Fully modern Homo sapiens ('wise man') became established in Africa
after descending from Homo
heidelbergensis and going through a transitional phase with
Homo
sapiens idaltu.
Homo sapiens had a characteristic look: their faces were (and of
course still are) small and tucked under a high, domed braincase. They had
small eyebrow ridges and their lower jaw ended in a prominent chin. On
average, their bodies were less muscular than those of earlier hominids.
The appearance of modern humans coincided with the appearance of highly
crafted tools, efficient food-gathering strategies and a complex social
organisation.
Homo sapiens
100,000
In search of new food supplies, Homo sapiens began to cross from
Africa into the Middle East. By this Late Pleistocene period, its numbers appear to have been dramatically
reduced by a lack of food stocks, perhaps to as low as 2,000
individuals (according to recent genetic research) in the main groups, which
meant that for a while Homo sapiens was perilously close to
extinction. Other, smaller groups seem to have remained in Africa.
By a strange twist of fate, the harsh conditions that caused this near
extinction may also have allowed the cultural explosion that gave rise to
human behaviour as we know it today. Professor David Goldstein, a
molecular biologist at UCL in London, has uncovered evidence to back up
the idea of a very
ancient population bottleneck. A bottleneck is an event that reduces the
genetic difference, or diversity, in a population of animals. One way this
can occur is through a catastrophe that wipes out a large proportion of a
population.
If we compare the genes of modern people from all over the
world, they are remarkably similar, suggesting that the ancestors of all
living people expanded from a small population that survived a bottleneck.
The ancient bottleneck proposed by Professor Goldstein must have occurred
in Africa, where modern humans evolved. "Our data suggests there was a
bottleneck that was not that recent," says Goldstein. The genetic data
puts the likely date for this event at just before 100,000 years ago.
It's not known what caused this bottleneck. But a plausible candidate
is emerging. By measuring the ratios of different oxygen isotopes in ice
cores, scientists can reconstruct climatic changes over time. Oxygen
isotope data suggests that between 190,000 and 130,000 years ago – a
period known as 'oxygen isotope stage 06' – Africa was drained of moisture
and became a parched wasteland, with little to sustain populations of
modern humans. "I'm not in a position to say what caused the bottleneck,
but it certainly could be a something like that (drought). That scale of
climatic change could be responsible for what we see in the genetic data,"
says Goldstein.
95,000
A tiny species of human
evolved in Indonesia at the same time as Homo sapiens was
first migrating out of Africa.
Homo floresiensis was a one-metre- (3ft) tall species which
lived on Flores Island (near Java) from between 95,000 to at least 12,000
years ago. It had long
arms and a skull the size of a large grapefruit and shared its habitat
with a golden retriever-sized rat, giant
tortoises and huge lizards - including Komodo dragons - and a pony-sized
dwarf elephant called Stegodon which floresiensis probably hunted.
Floresiensis probably evolved from
Homo erectus, whose
remains have been discovered on the Indonesian island of Java. Homo
erectus may have arrived on Flores about one million years ago,
evolving its tiny physique in the isolation provided by the island in
response to the local scarcity of resources (later influxes of Homo
sapiens appear to have evolved in the same way).
Homo sapiens reached the area by 50,000 years ago, but the last evidence of this hominid at Liang Bua dates to just before
12,000 years ago, when a volcanic eruption snuffed out much of Flores'
unique wildlife, although there are hints that floresiensis could
have lived on much later than this.
Some groups of Homo sapiens followed the coastline east from
northeastern Africa,
heading into Persia and South East Asia.
Other Homo sapiens groups settled along the Fertile
Crescent and in the south eastern corner of Anatolia. They lived alongside
tribes of Homo neanderthalis, and there was a considerable overlap
in their competition for resources which lasted for at least 30,000 years
(as proved by the discovery of Kebara, a Neanderthal fossil found in
Israel and dated to 60,000 years ago) - this was nearly five times longer
than when sapiens later reached Europe. The considerably smaller
numbers of sapiens at this time, as they moved into a land
dominated by neanderthalis probably goes a long way to explaining
this.
