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The geological, isotopic, botanical, invertebrate, and lower vertebrate contexts for aripithecus ramidus

Journal Article · · Science
 [1];  [2];  [3];  [3];  [4];  [5];  [6];  [5];  [7];  [8];  [9];  [10];  [8]
  1. Los Alamos National Laboratory
  2. UNIV OF ILLINOIS
  3. CEREGE, FRANCE
  4. MONTPELLIER, FRANCE
  5. MIAMI UNIV, OXFORD, OHIO
  6. STANFORD UNIV.
  7. UNIV OF ALBERTA
  8. UC/BERKELEY
  9. NANTERRE, FRANCE
  10. CANADA

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 {sup 40}Ar/{sup 39}Ar 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.

Research Organization:
Los Alamos National Laboratory (LANL)
Sponsoring Organization:
DOE
DOE Contract Number:
AC52-06NA25396
OSTI ID:
971297
Report Number(s):
LA-UR-09-06141; LA-UR-09-6141
Journal Information:
Science, Journal Name: Science Journal Issue: 5949 Vol. 326; ISSN 0193-4511; ISSN SCEHDK
Country of Publication:
United States
Language:
English

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