Museum Grade Cambrian Madusa Jellyfish Fossil

Madusa Scyphozoa Jellyfish Ichnofossil

Phylum Cnidaria, Class Scyphozoa; with similarity to extant Order Scyphomedusae

Geological Time: Upper Cambrian (about 510 million years ago)

Size: Matrix measures 24 by 26 inches, and up to 2.5 inches thick; actual weight is 95 pounds

Fossil Site: Blackberry Hill, Krukowski Quarry, Elk Mound Group, near Mosinee, Wisconsin

Code: DD701

Price: $1800.00


Cambrian Madusae Jellyfish FossilPhylum Cnidaria (anemones, corals, jellyfish and sea pens) are among the most ancient animals, simplest in body form, and yet are ubiquitous and widespread even today in marine environments. The earliest forms in the fossil record appear in Ediacarian fauna of Southern Australia, which dates to the Precambrian some 600 million years ago. This is clear testiment that old and simple animals can be enormously successful.

Here we have a sandstone plate with a large Madusa Cambrian Ichnofossil from the Mount Simon Wonewoc Sandstone in Central Wisconsin. Being comprised entirely of soft tissue unlike animals with exoskeletons (e.g., trilobites) or skeletons Scyphomedusae jellyfish(vertebrates), jellyfish fossils are body fossils that are impressions of the jellyfish. Such fossil impressions are rare, especially from the Cambrian. Jellyfish were some of the most ferocious predators of Cambrian Jellyfishthe Cambrian marine environment. These fossils from the Wisconsin quarry are not just large for the Cambrian, but are the largest jellyfish in the entire fossil record. The epirelief preservation found in these jellyfish fossils was likely due to sediment that was trapped within the gastric cavity and/or attached to oral arms and lappets a the animal struggled after standing on a Cambrian shoreline. This particular specimen is one of the few largest and most detailed to be extracted from the quarry, and truly deserving of the accolade, Museum Grade. The specimen is entirely natural. The block was cracked during cutout, and repaired but this does not detract from front-facing appearance.

These jellyfish come from a particular horizon in the Mount Simon Sandstone that also yields facinating Diplichnites, Protichnites, and Climactichnites.

Also see: Cambrian Shadows Madusae Jellyfish Fossils

Hagadorn, J.W., Dott, R.H., and Damrow, D., 2002, Stranded on an Upper Cambrian shoreline: Medusae from Central Wisconsin: Geology, v. 30, p. 147-150.


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