Written by
C. David Kreger
Introduction
Throughout the early years of paleoanthropology, there
were only two different species that were attributed to
the genus Homo. These included the Neanderthals,
and Homo erectus. In the early 1960s, this began
to change, and human ancestry seemed to be populated by
many different players. Accordingly, erectus is
one of the better-known members of genus Homo,
especially in terms of its well-established place in paleoanthropology.
This has begun to change, however, and now some question
its place in human evolution.
Some
(e.g., M. Wolpoff) claim that erectus is an invalid
taxon, though few accept this interpretation at this
point in time. Others believe that the material previously
attributed to erectus should be split into several
different taxons: Asian and later African material remaining
as erectus (with erectus not contributing
to modern humans), early African material as ergaster,
and European material as heidelbergensis. In
this description of the species, the material that has
been attributed as ergaster and erectus
in the above splitting scenario will be covered, with
the heidelbergensis material discussed under
the page dedicated to that species.
The
species was named by Eugène Dubois (it was originally
designated as Pithecanthropus erectus) in 1894,
after his 1891 find from Trinil, Java, in Indonesia
(Trinil 2). Dubois was inspired by A. Wallace's conviction
that the origins of modern humans might lie in Southeast
Asia. Dubois enlisted as an army surgeon in the Royal
Dutch East Indies Army, and searched for fossils in
Sumatra. He had little success in Sumatra, but found
unearthed a thick mineralized hominid skull near the
bank of the Solo River in Java. Dubois made his find
public a few years later, and was met by derision from
the dominant British paleontological hierarchy. Dubois
was disillusioned, and this important find actually
spent some time in a box underneath the floorboards
of Dubois' home.
The
material was later associated with the Chinese material
from Zhoukoudian, and renamed Homo erectus. Except
for modern Homo sapiens, erectus was the
most far-ranging hominid to have existed. Material that
has been attributed to erectus has come from
South Africa, Indonesia, England, and just about everywhere
in between, covering the entire continents of Africa,
Asia, and Europe. The European material will not be
discussed here (it is discussed under heidelbergensis),
but the rest of the material will be covered here under
erectus.
Diagnostic Features
The dates for erectus have become earlier and
earlier, while habilis remains have been found
in later and later deposits, making a lineage involving
habilis ancestral to erectus increasingly
unlikely. Specimens that are considered erectus
are dated very securely to at least 1.8 myr, and fairly
securely to 1.9 myr. The question of this species' evolutionary
destiny is under some disagreement. Those who accept
the validity of ergaster usually consider erectus
an evolutionary dead-end that went from Africa into
Asia, and went extinct there. Those who see erectus
as a modern human ancestor, either see the Asian specimens
as a dead-end side branch, or see all the ergaster,
heidelbergensis, and erectus specimens
as belonging to Homo sapiens.
This
view has some validity in that these species are usually
considered "chronospecies" due to anagenesis.
Some researchers do not support the concept of anagenesis
as a valid mechanism of speciation, since there is a
"fuzzy" area where the transition between
species occurs, whereas in cladogenesis (the splitting
of a species into two new species or the branching off
of one species from another) there is a "clear"
boundary. However, the method of speciation is the same
in both, since beyond the moment of the split in cladogenesis,
the transition to new species is by anagensis. So this
is really a matter of semantics and differing ideologies.
In any case, erectus shows clear trends in the
modern direction, and I personally think that the most
parsimonious answer is that erectus is an ancestor of
modern humans, and not an evolutionary dead-end. However,
that is just my personal opinion.
There
are specimens from a wide time span and a vast geographical
area that have been attributed to erectus. The
traits of these specimens are very similar, and show
a trend toward the modern human condition. Some of the
trends linking erectus with sapiens includes:
- An
increase in brain size (erectus approximately 900
cc., sapiens approximately 1350 cc.).
- A
reduction in postcanine dentition, and a correlated
decrease in jaw size.
- Vertical
shortening of the face.
- Shortening
of armbones (especially the forearm) to come to a
very humanlike limb proportions (postcranial proportions
are very similar to tropically adapted modern humans).