However, one significant drawback for Neanderthals was the fact that
their physique forced them to maintain a high calorific intake. They were
forced to hunt for food containing twice as much energy as Homo sapiens.
Once they found themselves in direct competition with increasing numbers
of Homo sapiens, their hunt successes would have been harmed,
perhaps significantly. This would certainly have had a detrimental effect on
their existence.
70,000
There may have been other bottlenecks that contributed to the
small amount of genetic diversity we see in modern humans. Professor
Stanley Ambrose of the University of Illinois at Urbana-Champaign believes
that the eruption of the volcano Toba in Sumatra at this time was
responsible for a volcanic winter that caused an instant ice age.
The large amount of sulphur thrown up into the atmosphere by the
eruption reflected sunlight away causing temperatures around the world to
plummet. Temperatures in Africa may have fallen by as much as 9°C,
creating a freeze that lasted 1,400 years.
"It was a long time, it was
unrelentingly cold," says Ambrose. But it didn't just get cold, a
temperature change of this magnitude would almost certainly have caused
another terrible drought. "Lakes dried up, the earth turned to sand. Every
year of drought was geometrically worse than the year before," adds
Ambrose.
Ambrose believes it is no coincidence that around this time, modern
humans in Africa were undergoing drastic changes in the ways they
organised their societies. The harsh climatic conditions that accompanied
the volcanic winter may have placed pressure on humans to cooperate with
each other. Small foraging groups became larger societies. Ambrose calls
this the 'troop-to-tribe transition'.
50,000
Homo sapiens first reached Australia after spreading slowly
through South Asia and Sunda-land. Lowered sea levels had created a
landbridge which meant that the South Asian islands were joined together
above sea level as far south as Java.
But the peopling of Australia was a long-term process involving
numerous subsequent movements of people out from Asia. Two routes were
possible: one from Southern China through the Philippines and into New
Guinea, the second from South East Asia through the islands of Indonesia
and into Northern Australia.
Although the frequent lowering of sea levels during Ice Ages caused
the Sunda shelf to become fully exposed, and the same thing happened to
the Sahul shelf - comprising Australia, New Guinea and Tasmania -
the two were never linked. Both of the colonisation routes therefore
required a sea journey of at least 60 kilometres of open sea, so sea-going
craft would have been essential. What these groups of Homo sapiens
used for this so far remains unknown.
Settlement in Sahul-land expanded rapidly, with the southern and
eastern areas becoming fully occupied within 25,000 years. During this
time the environment changed quite dramatically, becoming increasingly dry
and reaching a peak of aridity 18,000 to 16,000 years ago, followed by a
slight improvement in conditions. The same dramatic changes brought about
the extinction of the giant marsupials at the end of this period.
After 40,000 years of Homo sapiens settlement on on Sahul-land,
rising sea levels cut off New Guinea and Tasmania, and covered the rich
coastal sites. This was simultaneous with the appearance of another
variety of human type in Australia, fully modern but with a heavy robust
skull. These individuals may be a later wave of immigrants, but it is also
possible that they are the result of local breeding effects on a small
community.
Homo erectus was still in existence in Java, but probably not
for long.
Recent studies into the complicated stratigraphy of the Java Homo
erectus sites have revealed some surprising information. Researchers
have dated the deposits thought to contain erectus fossils near the
Solo River in Java to only 50,000 years ago. This would mean that at least
one population of Homo erectus in Java was a contemporary of
Homo sapiens.
The two species had some level of direct contact, as is proven by the
distribution of lice. Lice have stuck with hominids and their primate
ancestors for at least 20 million years, and their lineages are remarkably
close to those of the hominids. The distribution of lice around the world
proves that there was either some interbreeding on a limited scale between
erectus and sapiens, or sapiens hunted erectus
for food and the lice were transmitted during the process of
preparing the meat. This very individual strain of lice (found only in the
Americas) was then carried by sapiens as they headed northwards
towards Beringia. The first wave of humans arrived there around 48,000
years ago.
