"The recent dating of the Siberian trap volcanoes to be contemporaneous with
the end-Permian extinction suggests that they were the trigger for the
environmental events that caused the extinctions," says Lee R. Kump, professor
of geosciences. "But the warming caused by these volcanoes through carbon
dioxide emissions would not be large enough to cause mass extinctions by
itself."
That warming, however, could set off a series of events that led to mass
extinction. During the end-Permian extinction 95 percent of all species on Earth
became extinct, compared to only 75 percent during the K-T when a large asteroid
apparently caused the dinosaurs to disappear.
Volcanic carbon dioxide would cause atmospheric warming that would, in turn,
warm surface ocean water. Normally, the deep ocean gets its oxygen from the
atmosphere at the poles. Cold water there soaks up oxygen from the air and
because cold water is dense, it sinks and slowly moves equator-ward, taking
oxygen with it. The warmer the water, the less oxygen can dissolve and the
slower the water sinks and moves toward the equator.
“Warmer water slows the conveyer belt and brings less oxygen to the deep
oceans,” says Kump.
The constant rain of organic debris produced by marine plants and animals,
needs oxygen to decompose. With less oxygen, fewer organics are aerobically
consumed.
"Today, there are not enough organics in the oceans to go anoxic," says Kump.
"But in the Permian, if the warming from the volcanic carbon dioxide decreased
oceanic oxygen, especially if atmospheric oxygen levels were lower, the oceans
would be depleted of oxygen."
Once the oxygen is gone, the oceans become the realm of bacteria that obtain
their oxygen from sulfur oxide compounds. These bacteria strip oxygen from the
compounds and produce hydrogen sulfide. Hydrogen sulfide kills aerobic
organisms.
Humans can smell hydrogen sulfide gas, the smell of rotten cabbage, in the
parts per trillion range. In the deeps of the Black Sea today, hydrogen sulfide
exists at about 200 parts per million. This is a toxic brew in which any
aerobic, oxygen-needing organism would die. For the Black Sea, the hydrogen
sulfide stays in the depths because our rich oxygen atmosphere mixes in the top
layer of water and controls the diffusion of hydrogen sulfide upwards.
In the end-Permian, as the levels of atmospheric oxygen fell and the levels
of hydrogen sulfide and carbon dioxide rose, the upper levels of the oceans
could have become rich in hydrogen sulfide catastrophically. This would kill
most the oceanic plants and animals. The hydrogen sulfide dispersing in the
atmosphere would kill most terrestrial life.
"A hydrogen sulfide atmosphere fits the extinction better than one enriched
in carbon dioxide," says Kump. "Carbon dioxide would have a profound effect on
marine life, but terrestrial plants thrive on carbon dioxide, yet they are
included in the extinction."
Another piece in the puzzle surrounding this extinction is that hydrogen
sulfide gas destroys the ozone layer. Recently, Dr. Henk Visscher of Utrecht
University and his colleagues suggested that there are fossil spores from the
end-Permian that show deformities that researchers suspect were caused by ultra
violet light.
"These deformities fit the idea that the ozone layer was damaged, letting in
more ultra violet," says Kump.
Once this process is underway, methane produced in the ample swamps of this
time period has little in the atmosphere to destroy it. The atmosphere becomes
one of hydrogen sulfide, methane and ultra violet radiation.
The Penn State researcher and his colleagues are looking for biomarkers,
indications of photosynthetic sulfur bacteria in deep-sea sediments to
complement such biomarkers recently reported in shallow water sediments of this
age by Kliti Grice, Curtin University of Technology, Australia, and colleagues
in the Feb. 4 issue of the journal, Science. These bacteria live in places where
no oxygen exists, but there is some sunlight. They would have been in their
heyday in the end-Permian. Finding evidence of green sulfur bacteria would
provide evidence for hydrogen sulfide as the cause of the mass extinctions.