- The
development of a more barrel-shaped chest.
- The
formation of an external nose.
- Reached
modern human size in terms of height.
One
of the most important erectus specimen is the
Nariokotome Boy, KNM-WT 15000. This specimen was discovered
by a team led by R. Leakey and A. Walker at Nariokotome,
Kenya, in 1984. This is the most complete early human
skeleton ever discovered. The specimen was dated to
1.6 myr, and is considered by some as ergaster,
but to most researchers it is definitely erectus. The
relative completeness of this specimen allowed detailed
examination of the anatomy of erectus, and has
led to many influential ideas about this species. Some
of its important features include:
- It
is
the skeleton of a 10-12 year old individual (generally
considered male).
- The
teeth are unworn.
- Shovel-shaped
incisors.
- Was
5'3" (168 cm) tall at death, and may have been
as tall as 6'0" (183 cm) if it had reached maturity.
- Resembles
a very robust modern human from the neck down.
- A
880 cc. brain (estimated that its mature brain size
would be 909 cc.).
- Brachial
and humero-femoral index in the modern human range.
- Had
relatively small (compared to modern humans) thoracic
spinal canal diameter.
- Smaller
cervical and lumbar swellings (relative to modern
humans).
- External
projecting nose.
- Longer
vertebral spines (relative to modern humans).
- An
elongated femoral neck.
- A
narrow biilliac breadth.
The
narrow spinal canal has been an issue of much speculation.
Some contend that this means that KNM-WT 15000 had small
intercostal muscles (used for fine air control during
speech in modern humans). However, this was a juvenile
and the neurocanal size may have increased by 30% by
maturity. Also, even though it has a small canal size
relative to its body size, it is still within the modern
human range (albeit, at the bottom.) This is a very
tenuous piece of evidence that has been used to make
very specific statements about early human capacity
for speech. Considering it is within the human range
at all, it makes it unlikely that this would have prevented
the capacity for speech, and since it is a juvenile
specimen, sweeping statements about the species capacity
for language based on this trait is very weak.
A
very important specimen (especially in terms of the
history of paleoanthropology) is KNM-ER
3733. This fairly complete cranium is responsible
for sinking the single species concept as a hard and
fast rule. The specimen was found by a team led by R.
Leakey at Koobi Fora, Kenya, in 1975. The specimen has
been dated to approximately 1.75 myr. This is usually
considered the remains of a female due to the decreased
level of robusticity compared to conspecifics such as
KNM-WT 15000. Some of its key features include:
- Is
a mature adult specimen (known from the closed cranial
sutures and the erupted M3s).
- A
low cranial vault (characteristic of Asian erectus).
- Some
keeling along the midline of the cranium.
- A
round torus across the occipital bone.
- A
cranial base that is wider at the base than at the
top of the cranium.
- Possible
evidence of alveolar torus.
- An
848 cc. brain.
- Moderately
sized postcanines and large anterior teeth.
- Clear
evidence of an external projecting nose.
- Double-arched
supraorbitals.
Another
African erectus specimen is KNM-ER 3883. This
specimen is thought to be a male from the same population
that ER 3733 came from. It was found in the same area,
Koobi Fora, Kenya. It has been dated to approximately
1.57 myr and is the best-preserved early male cranium.
Some of its features include:
- Roughly
equivalent brain size to ER 3733 (minimally 804 cc.,
but likely larger).
- Clear
evidence of an external projecting nose.
- Projecting
nasal bones, which tend to be convex and relatively
wide.
- Margins
of nose everted laterally (deviate laterally).
- Presence
of anterior nasal spine.
- Clear
angulation of margin of nasal floor and premaxillae.
- A
forehead flatter than ER 3733 with less of a supratoral
sulcus separating it from the top of the supraorbitals.
- Much
larger mastoids than ER 3733.
- A
slightly developed nuchal torus.
- Well-developed
supraorbitals that are not double-arched.
