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LARGE BEAUTIFUL
EXTINCT CARBONIFEROUS SEED FERN FOSSIL FROM FRANCE -
Graissesac, France
CARBONIFEROUS
PERIOD: 320 million years ago In
a superb state of preservation and on a large and heavy block of matrix, this is an excellent
example of an extinct seed fern of the species Neuropteris.
Impressions are
highly detailed and distinct. Light brown matrix has multiple
layers of fern fossils with one complete layer and another partially
exposed beneath. Top has a crack that is not all the way through
and has been stabilized to prevent breakage. Matrix is whole and
complete.
Seed
ferns are known as Pteridospermales and belong to an extinct group of
gymnosperms. Despite their resemblance to modern ferns, seed ferns
reproduced by means of seeds. Modern ferns reproduce by means of
spores. During
the Carboniferous Period, a large portion of Europe and North America
was on the equator. The warm and consistently humid climate was
ideal for the growth of extensive swampy forests. The Paralic
Basin was the largest Carboniferous basin which comprised regions of
what are now Ireland, England, northern France, Belgium, The
Netherlands, Germany (Ruhr District) and Poland. Periodic changes
in the sea levels caused the rivers that traversed these forests to
flood, depositing massive amounts of sand and mud thereby burying the
forest along the banks. In a period of one million years, several
thousand meters of sediment would be deposited, densely packing and
pressing the abundant vegetation into flattened rock fossil
impressions. The most common vegetation in these forests were Sigillaria
and Lepidodendron. Low-lying vegetation was dominated by
seed ferns such as Neuropteris.
UNIQUE
SITE AND WELL-DEFINED SPECIMEN OF VERY HIGH QUALITY
11"
x 6" x 2" overall, plant impressions 9" in length
SOLD
PL-009 STAND INCLUDED
Actual
Item - One Only
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