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Interview: Helen F. James, Smithsonian Institution |
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Q: What was the chief role of humans in causing extinctions?
HJ: My particular focus is on island
extinctions. There have been a tremendous number of these,
and they're ongoing. They're occurring as we speak.
Looking specifically at these island extinctions,
the chief role of humans was alteration to habitat -- the removal
of the essential factors in the environment that the species needed
to survive. Change in the fire regime has been important in many
of the island extinctions. Tremendous population growth on certain
islands in prehistoric times led to overexploitation of
resources for the human population. This was absolutely necessary
to maintain the population, but perhaps actually depleted resources
in the environment, so that the human population itself began
to collapse in numbers. At that stage, I think there was
a real crisis -- and this is when probably most of the island
extinctions occurred.
In Hawaii, where
I have done most of my research, we estimate that maybe as high
as 90% of the native vertebrates have indeed gone extinct, or
are imminently threatened with extinction. So we need to have had major changes
in the environment to cause this kind of extinction. Another
way in which island extinctions have differed from continental
extinctions is that many small animals have become extinct on
islands. On continents, the human-era extinctions mainly involve
large animals. It's very difficult for Stone Age people to hunt
a small, abundant animal to extinction. Populations of widespread
and abundant island animals would simply not be wiped out by using
what the prehistoric Hawaiians had available to them as far as
hunting: bird lime, bird nets, and so forth. The technology
was insufficient to wipe out small animal populations. So I think
that drastic environmental perturbations were required in order
to cause as much extinction as we've actually observed.
Q: What is the relevance of prehistoric extinctions to
our current biodiversity concerns?
HJ: One of our big societal concerns
about biodiversity and about the environment at the current time
is that we are transforming biodiversity reserves on continents
into what are essentially habitat archipelagos. As we convert
more and more land -- either for industry or agriculture, or simply
for human settlement -- the biodiversity that we have on continents
is being restricted to reserves of habitat, which are essentially
islands within continents. If we look at the history of humans
on islands, as prehistoric humans arrived on and colonized islands,
a major biodiversity crisis ensued, and this happened all around
the world. Many people don't realize that the biodiversity crisis
dates back to biblical times and before. Around 2,000 years ago,
when the aboriginal Polynesians arrived in Hawaii, over half of
the native species of birds became extinct -- and this story is
repeated all over the world on islands. Looking at the island record
teaches us to be very concerned that all of our worries are
justified, as far as conservation of biodiversity on habitat
archipelagos, on continents. If we don't thoroughly investigate
and try to learn from the island record, perhaps we will
be just as poor managers of habitat archipelagos on continents
as our predecessors were on islands.
Q: How would you convince skeptics that extinction
rates are indeed high?
HJ: I would respond to that by
exhibiting the actual hard evidence, the bone evidence,
that many creatures have disappeared very recently. There is
a long geological record of past life, and it's been studied for
hundreds of years now. So we can document that many creatures
have appeared on earth, and there have been periods of major extinctions.
Looking at the most recent geological
past, the Late Pleistocene -- in other words, the last ice age
-- and our current epoch, the Holocene -- the last 10,000 years
-- I would bring forth the actual bone evidence of many creatures
that were widespread and abundant, and have simply vanished
during the human era. On islands, I could show you bones of 200
species of birds that are no longer with us and have disappeared
in the last 5,000 years or less This is a very high extinction
rate, comparatively, with what has been recorded through most
of the history of life. I think that the hard evidence is before
us, and we have to accept that extinction rates are extremely
high.
Q: Were there any facts from the symposium that would
lead you to change your mind about how these extinctions in prehistoric
times began?
HJ: I would say that I gained a wonderful
appreciation for the complexity of the problem, and I really thoroughly
enjoyed hearing the viewpoint and seeing the evidence that my
colleagues presented. In particular, I enjoyed the viewpoint of
Norman Owen-Smith, who, using modern African ecosystems
as an analog for the Pleistocene of North America, explained
the relationships of large herbivores to other animals -- that
large herbivores can transform the environment in such a way that
other animals may be dependent for their existence on the presence
of those large herbivores. And I think there are many possibilities
for interactions in what we might call the "complex ecological
web" that could have contributed to the extinctions.
Q: You seem to have evidence that extinctions
in small places could be protracted. Does this need to be considered in
more detail by others?
HJ: The radiocarbon record is always
extremely important to the study of these extinctions, and it's
very instructive because it contests some of our preconceptions
or hypotheses. In the Hawaiian instance, as we have
gone and dated the actual bones of extinct animals, we have found
that there may have been a period of perhaps a thousand years
of human coexistence with the animals before even the most vulnerable
species disappeared. That has changed my concept of what
caused the extinctions. The idea of first
contact with a naïve fauna is one that I have left
behind in my thinking, because of the radiocarbon evidence. It
has turned my thoughts toward what happens with human populations,
and how they transform the environment. The human population
in Hawaii was free of many of the diseases that control human
populations elsewhere. There were more people living on each Hawaiian island -- except
for the island of Oahu, where Honolulu is -- at the time that
Captain Cook arrived in 1778 than are living there
now. These people were not trucking in vegetables from California.
They were living off local resources -- terrestrial and marine resources.
So there was a period of population crisis
that the archeologists have recorded. It led to warfare, and
it probably led to human population decline. It led to the organization
of state societies and consolidation of power through warfare.
It had large implications for the human population, and I think
that it may have had large implications for animal populations --
because, at this time, the aboriginal Hawaiians had to expand their
agriculture into marginal areas of the islands. They dispersed across
the islands to areas that had not been settled before. Suddenly animal populations were
in contact with humans much more than before. They
were in contact with disease associated with human settlement;
in contact with introduced domesticated animals that the Polynesians
brought with them. Every kind of pressure on Hawaiian natural
populations would have increased during this period of human population expansion.
It's at that point that the major extinction
could have been precipitated. And I think that could be a very
important insight into understanding human-caused extinctions
on islands and elsewhere. It could really have applications
to our concerns about continental species, as well -- that it
may require real contact with a human settlement before
you begin to get extinctions, especially of the abundant
small populations. presentation | abstract
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