Homo erectus may have held on in Java for another 20,000 years
before it died out totally.
Something happened that transformed the world of Homo neanderthalis,
especially in Europe. There was a sudden change in the weather. The climate in Europe
began to deteriorate significantly, getting
colder and drier. Although this had happened before, during other gaps
between Ice Ages, this was different. The
changes were more rapid, and very unsettled, with no particular pattern
emerging.
And they were simply getting worse and worse.
Neanderthals were
built to survive the cold, but the speed of this climate change was
different to anything they had experienced before. These changes were not
happening at a scale of thousands of years, sometimes they were at a scale
of tens of years or hundreds of years, within the space of a few
Neanderthal generations.
They faced a crisis of survival. The
forests in which they lived were dying out because of the weather. And in
this new, more open landscape, they would have found it increasingly
difficult to hunt. Neanderthal hunting methods - on the edge of woodland
where their prey wouldn't see them coming - just wouldn't work so well on open
step land environments because the size and weight of their heavy spears
made them almost useless for throwing any distance.
40,000
Homo sapiens' 'troop-to-tribe' transition seems to have involved systems of gift
exchange between distant peoples. Beads made out of ostrich eggshell seem
to have been important items in this system of gift-giving, as they are
today amongst South African !Kung San hunter-gatherers.
The earliest
examples of these beads have been dated to 40,000 years old. These beads
were exchanged over areas of 200km in order to secure future favours when
times became tough. In this way, humans increased the likelihood of
survival or 'spread the risk of survival'. Gift-giving was a key activity of early modern humans, as it is today.
Another important innovation after 70,000 years ago is the invention
of a stone tool technology called 'microliths' in Africa. Microliths are
small flakes and blades that characterise the Later Stone Age in Africa.
These tools are very diverse, because each was specialised for a task.
Ambrose describes previous stone technologies as jack-of-all-trades
(master of none) toolkits, whereas microliths reflect modern humans using
the right tool for the job.
At the same time, Homo sapiens first emerged into Europe and began to compete with the
indigenous Homo neanderthalis population for food and resources.
Neanderthals were already facing problems from abrupt climate change, so
when the first Homo sapiens arrived in northern Europe with their
new technology - a much lighter spear that could be thrown - Neanderthals
were hit again with the blow of being out-hunted.
In fact, it could have
been Neanderthal's loss of dominance in Europe that opened the door for
Homo sapiens to begin moving west from Anatolia and competing directly
with them. Homo sapiens was established across all of habitable
Europe within 5,000 years.
24,000
What characterised all Neanderthals was their extraordinarily short
lower limbs, built for power but not so good for speed or long distance
running. They also had a pelvis that itself was extraordinarily broad.
This meant that the pelvis was not going to be as bio-mechanically
efficient in long distance locomotion as that of Homo sapiens.
It seems that the very features that made Neanderthal perfectly
adapted to the rigours of the Ice Age had also locked him into an
evolutionary dead end. Homo sapiens may not have been adapted to
the cold, but they were tailor made for the open plains. They were better
able to exploit the open spaces, the step land habitats that were
expanding in Ice Age Europe. And as the forest retreated, the Neanderthals
retreated along with them.
Unable to survive in the open Neanderthals could only have clung on in
ever decreasing woodland refuges. And as their habitat collapsed around
them their population fell.
The effect seems to be that the populations that were once closely
connected across Europe began to get fragmented and scattered. There came
a point at which these populations were no longer viable and the
Neanderthals became extinct, with their last communities on the western edges
of Europe, in modern Portugal, disappearing.
A new wave of Homo sapiens crossed the frozen Baring Straits -
Beringia - and entered the Americas. This species was now the most
successful ever, having colonised and thrived on all six habitable
continents and out-competed all related Homo species.