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RARE
LARGE JURASSIC DACTYLIOCERAS AMMONITE ON LITHOGRAPHIC LIMESTONE
SLAB FROM SOLNHOFEN
Solnhofen Plattenkalk
Formation - Eichstatt, Germany
JURASSIC
PERIOD (OXFORDIAN AGE): 161.2 - 155 million years ago Famous
for producing an astonishing diversity of rare and most intricately
preserved fossils found anywhere in the world, the Jurassic lithographic
limestone deposits of southern Germany are legendary. Quarries in
the region are privately held and mostly worked by hand on a small
scale. The finest grade fossils are few and far between and much
rock must be split to locate them. The best fossils are most often
kept by the quarry owners who themselves, are often collectors.
Some quarries are operated on a large scale but these are now dug with
machinery instead of manual labor. Because of this the rock is
damaged and along with it, the rare fossils. What all this means
today is that even fewer fine grade Solnhofen fossils are found and when
they are, rarely do the best pieces make it to market.
Occasionally, an old private collection surfaces and specimens are sold
or traded. This is where the rare opportunity comes along to
acquire a specimen on a level that truly is a prize find.
Typically, the older material is often the best as it was collected when
the deposits were first being worked and quality was in greater
abundance.
This
is an Oxfordian Age Jurassic ammonite fossil of the species
Dactylioceras. Not only is this a rare ammonite from
Solnhofen, it is an extremely attractive specimen of sizeable
proportions. The limestone plate it is on is a very large and
with beautiful varying bands of natural golden tones adding to its overall aesthetics.
The outer chamber ridges can be seen protruding up off the rock.
This is NOT a negative impression but an actual outward-protruding
fossil specimen. Visible is superb delicate detail of the centrum and whorls with a defined
end of the shell. Ammonites are not rare in the fossil record but
examples from the famous Solnhofen deposits are and you seldom can find
them on the marketplace as you see from other deposits. A
perfect piece for advanced collections of unique specimens.
NO RESTORATION, FABRICATION. Very
highly recommended!!!
Ammonites
are extinct members of the Cephalopod class.
Modern members include nautilus, squid and octopus.
They first appeared during the Silurian Period (435 million to
410 million years ago) and were abundant and widespread in the seas of
the Jurassic and Cretaceous periods (175 million to 65 million years
ago). Ammonites are important index
fossils—that is, they often link the rock layer in which they
are found to specific geological time periods.
Ammonites varied greatly in size.
The largest
known
as small
as 2 cm (0.75 in) in diameter. During the Jurassic and Cretaceous
periods, ammonites evolved more streamlined shells for swimming and the
structure of the shell became stronger. Different shell shapes emerged
as well, such as snail-like or uncoiled.
The shells of
ammonites
had hollow chambers separated by walls called septa. A tube called the siphuncle,
connected the body with the
chambers allowing the animal to fill them with water or air, changing
its buoyancy in order to rise or drop in the ocean.
Only
the last and largest chamber was occupied by the living animal.
Ammonites
probably lived for one to six years, with the majority living two to
four years. They fed on plankton (tiny free-floating organisms), sea
lilies, and smaller
orthoceras. Although many fed off the ocean floor, others may have
caught plankton while floating or swimming via jet propulsion,
expelling water through a funnel-like opening to propel themselves in
the opposite direction.
Because ammonites lived
exclusively in marine environments, their presence also indicates the
location of prehistoric seas.
RARE,
LARGE EXAMPLE THAT IS EQUALLY AESTHETIC WITH FINE NATURAL CHAMBER AND
WHORL DETAIL!
17.25"
x 11.75" overall with ammonite 4.25" across
$395
AMX206 INCLUDES
STAND
Actual Item - One
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