life
-> death -> preservation -> survival
-> discovery
What is Petrification?
Before
petrification can begin, there has to be plenty of wood near a water source,
an event occurs, and the trees are knocked over, usually into the water
source. Most of the time that event is a volcanic eruption. To ensure petrification
the wood is saturated with water, and eventually, as the wood moves downstream,
it becomes bunched together and buried by mud, silt, and ash. The logs
that have traveled downstream now need to become buried by mud and sediment,
as well as being covered with some of the ash from the volcanic eruption. Petrification
occurs by the replacement, recrystallization or permineralization of the
original plant. (Permineralization just means that mineral material fills
in the voids of the fossil-to-be rather than replacing or recrystallizing
the original materials).In almost
every case, ground water is the agent that causes petrification and silica
and calcite are the main replacing minerals.
What are the Variables Involved in
Petrification?
In
1906 Professor Wieland created a theory on the petrification process of
wood based on five variables:
1.The
tissue systems of the plant
2. Temperature
3. Minerals
necessary for the process of silification or calcification
4.Duration
of chemical activity
5.The
nature of the embedding rock material
The
mineralization of the entire plant is first conditional on the tissue system,
which is reliant on the state of growth, prefoliation, and preflorations
of the plant species.Temperature,
the surrounding sediments, and the abundance and type of minerals facilitate
the petrification process.
Altered Remains (changed structural and/or chemically)
How
long it takes for petrification to occur depends on factors such as pH
and temperature, but all things being equal, groundwater saturated with
calcium carbonate (calcite) acts the fastest because calcite is more soluble
than silica or other petrifying minerals. So if we accept the fact that
petrification occurs as a continuum (in other words, a gradual process
from partial to complete replacment/recrystallization/permineralization)
Under ideal chemical conditions, petrification is possible in a few hundred
years or even less.The tree must
be sealed from oxygen to prevent decay. if it is not sealed bacteria will
usually decompose the wood.
To
demonstrate the process of petrification using everyday objects.
Materials
Activity
Worksheet
Small pieces of wood, such as 4 cm long sections of small dowels, or
similarly sized fresh twigs
5-10 lbs of playground sand
Food coloring (at least two colors)
Plastic wrap
6 small clear plastic cups
6 rubber bands
1 stirring rod or 1 popcicle stick
Water (at room temperature)
Introduction
This
experiment will model the process of petrification. While performing the
experiment, try to think of the natural processes that the experiment is
modeling. Before performing the experiment, read the instructions and predict
what you think your results will be. Record your thoughts in the section
marked "Prediction" on your worksheet.
Instructions
- clay instead of sand
- temperature of water
- old chicken bone instead of wood
- salinity of water
- piece of plastic instead of wood
Before you begin, tell what you think will happen.
Investigation
2. What part of natural petrification does the food coloring represent
in this experiment?
3. Why were the cups covered with plastic wrap and a rubber band?
4. How would real petrified wood be different from the petrified wood
that you created in the experiment? Why?
5. Explain the importance of the presence of water for petrification
to occur.
1. What physical characteristics of the wood have changed? How did
these changes occur?