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an emergent
website design
by
peter jay stein, md, ma
atmosphere
asthenosphere
lithosphere
regolith
biosphere
hydrosphere
This 54 page synopsis of the evolution
of the Earth, the origin and progression of life, and the
emergence of humans as descendants of the hominin lineage, divides the last 4.57 billion years into progressively overlapping, imagistic, time segments, to outline our place in biological existence.
magnetosphere
ionosphere
TWENTY-SIX
Emergent Primates II
adapted from Roberts, 2011, p. 41; Springer, 2005, pp. 82-83;
J. Kendrick, 2014; anthro.palomar.edu; and news.NationalGeographic.com, 2007
Following the extinction of the reptilian (diapsid lineage) dinosaurs, around 66 mya, and closer to 56 mya, there survived small, nocturnal mammals, the tree shrews (order Scandentia).
There then followed what may be considered the most primitive of early primates, the plesiadapiforms (e.g., Carpolestes simpsonii, an extinct, insectivore, with an abducted hallux and nail (instead of claw), allowing for arboreal grasping), also represented by Dromomys szalayi (National Geographic News, 2007), one of the earliest primate fossil remains, and possibly the last common ancestor (LCA) to modern primates, based on its pattern of molar teeth, suggestive of a diet of fruit and insects, and grasping hands and feet, to facilitate tree-living.
However, with no orbital convergence, no leaping, small brains, and with growing incisors and loss of canine teeth, this group diverged away from modern primates.
These earliest of primates probably co-evolved with flowering plants and trees, in a world characterized by tropical and semi-tropical climates, even at the poles.
In the late
Paleocene (66-56 mya),
Altiatlasius (a haplorrhine),
represents another early ancestral candidate
of modern primates,
only identified by its teeth.
Soon after this period,
in the early Eocene (56-34 mya),
are found fossil
strepsirrhines (adapids), and
haplorhines (omomyids),
considered sister clades to the
plesiadapids.
The omomyids,
spread across several continents,
are the earliest
haplorhines,
possibly the ancestors to the
tarsiers, monkeys, apes,
and
humans.
CENOZOIC ERA
66 mya to present
paleocene epoch
66-56 mya
tree shrew
(Scandentia)
and
Altiatlasius koulchii
(haplorhine?)
plesiadapiforme
primate-like
"proto-primate"
dromomys
Carpolestes simpsonii
(55 mya)
dinosaur extinction
end of MESOZOIC
(66 mya)
EUPRIMATE #2 - omomyids
(haplorhines)
EUPRIMATE #1 - adapids:
(strepsirrhines)
Darwinius Masillae
47 mya
discovered in Messel, Germany 1983
Infra-order: Adapiformes
resembles modern lemur
middle Eocene
basal primate characteristics
ancestor to modern lemurs & lorises
(Prosimii or Prosimian)
anthropoids:
NEW OLD
world monkeys
Archonta
mammalian superorder
that suggests a common ancestor of:
tree shrews, bats, flying lemurs, and primates
image from J. Kendrick, 2014:
Eosimiidae
catarrhini
two groups of Eocene (56-34 mya) primates
(Eocene is Greek for "dawn" and "new")
hominoids:
gibbons
orangutans
gorillas
chimpanzees
hominins (23)
genus Homo (9)
Humans
(Homo sapiens)
Eosimias
45 mya
"Dawn Monkey"
known by its fossil jaw and skull fragments,
an example of the earliest anthropoid.
platyrrhini
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