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Many different creatures contribute to bioturbation, and many different
forces (besides biological ones) contribute to the mixing of the soil.
As an overall term, Pedoturbation encompasses all different types of soil
mixing (ped = soil; soil science is termed Pedology).
Bioturbation means specifically the mixing of the soil through biological
means. This can be further divided into Floralturbation (mixing through
plants) and Faunalturbation (mixing through animals).
Other types of pedoturbation include cryoturbation, which is the mixing
of soil through freezing and thawing, and even seismoturbation, the mixing
of soil through earthquakes.
Below is a gallery of some interesting and unusual forms of soil turbation,
particularly as they relate to archaeology. If you have other material
you think would be appropriate to post here, feel free to send it along!
(ggvogel@gmail.com).
Click each image for a larger version.
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Jeff Homburg (an archaeologist and soil scientist
at Statistical Research,
Inc.) sent this poster about western harvester ants and
their affects on the soil. Click on the poster thumbnail for
a full version in PDF format.

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Western harvester ants
(Pogonomyrmex occidentalis) are widespread in the Western U.S.,
and because of their large size, large colonies, and high levels
of activity, they are significant agents of bioturbation and
nutrient cycling, as well as an important biotic factor in soil
formation. Harvesters, in fact, transport more sediment in the
Western U.S. than any organism but humans, so they can have
an enormous effect on the bioturbation of archaeological deposits.
This poster, which was presented by Jeffrey Homburg and Jonathan
Sandor at the 1999 meeting of the Soil Science Society of America
in Baltimore, shows how these ants affect physical, chemical,
and micromorphological soil properties. Research on the rate
at which harvesters turnover the soil in cultivated, uncultivated,
and fallow fields is also presented. |
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Crayfish chimney from the Spiro archaeological site in eastern
Oklahoma - the mud was ejected as a burrow was formed. I have
seen crayfish burrows extend more than 2 meters deep at archaeological
sites. I once read that crayfish feed mostly at night and crawl
into burrows in the morning, and that they use the first empty
crayfish burrow they find, only digging a new one if they have
to. Musical burrows!
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Armadillo dig from Northwest Arkansas. Armadillos dig into the
soil with their front claws to get at grubs and other bugs. These
diggings aren't usually very deep, but can be numerous in an area
with lots of armadillos. They also use their snouts to "plow"
through leaf layers looking for bugs to eat, and I've seen them
waddling backwards scooping up leaves in their arms to take back
to their dens.
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This is a tiny path in the desert soil of Buckeye Hills Recreation
Area south of Tempe, Arizona. Notice that the pebbles have all
been cleared and the path itself is composed mostly of sand. These
little paths criss-crossed much of the desert, running from one
bush to the next. I'm not sure what made them - probably a rodent,
or maybe lizards?
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Killdeer are ground-nesting birds that dig small depressions
and line them with twigs and stones. In this case, the nest is
lined with artifacts from a prehistoric archaeological site -
including scrapers (stone tools used in processing wood and hides),
and flakes (chips left over from stone-tool making). This photo
was taken by Adam Newman of the Iowa Office of the State Archaeologist
in Missouri near I-70.
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Bill Whittaker is an archaeologist with the Iowa Office of the
State Archaeologist. Here he has his leg in a hollow tree stump,
on top of a prehistoric mound at Effigy Mounds National Monument.
When the stump rots away completely, it may look like a looter's
hole in the mound. Bill Whittaker and Glen Story wrote a publication
on factors that can create false mounds or cause depressions in
mounds (listed on the technical articles page here).
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Frost pillars pushing up particles of soil. The pillars are tiny
(about 3 cm tall), but over time they can significantly alter
the top layer of soil. This picture was taken near West Fork,
Arkansas, where it doesn't frost very often. The hill slopes have
lots of exposed soil, though, so frost pillars are able to move
soil more easily than in areas with thick vegetation.
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This is a prehistoric spear point I found on an archaeological
survey along the Alaska Peninsula just north of Kodiak Island.
Bears dig into the tundra to get at roots and berries, and we
found them to be very useful for looking beneath the moss of the
tundra without further disturbing the vegetation.
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A somewhat unusual form of bioturbation: sailfin catfish burrowing
several meters into the shoreline in south Florida. Story from
"Off the beaten path" compilation by Trey Reid, Arkansas Democrat
Gazette, Sept. 27, 2001.
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This is a gravestone in Evergreen
Cemetery in Fayetteville, Arkansas. It was set flush with
the ground in 1982 or later, and by the time this picture was
taken (2004), it had already been partially buried through bioturbation.
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Another gravestone from Evergreen
Cemetery, this one dating to the 1870s. It is broken, and
the lower portions had been completely buried through bioturbation.
A footstone to a different burial was buried too, about 30 centimeters
beneath the ground surface. The "sinking" of older monuments is
a common problem at many cemeteries.
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Tree throw at Fort Harrison State Park, Indianapolis Indiana.
Trees can move a great deal of soil when they fall over, bringing
material up with their roots and leaving a deep pit below. This
creates 'pit and mound' topography in many forested areas. It
can mix artifacts in the upper portion of the soil, and create
features that mimic prehistoric storage pits.
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Saguaro cactus throw in Arizona. The dynamics of cactus throws
are similar to tree throws, but the amount of soil moved is much
smaller. Notice also that there is a ring of larger stones right
at the base of the cactus - these appear to have been pushed out
of the way as the cactus grew. Will this look like a fire ring
when the remains of the cactus are completely gone?
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Strips of cleared forest floor at Fort Harrison State Park, Indianapolis
Indiana. Tree falls, burrowing mammals, and other factors are
evident in the irregular surface of the bare soil. High School
students cleared all forest debris from the soil as part of a
large surface collection in Martin University's Next Step Education
Through Archaeology Program (NSEAP).
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