About
Metasequoia occidentalis (Dawn Redwood): These beautiful
Metasequoia plant fossils come from the lacustrine deposits of
the McAbee Flora of the Eocene of British Columbia, Canada. Note
the fine preservational details. During the Eocene, the region
was dominated by a shallow lake. Plant matter which fell into
the water was covered with a fine layer of silt which built up
over the years as a result of deposition of diatoms which bloomed
in the lake each spring and died in the summer. The Dawn Redwood
(Metasequoia) is a genus that was first discovered in Korea over
60 years ago. The first living specimens were discovered in central
China in 1944; Dawn Redwood is considered a living fossil. The
flora of the region during the Eocene was dominated by conifers
farther away from the lake, and elm, birch, beech, and alder near
to the lakeshore.
Metasequoia
fossils are known from many areas in the Northern Hemisphere;
over 20 fossil species have been named, but are now treated in
just three species, M. foxii, M. milleri, and M. occidentalis
(Farjon 2005). During the Paleocene-Eocene Thermal Maximum, extensive
forests of Metasequoia occurred as far north as Axel Heiberg Island
(northern Canada) at around 80°N latitude. Large petrified
trunks and stumps of the extinct Metasequoia occidentalis also
make up the major portion of Tertiary fossil plant material in
the badlands of western North Dakota in the United States.
|