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long term climate change
food resources limited and geographically separated, requires travel between locations and stimulates exploitation of new resources
is bipedalism a response to changing environments
loss of habitat forces shift to using new resources
loss of habitat forces travelling between resources
why bipedalism
seeing over the grass
carrying food/offspring
efficient locomotion
holding weapons and tools
thermoregulation
was there a savanna expansion
as a result of their different photosynthetic pathways C3 and C4 plants have very distinct carbon isotope signatures
expansion of the C4 savanna ecosystem
Expansion of grasslands from 9-7 million years ago (% Poaceae). Followed by a more gradational increase in desert/semi-desert pollen from ~7 Ma.
timescale for C4 savanna global expansion
~10-2 million years ago
oldest hominin candidate
Sahelanthropus tchadensis - Northern Chad
Sahelanthropus tchadensis
discovered in 2002, lived ~7 million years ago in Northern Chad
limited fossil record
fragments on nine crania, 2 partial ulnae and a femur shaft
strong variability in the climate
sediments at fossil sites are fluvial, lacustrine and aeolian
Late Miocene climate
warmer (possibly wetter) than today
Candidate 2
Orrorin tugenensis
Orrorin tugenensis information
lived in Kenya ~6-5.8 million years ago
Orrorin tugenensis remains
teeth and lower jaw fragments, pieces of the humerus, partial femora and a phalanx
why bipedalism
size and shape of femur
evidence for bipedality - Ardipithecus ramidus
upper pelvic anatomy consistent with bipedality
lower pelvic anatomy ape like
Ardi evidence for arboreal activity
foot anatomy
evidence for a mixed lifestyle
more than 150,000 specimens of fossilised plants and animals from nearby localities - 36 Ardi individuals found so far
home for Ardi
river-margin forest in an otherwise savanna
riparian attracts
number of fauna - modern afar tribes
bipedal like behaviour
observed in chimpanzees and orangutans - hands for stabilisation/feeding