Tree rings are frozen environmental records. Unlike many
other historical data that are averaged over decades or even centuries, tree
rings grow in distinct individual annual segments. These segments are
indicative of the environment the tree experienced during a specific year. In
general, more favorable conditions of moisture and length of the growing season
result in wider rings. Tree rings of multiple trees growing nearby are closely
correlated, and their ages can be cross-correlated with carbon-14 dating
techniques; tree rings can be tied to specific years.
It has recently been discovered that rings from cedar trees
grown on Japan’s Yakushima island show an unusually high content of the
carbon-14 isotope in rings formed in the late 8th century. Carbon-14 in rings
from a specific year (775 AD) jumped 12% from the prior year, which is 20 times
the normal variability of C-14 due to solar modulation. High C-14 levels have
been found in contemporaneous samples of European and North American forests. The
high C-14 levels are believed to have been caused by an extremely intense burst
of radiation, still of unknown origin.
Studies of arboreal growth patterns are important for the determination of climate history as well as of the impact of cosmic events on life on Earth.
Studies of arboreal growth patterns are important for the determination of climate history as well as of the impact of cosmic events on life on Earth.
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