- The
erectus specimens from China were some of the
first hominids that were discovered. The various specimens
from Dragon Bone Hill, in the cave of Zhoukoudian
were discovered in the late 1920s; however, all but
two teeth that were sent abroad for analysis were
lost in the chaos of W.W.II. The material included
five skullcaps, several cranial and facial fragments,
eleven mandibles, and 147 isolated teeth. This material
was used for the reconstruction of "Peking Man"
by F. Weidenreich. A newer reconstruction has been
made by I. Tattersall and G. Sawyer that uses fragments
that are assumed to be male, as the original reconstruction
used both male and female remains. The newer cranial
reconstruction results in a larger cranial capacity
with a more massive and projecting face, with a broader
taller nasal region. This new reconstruction is more
similar to erectus from elsewhere in the world.
The material has been dated to approximately 400 kyr
to 500 kyr.
The
five skullcaps have a mean cranial capacity of 1043
cc. The supraorbital torus on the reconstruction is
smaller than that of OH 7 or Sangiran 17 from Java.
The Zhoukoudian occipital bones are strongly flexed
with a broad torus across the bone's width. The skullcaps
are also characterized by flat, thick, rectangular parietal
bones. The facial bones are massive, and the mandibles
are very robust. The Asian specimens show some general
differences from African erectus, including more robust
ridges of bone with the walls of the skull greatly thickened.
The
Javanese specimens are a source of great controversy.
No specimen from Indonesia has been found in a well-dated
locale. Often, they have been found by locals and bought
by researchers or interested laypersons. The older dates
(ranging near 1.7 myr) are very controversial, and very
tenuous. For example, the Modjokerto child was discovered
by a hired workman in 1936, and the specimen was "dated"
decades later by looking at the material that adhered
to the cranium, and matching that matrix to a strata
based on the information of where the specimen was found,
finding a strata that matched the material taken from
the specimen, then dating the samples of stratum that
were assumed to be where the specimen originally came
from. Specimens like Sangiran 17 and Trinil 2 have been
dated to approximately 800 kyr and 400 kyr, respectively.
The
best preserved hominid cranium from Java is Sangiran
17. This specimen was discovered by a farmer at Sangiran,
Java, Indonesia, in 1969. Sangiran 17 has been an important
specimen for those who accept the multiregional hypothesis
that has erectus moving into Asia early, and
evolving into Homo sapiens with gene flow being
maintained between various African, Asian, and European
populations. In Indonesia, this hypothesized lineage
begins with Modjokerto, moves on through Sangiran 17,
the material from Sambungmachan, Ngandong, all the way
through present day Javanese. Some of the traits that
are cited to link this lineage together includes:
- A
long relatively flat frontal bone.
- A
projecting face with massive, flat zygomatics.
- A
zygomaxillary tuberosity at the base of the zygomatics.
- A
rounded edge to the bottom at the eye sockets.
- The
lack of a clear demarcation between the nasal region
and the lower face.
The
Sangiran 17 specimen itself shows several other features
that distinguish the Indonesian material from other
populations of erectus. Many of these also fit
into the multiregional model. These features include:
- Very
thick cranial bones which are flattened along the
sides of the braincase.
- A
maximum cranial breadth at the base of the cranium.
- A
reduced development of the frontal and parietal lobes
of the brain, though more developed elsewhere (Sangiran
17 is at the high end of the erectus scale with an
approximate 1029 cc. brain).
- Prominent
muscle markings along the sides and back of the cranium.
Conclusions
Homo erectus (or the various species which may
be subsumed under that appellation) are extremely important
in the study of modern human origins. The Middle Pleistocene
is where the modern human postcrania develops, the modern
cranial features begin to develop, and significant increases
in brain size occur. It is also important because many
behavioral changes occur in this time period, e.g.,
much more developed lithic industries, the controlled
use of fire, regular meat-eating, hunting, etc. This
is where the things most people consider "human"
start to develop to the point where most people would
recognize these pattern of anatomy and behavior as human.
This is also a dynamic time in the evolutionary perspective
caused by these species, with the recent well-dated
Dmanisi remains in the Republic of Georgia, dated to
1.7 myr.
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