Figure 1. Small echinoderm fossils in fine-grained marine limestone from the famous Jurassic fossil locality of Solnhofen in Bavaria. Species identified as a brittle star (slang-zeester in Dutch), Geocoma carinata. Sample from Stenelux of Amsterdam, Netherlands. In order to yield high contrast on this finely-detailed specimen, this photograph was made with oblique, early morning sunlight. Specimen size 100x70 mm.
Figure 2. Another sample from Solnhofen, in the historic collection of the Teyler's Museum, Haarlem, Netherlands. This sample, #5704, is identified as Saccocoma bajeri (Konig), Jura, Solnhofen. This is a pelagic, stemless crinoid.
"Rock of the Month #168, posted for June 2015" ---
Echinoderms
This month's specimen (Figure 1) is a brittle star,
an ophiuroid, part of the phylum Echinodermata.
This large marine grouping includes echinoids (sea urchins)
and crinoids (sea lilies).
The echinoderms also include stelleroids,
e.g., starfish and ophiuroids such as the Jurassic
Ophiurella (Black, 1972, p.140), also from Solnhofen.
The diversity of physical form in echinoderms is very strong,
though a five-fold symmetry is a common element, at least
in most well-preserved specimens (Black, 1972; Turek et al., 1988,
pp.360-415).
Jurassic strata in Bavaria
The Solnhofen limestone of Bavaria is noted for its extremely
fine-grained micritic ** limestone,
capable of supporting the reproduction of fine illustrations and
text (Fig. 3).
The purity and even texture that renders this the best-known
lithographic stone also makes the Solnhofen limestone a wonderful
medium for the preservation of fossils.
These strata in the drainage basin of the river Danube were laid down in
upper Jurassic time, some 150 million years ago.
Chilingar et al. (1967) edited a volume
reviewing the physical properties and
other qualities of carbonate
rocks from
many areas, including Solnhofen and sites in the U.S.A.
(Ohio, Tennessee, Pennsylvania), southern Ontario in Canada
and elsewhere.
The limestone is extraordinarily pure in bulk, but
is also known for the development of dendrites of iron and manganese
oxides across exposed surfaces (e.g., pyrolusite dendrites, in
Von Straaten, 1978; Desautels, 1968, p.48;
Chopard et al., 1991).
** Micrite is a term used in carbonate sedimentology,
referring to a very fine-grained limestone, formed from limy mud, composed of minute crystals of calcite less than 5 microns (0.005 mm) in diameter.
The Solnhofen limestone is the most famous Lagerstätten
(assemblage of superbly preserved fossils) in the world. The
oldest-known fossil bird (Archaeopteryx) was discovered here in
the late 19th century.
Archaeopteryx represents the early phase
of the very successful and long-lived aerial
reign of the pterosaurs, across Jurassic and Cretaceous times, and
six continents
(Monastersky et al., 2001).
The Teylers museum in Haarlem, Netherlands,
is an historical museum of science, and a unique showcase of late
18th century museum curation, with samples and equipment,
labels, and eclectic displays and display cabinets of wood and glass.
The exhibits include
excellent fossil fish from the Solnhofen lithographic stone.
Smaller fossils include Saccocoma from Solnhofen (viewed 17 September
2014).
The very fine-grained, uniform, platy
limestone (plattenkalk) formed during calcareous deposition in a
set of semi-isolated basins in a late Jurassic back-reef complex
(Barthel et al., 1990).
The fossils include many
genera that are but seldom preserved,
including jellyfish, crustaceans and insects.
Seilacher et al. (1985, pp.11-15) note
the unusual aspects of the Solnhofen fauna,
including fossil
birds and fossil fish, as well as pelagic crinoids (Saccocoma, a stemless
crinoid, is the most common Solnhofen fossil).
Modern echinoderms
The echinoderms are very diverse, including echinoids, crinoids, starfish and other forms. Many of the Mesozoic to Cenozoic echinoids developed tall, domed tests, though modern variants such as the sand dollars are highly flattened.
Figure 4. This modern echinoderm, a "sand dollar", displays a flattened, discoidal test (shell, or skeleton) and the five-sided (pentameral) symmetry typical of the class. Example from the Myrtle Beach area of South Carolina, on the American Atlantic seaboard (Wybourn collection). This is a keyhole urchin, Mellita quinquiesperforata.
References
Barthel,KW, Swinburne,NHM and Conway Morris,S (1990) Solnhofen: A Study in Mesozoic Palaeontology. Cambridge University Press, 236pp.
Black,RM (1972) The Elements of Palaeontology. Cambridge University Press, 339pp.
Chilingar,GV, Bissell,HJ and Fairbridge,RW (editors) (1967) Carbonate Rocks: Physical and Chemical Aspects. Elsevier, Developments in Sedimentology 9B, 413pp.
Chopard,B, Herrmann,HJ and Vicsek,T (1991) Structure and growth mechanism of mineral dendrites. Nature 353, 409-412, 03 October.
Desautels,PE (1968) The Mineral Kingdom. Ridge Press, Inc. / Madison Square Press / Grosset & Dunlap, New York, 252pp.
Monastersky,R, Blair,J and Sibbick,J (2001) Pterosaurs: lords of the ancient skies. National Geographic 199 no.5, 86-105.
Seilacher,A, Reif,W-E and Westphal,F (1985) Sedimentological, ecological and temporal patterns of fossil Lagerstätten. Phil.Trans. Royal Society London B 311, no.1148, 5-24.
Turek,V, Marek,J and Benes,J (1988) Fossils of the World: a Comprehensive Practical Guide to Collecting and Studying Fossils. Arch Cape Press, New York, 1990 edition, 495pp.
Van Straaten,LMJU (1978) Dendrites. Quart.J.Geol.Soc. 135, 137-151.
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