BIO 113 — Dinosaurs

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Virtual Museum: Miscellaneous Invertebrates

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Contents: Vendobionta, etc. | Porifera | Cnidaria | Bryozoa | Brachiopoda | Annelida, etc. | Hemichordates
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"Vendobiontans": Ediacaran Mystery Animals


Charniodiscus arboreus (fossil cast), Phylum Rangeomorpha, is a strange frond-like organism with a quilted pattern on its surface. It is not even clear if it was an animal, but we know it didn't photosynthesize because it lived in water too deep for much light to penetrate. It probably absorbed dissolved nutrients directly from the water.

Ediacaran Period, 565-555 Ma

New Mexico Museum of Natural History & Science, Albuquerque

Charniodiscus

Chondroplon bilobatum (fossil cast) is an animal of unknown relationship, possibly belonging to the Cnidaria or an extinct group.

Ediacaran Period, 555 Ma

New Mexico Museum of Natural History & Science, Albuquerque

Chondroplon

Dickinsonia costata, Phylum Proarticulata, was a flat, bilaterally symmetric (can be evenly divided into right and left halves) animal with a series of segments. Although they may resemble flat-bodied segmented worms, their segments on each side are off-set from the other side, unlike all modern worms. Trace chemical analysis indicates they were animals.

Ediacaran Period

Denver Museum of Science & Nature

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Ediacaran Diorama, featuring Charniodiscus arboreus, Mawsonites spriggi, Ediacaria flindersi, Kimberella quadrata, & Dickinsonia costata

Ediacaran Period

Denver Museum of Science & Nature

Ediacara 1

Phylum Porifera — The Sponges


Sponges, such as this Diagonella sp., are the simplest animals, lacking true tissues or organs. They feed by drawing water through their body and filtering out bacteria, algae, and other tiny bits of food.

Utah

Middle Cambrian, Wheeler Shale, 507 Ma

Museum of Ancient Life, Utah

Diagonella sponge

There is some debate as to whether these Chancellaria sp. are actually true sponges or evolved independently.

Utah

Middle Cambrian, Wheeler Shale, 507 Ma

Museum of Ancient Life, Utah

Chancellaria

Choia sp., a sponge in the Class Desmospongiae.

Utah

Middle Cambrian, Wheeler Shale, 507 Ma

Museum of Ancient Life, Utah

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Phylum Cnidaria — Jellyfish, Corals, & Anemones


These disk-like Medusinites asteroides fossils from the Ediacaran are thought to be jelly-fish like animals, but this view is debated.

Ediacaran Period, 610-550 Ma

New Mexico Museum of Natural History & Science, Albuquerque

Medusinites

Horn Corals and a Tabulate Coral (center). Corals are simple animals that secrete a calcium carbonate skeleton around them. These skeletons can form complex reefs that become habitat for many other kinds of animals. These corals are from a different group than modern corals (which evolved only after these went extinct).

near Tonto Village, AZ

Middle Devonian Period, Martin Formation, 380 Ma

personal collection

horn corals

Sun Coral, Pachyphyllum nevadens, a colonial coral.

near Tonto Village, AZ

Middle Devonian Period, Martin Formation, 380 Ma

personal collection

Pachyphyllum

Hexagonaria sp. is a colonial coral similar to Pachyphyllum, above, but this specimen has been polished to show its internal structure.

Assa Zag, Western Sahara, Morocco

Devonian Period, 350 Ma

personal collection

Hexagonaria

Horn corals, probably Zaphrenthis sp.

Falls of the Ohio State Park, Indiana

Devonian Period, 387 Ma

In situ

Horn Corals

Eridophyllum sp. coral colony

Falls of the Ohio State Park, Indiana

Devonian Period, 387 Ma

In situ

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Phylum Bryozoa — Moss Animals


Bryozoans are tiny animals that secrete a calcite case in which they live. They nearly always form colonies of many individuals that can resemble some coral colonies. Colonies can form flat crusts over rocks or shells, or have branching or grid-like structures. Two species are shown here, the branching Pseudohornera bifida and Pachydictya kuckersensis, which has larger pores through which the individual animals would extend their tentacles (each opening is thus one individual in the colony).

Narva, Estonia

Late Ordovician Period, Viivikonna Formation

personal collection

bryozoans

An unidentified branching bryozoan. Each tiny pore represents the opening to one individual "house".

Taylor Mill, KY

Ordovician Period

personal collection

Branching Bryozoan

These bryozoan colonies, most likely Fenestella sp., form a grid-like branching pattern.

Kohl's Ranch, AZ

Carboniferous Period, Pennsylvanian Epoch, Desmoinesian Stage, Naco Formation, 310 Ma

personal collection

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Brachiopoda — Lamp Shells


Brachiopods have two shells ("valves") so they superficially resemble bivalve mollusks such as clams and scallops. However, Brachiopod valves are top and bottom instead of left and right, and their internal anatomy is also quite different.

These brachiopods all were collected at a single locality reflecting a shallow marine environment. They are as follows: top row: Derbyia crassa (left & right); Anthracospirifer occiduus (middle); middle row: 2 Cleiothyridina orbicularis; bottom row: 2 Composita subtilita, Antiquatonia portlockiana.

Kohl's Ranch, AZ

Carboniferous Period, Pennsylvanian Epoch, Desmoinesian Stage, Naco Formation, 310 Ma

personal collection

brachiopods

Sowerbyella sp. brachiopods.

Kincaid Lake, KY

Ordovician Period

personal collection

brachiopods

Hyolithids, such as this Hyolithes cecrops, are extinct cousins of the brachiopods (but are technically a separate group). The curved structure at right (one of two) probably supported them above the sea bed.

Box Elder Co., UT

Middle Cambrian Period, 525 Ma

Denver Museum of Science & Nature

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Annelida & Priapulida — Segmented & Other Worms


Since worms are mostly soft-bodied, their fossilization requires special conditions, such as the formation of these concretions. Astreptoscolex anasillosus is an example of an annelid or segmented worm (the group that includes earthworms).

Mazon Creek, Grundy Co., IL

Carboniferous Period, Middle Pennsylvanian Epoch, Francis Creek Shale, Carbondale Formation

personal collection

Astreptoscolex

This Fossundecima konecniorum worm has swimming appendages and spines

Mazon Creek, Grundy Co., IL

Carboniferous Period, Middle Pennsylvanian Epoch, Francis Creek Shale, Carbondale Formation

personal collection

Fossundecima worm

Priapulid worms, such as this Ottoia sp., are not at all closely related to the annelid worms.

Utah

Middle Cambrian, Wheeler Shale, 507 Ma

Museum of Ancient Life, Utah

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Hemichordata — Acorn Worms and Relatives


Graptolites are, like bryozoans, colonies of tiny animals. In this Amphigraptus sp. , the saw-blade-like structures are colonies, and each tooth represents a single individual in that colony.

Murray Co., OK

Ordovician Period, Trentonian Stage, Viola Limestone

personal collection

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This page last updated 10 July 2021 by Udo M. Savalli ()
Images and text © Udo M. Savalli. All rights reserved.