afar rift. The Lower Aramis Member hominid-bearing unit, now exposed across a >9-kilometer structural arc, is sandwiched between two volcanic tuffs that have nearly identical 40Ar/39Ar ages. Geological data presented here, along with floral, invertebrate, and vertebrate paleontological and taphonomic evidence associated with the hominids, suggest that they occupied a wooded biotope over the western three-fourths of the paleotransect. Phytoliths and oxygen and carbon stable isotopes of pedogenic carbonates provide evidence of humid cool woodlands with a grassy substrate.
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