This
is yet another form of stromatolite that is at once beautiful
and has interesting scientific characteristics. It derives its
name, Brecciated Basal, from the fact that it originates at the
base (Basal) of a large overlaying stromatolite structure. Brecciated
(angularly broken) signified that, in fact, the original stromatolitic
structures were shattered into irregular shapes, probably in a
surf, and were then buried under the stromatolite colonies that
subsequently grew above. Mineral replacement has been hard at
work with a bluish gray silica predominating, making for an attractive
creation through the interaction of biology and chemistry. The
mineral replacement was likely formed by cold water precipitation,
resulting in the crypto crystalline (blue agate) structure that
yet retains the definitive imprints of growth of ancient microbial
mats.
A
final point of scientific interest is the age, Lower Ordovician,
some two Billion years after stromatolite reached its peak on
Earth, and during a time when stromatolite niches were disappearing
because of competing metazoan and benthic life forms. The final
major decline of stromatolite on Earth was a mere 50 million years
after this stromatolite was formed.
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