Imagine a year in Africa that
summer never arrives. The sky takes on a gray hue during the day and
glows red at night. Flowers do not bloom. Trees die in the winter. Large
mammals like antelope become thin, starve and provide little fat to the
predators (carnivores and human hunters) that depend on them. Then,
this same disheartening cycle repeats itself, year after year. This is a
picture of life on earth after the eruption of the super-volcano, Mount
Toba in Indonesia, about 74,000 years ago. In a paper published this
week in
Nature, scientists show that early modern humans on the coast of South Africa thrived through this event.
An eruption a hundred times smaller than Mount Toba - that of
Mount Tambora, also in Indonesia, in 1815 - is thought to have been
responsible for a year without summer in 1816. The impact on the human
population was dire - crop failures in Eurasia and North America, famine
and mass migrations. The effect of Mount Toba, a super-volcano that
dwarfs even the massive Yellowstone eruptions of the deeper past, would
have had a much larger, and longer-felt, impact on people around the
globe.
The scale of the ash-fall alone attests to the magnitude of the
environmental disaster. Huge quantities of aerosols injected high into
the atmosphere would have severely diminished sunlight - with estimates
ranging from a 25 to 90 percent reduction in light. Under these
conditions, plant die-off is predictable, and there is evidence of
significant drying, wildfires and plant community change in East Africa
just after the Toba eruption.
If Mount Tambora created such devastation over a full year - and
Tambora was a hiccup compared to Toba - we can imagine a worldwide
catastrophe with the Toba eruption, an event lasting several years and
pushing life to the brink of extinctions.
In Indonesia, the source of the destruction would have been
evident to terrified witnesses - just before they died. However, as a
family of hunter-gatherers in Africa 74,000 years ago, you would have
had no clue as to the reason for the sudden and devastating change in
the weather. Famine sets in and the very young and old die. Your social
groups are devastated, and your society is on the brink of collapse.
The effect of the Toba eruption would have certainly impacted
some ecosystems more than others, possibly creating areas - called
refugia - in which some human groups did better than others throughout
the event. Whether or not your group lived in such a refuge would have
largely depended on the type of resources available. Coastal resources,
like shellfish, are highly nutritious and less susceptible to the
eruption than the plants and animals of inland areas.
When the column of fire, smoke and debris blasted out the top of
Mount Toba, it spewed rock, gas and tiny microscopic pieces
(cryptotephra) of glass that, under a microscope, have a characteristic
hook shape produced when the glass fractures across a bubble. Pumped
into the atmosphere, these invisible fragments spread across the world.
Panagiotis (Takis) Karkanas, director of the Malcolm H. Wiener
Laboratory for Archaeological Science, American School of Classical
Studies, Greece, saw a single shard of this explosion under a microscope
in a slice of archaeological sediment encased in resin.
"It was one shard particle out of millions of other mineral
particles that I was investigating. But it was there, and it couldn't be
anything else," says Karkanas.
The shard came from an archaeological site in a rockshelter
called Pinnacle Point 5-6, on the south coast of South Africa near the
town of Mossel Bay. The sediments dated to about 74,000 years ago.
"Takis and I had discussed the potential of finding the Toba
shards in the sediments of our archaeological site, and with his eagle
eye, he found one," explains Curtis W. Marean, project director of the
Pinnacle Point excavations. Marean is the associate director of the
Institute of Human Origins at Arizona State University and honorary
professor at the Centre for Coastal Palaeoscience at Nelson Mandela
University, South Africa.
Marean showed the shard image to Eugene Smith, a volcanologist
with the University of Nevada at Las Vegas, and Smith confirmed it was a
volcanic shard.
"The Pinnacle Point study brought me back to the study of glass shards from my master's thesis 40 years earlier," says Smith.
Early in the study, the team brought in expert cryptotephra
scientist Christine Lane who trained graduate student Amber Ciravolo in
the needed techniques. Racheal Johnsen later joined Ciravalo as lab
manager and developed new techniques.
From scratch, with National Science Foundation support, they
developed the Cryptotephra Laboratory for Archaeological and Geological
Research, which is now involved in projects not only in Africa, but in
Italy, Nevada and Utah.
Encased in that shard of volcanic glass is a distinct chemical
signature, a fingerprint that scientists can use to trace to the killer
eruption. In their paper in
Nature, the team describes finding
these shards in two archaeological sites in coastal South Africa,
tracing those shards to Toba through chemical fingerprinting and
documenting a continuous human occupation across the volcanic event.
"Many previous studies have tried to test the hypothesis that
Toba devastated human populations," Marean notes. "But they have failed
because they have been unable to present definitive evidence linking a
human occupation to the exact moment of the event."
Most studies have looked at whether or not Toba caused
environmental change. It did, but such studies lack the archaeological
data needed to show how Toba affected humans.
The Pinnacle Point team has been at the forefront of development
and application of highly advanced archaeological techniques. They
measure everything on site to millimetric accuracy with a "total
station," a laser-measurement device integrated to handheld computers
for precise and error-free recording.
Naomi Cleghorn with the University of Texas at Arlington, recorded the Pinnacle Point samples as they were removed.
Cleghorn explains, "We collected a long column of samples -
digging out a small amount of sediment from the wall of our previous
excavation. Each time we collected a sample, we shot its position with
the total station. We could then precisely compare the position of the
sample to our excavated cultural remains - the trash ancient humans left
at the site. We could also compare our cryptotephra sample position
with that of samples taken for dating and environmental analyses."
In addition to understanding how Toba affected humans in this
region, the study has other important implications for archaeological
dating techniques. Archaeological dates at these age ranges are
imprecise - 10 percent (or 1000s of years) error is typical. Toba
ash-fall, however, was a very quick event that has been precisely dated.
The time of shard deposition was likely about two weeks in duration -
instantaneous in geological terms.
"We found the shards at two sites," explains Marean. "The
Pinnacle Point rockshelter (where people lived, ate, worked and slept)
and an open air site about 10 kilometers away called Vleesbaai. This
latter site is where a group of people, possibly members of the same
group as those at Pinnacle Point, sat in a small circle and made stone
tools. Finding the shards at both sites allows us to link these two
records at almost the same moment in time."
Not only that, but the shard location allows the scientists to
provide an independent test of the age of the site estimated by other
techniques. People lived at the Pinnacle Point 5-6 site from 90,000 to
50,000 years ago. Zenobia Jacobs with the University of Wollongong,
Australia, used optically stimulated luminescence (OSL) to date 90
samples and develop a model of the age of all the layers. OSL dates the
last time individual sand grains were exposed to light.
"There has been some debate over the accuracy of OSL dating, but
Jacobs' age model dated the layers where we found the Toba shards to
about 74,000 years ago - right on the money," says Marean. This lends
very strong support to Jacobs' cutting-edge approach to OSL dating,
which she has applied to sites across southern Africa and the world.
"OSL dating is the workhorse method for construction of timelines
for a large part of our own history. Testing whether the clock ticks at
the correct rate is important. So getting this degree of confirmation
is pleasing," says Jacobs.
In the 1990s, scientists began arguing that this eruption of
Mount Toba, the most powerful in the last two million years, caused a
long-lived volcanic winter that may have devastated the ecosystems of
the world and caused widespread population crashes, perhaps even a
near-extinction event in our own lineage, a so-called bottleneck.
This study shows that along the food-rich coastline of southern
Africa, people thrived through this mega-eruption, perhaps because of
the uniquely rich food regime on this coastline. Now other research
teams can take the new and advanced methods developed in this study and
apply them to their sites elsewhere in Africa so researchers can see if
this was the only population that made it through these devastating
times.