Tullimonstrum gregarium

Tullimonstrum gregarium

Taxobox
name = "Tullimonstrum gregarium"
status =
fossil_range = fossil range|311|306Middle Pennsylvanian



image_width = 250px
image_caption = Life restoration of "T. gregarium"
regnum = Animalia
subregnum Eumetazoa
Bilateria (unranked)
phylum = Problematica
classis =
ordo =
familia =
familia_authority = Eugene S. Richardson, Jr., 1966
genus = "Tullimonstrum"
genus_authority = Eugene S. Richardson, Jr., 1966
subdivision_ranks = Species
subdivision =
*"T. gregarium" (type)

The Tully Monster ("Tullimonstrum gregarium"), so far apparently unique to Illinois, USA, was a soft-bodied invertebrate that lived in shallow tropical coastal waters of muddy estuaries during the Pennsylvanian geological period, about 300 million years ago.

Description

The "Tully Monster" had a pair of fins not unlike a cuttlefish at the tail end of its body, and possibly vertical fins as well (though the fidelity of preservation of fossils of its soft body makes this difficult to determine), and a long proboscis with eight small sharp teeth with which it may have probed actively for small creatures and edible detritus in the muddy bottom. A stalk protruding from either side of the lower forward body may have had an eye or other sensory organ at its tip, but this is speculative. It was part of the ecological community represented in the unusually rich group of soft-bodied organisms found among the assemblage called the "Mazon Creek fossils" from their site in Grundy County, Illinois.

The formation of the Mazon Creek fossils is unusual. When the creatures died, they were rapidly buried in silty outwash. The bacteria that began to decompose the plant and animal remains in the mud produced carbon dioxide in the sediments around the remains. The carbon dioxide combined with iron from the groundwater around the remains, forming encrusting nodules of siderite ('ironstone'), which created a hard permanent 'cast' of the animal which slowly further decayed, leaving a carbon film on the cast.

The combination of rapid burial and rapid formation of siderite resulted in excellent preservation of the many animals and plants that ended up in the mud. As a result, the "Mazon Creek fossils" are one of the world's major Lagerstätten, or concentrated fossil assemblages.Amateur collector Francis Tully found the first of these fossils in 1958. He took the strange creature to the Field Museum, but paleontologists remain stumped as to what phylum "Tullimonstrum" belongs. In 1989 "Tullimonstrum gregarium" was officially designated the State Fossil of Illinois.

ee also

*Burgess shale

External links

* [http://www.museum.state.il.us/exhibits/symbols/fossil.html "Tullimonstrum" described.]
* [http://www.museum.state.il.us/collections/newtully.html A particularly well-preserved "Tullimonstrum" in the Illinois State Museum.]
* [http://www.isgs.uiuc.edu/servs/pubs/geobits-pub/geobit5/geobit5.html Illinois State Geological Survey surveys "Tullimonstrum".]
* [http://www.statefossils.com/il/il.html Tully Monsters described and illustrated.]


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