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1.25" Worm (Didontogaster) Fossil (Pos/Neg) - Mazon Creek
This is a nicely defined fossil "tummy tooth worm" (Didontogaster cordylina), preserved inside an ironstone nodule that has been split open. It comes from the famous Mazon Creek Lagerstätte. These ironstone nodules have been collected for decades from the spoil heaps of abandoned coil mines near Coal City, Illinois. Both sides of the nodule are included.
Didontogaster cordylina worms are considered the most commonly found polychaete (marine annelid worm). They earn their species name cordylina from their club-like appearance. This swollen section of the worm from which they gained their name, housed the mouth which contained two conical jaws within its probiscus. It's segmented body and fine setae (body bristles) suggests that this worm was a burrower. It's likely it was a predator as well, for ostracodes and plant material have been found preserved in its gut.
Didontogaster cordylina worms are considered the most commonly found polychaete (marine annelid worm). They earn their species name cordylina from their club-like appearance. This swollen section of the worm from which they gained their name, housed the mouth which contained two conical jaws within its probiscus. It's segmented body and fine setae (body bristles) suggests that this worm was a burrower. It's likely it was a predator as well, for ostracodes and plant material have been found preserved in its gut.
The Mazon Creek fossil beds are a deposit with exceptional fossil preservation, known as a conservation lagerstätte, located in Illinois. This location of late Paleozoic (~307 million years old) biota ranks among the great fossil sites around the world. The large variety of fossils collected here vary between plants and animals, including soft-bodied and insect preservations. Fossils from this site are often quite detailed and are preserved within siderite (iron carbonate) nodules.
Over 500 animal and 200 flora species have been described from Mazon Creek. The event that caused this die-off and preservation is believed to have started with a catastrophic flood event that buried the biota of the modern day Mazon Creek area. The deposition of river-borne silt and clay, brought on by upland erosion and delta progradation, contributed to the incredible preservation of one of the most complete records of Paleozoic biota.
This site has been collected for more than 100 years, and likely will continue to be collected by both professionals and amateurs for many years to come.
Over 500 animal and 200 flora species have been described from Mazon Creek. The event that caused this die-off and preservation is believed to have started with a catastrophic flood event that buried the biota of the modern day Mazon Creek area. The deposition of river-borne silt and clay, brought on by upland erosion and delta progradation, contributed to the incredible preservation of one of the most complete records of Paleozoic biota.
This site has been collected for more than 100 years, and likely will continue to be collected by both professionals and amateurs for many years to come.
SPECIES
Didontogaster cordylina
LOCATION
Grundy County, Illinois
FORMATION
Francis Creek Shale, Carbondale Formation
SIZE
1.25" long worm (straightline)
CATEGORY
ITEM
#113224
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