Fossils
of Iowa
by Jean Cutler Prior
Many people have their beginning interest in geology
stimulated by finding fossils. Holding the shell of a
sea-dwelling organism found in an Iowa rock, far from the nearest
ocean, makes us think about the vast changes that have occurred
over the Earth's surface and the great length of geologic time
that has passed. Studying fossils helps us appreciate the history
of life on Earth. They provide a link between geology and biology
that is valuable to the study of global changes and how life
adapts. Fossil remains also are an important tool in dating
different rock layers, and in comparing the sequence of strata
from place to place across broad areas. Iowa has many well known
fossil-bearing rock formations, and fossils from around the state
have found their way into museums around the world. These pages
help to identify a few of Iowa's many fossils that may be found
by careful observation of road cuts, quarries, stream banks and
other exposures of earth materials.
  Colonial corals
Bottom-dwelling corals lived in reef-like communities in warm,
clear, tropical seas covering Iowa. Many species were colonial,
living together in a mass of individual skeletons of lime,
resembling a honeycomb. Distinctive colonial forms from eastern
Iowa include the "chain coral" (left), Pachyphyllum
(middle), and Lithostrotionella (right). They were
especially abundant in Devonian and Silurian seas, 375 to 425
million years ago.
Solitary
coral
Corals also lived alone in curved, cone-shaped skeletons
unattached to other individuals. This fossil "horn
coral" housed the animal's soft tissues, including tentacles
which filtered food particles from sea water.
Brachiopods
These shells are among the most common fossils found in Iowa.
Brachiopods lived inside the protective cover of two hinged
shells, attached to the floor of warm, shallow seas that once
covered the state. These eastern Iowa specimens are about 375
million years old (Devonian).
Gastropod
Shells of marine animals are often preserved as fossils. This
coiled shell from Winneshiek County was inhabited by a snail. The
sluggish, bottom-dwelling mollusk scavenged or grazed the ancient
sea floor about 440 million years ago (Ordovician). The snail
moved on a flat muscular foot and could withdraw inside its shell
for protection.
Fish jaw
This jaw belonged to a 2 to 3 ft-long placoderm, a primitive
fish partly covered by bony plates that gave it an armored
appearance. The black color of this 375 million-year-old
(Devonian) specimen from Black Hawk County results from
mineralization of the fossil bone.
Stromatoporoid
"Stroms" are extinct organisms related to sponges.
They constructed skeletons of lime and lived in various shaped
colonies that resembled layered mats, branches, and rounded
masses. This Floyd County specimen, with its prominent nodes,
lived 370 million years ago (Devonian) .
Crinoids
Crinoids lived anchored to the sea floor by flexible, rooted
stems. Segments of the rounded stems are commonly found as
fossils. Famous localities in Iowa include the LeGrand and
Burlington areas.
Crinoid
Often called "sea lilies," crinoids are actually
animals related to starfish. This 350 million-year-old
(Mississippian) specimen from Marshall County shows the arms,
which in life would filter sea water for food particles.
Trilobites
Prized by collectors, whole trilobites usually display a
three-lobed, oval-shaped, segmented skeleton, often with distinct
eyes. They belong to an extinct group of bottom-dwelling,
hard-shelled arthropods that scavenged the sea floor. These Scott
County specimens are 375 million years old (Devonian).
Bryozoan
"Moss animals" were also colonial, filter-feeding
organisms that inhabited the sea floor. A well known bryozoan (Archimedes)
consisted of concentric rows of lace-like fronds attached to a
corkscrew-shaped axis. The preserved core is seen in this Lee
County specimen (340 million years old, Mississippian).
 Cephalopods
These squid-like animals lived in chambered shells and could
propel themselves by ejecting water from a tube near their head.
The shell's partitions were filled with gas, enabling the animal
to regulate its buoyancy. These straight-shelled cephalopods
(left), from Marion County are 300 million years old
(Pennsylvanian). The coiled cephalopod (right) is a 365
million-year-old (Devonian) specimen from Butler County, and a
distant relative of the chambered nautilus seen in today's
oceans.
Seeds
These black fossil seeds are from Scott County. They grew at
the end of a frond on a fern-like tree about 300 million years
ago (Pennsylvanian).

Mastodon(left) and mammoth(right) teeth
Tooth shapes of these 15,000 year-old molars indicate
mastodons browsed tree branches, while mammoths grazed grasses.
Fossils of these extinct Ice Age (Pleistocene) creatures
resembling elephants have been widely found across Iowa.
Clam shell
Like gastropods and cephalopods, clams are also mollusks that
live in a protective shell. This Plymouth County specimen lived
on a sea floor 90 million years ago (Cretaceous). Clams were
abundant in these waters, the last of the great inland seaways to
cover Iowa.
Amphibian
pelvis
This pelvic bone belonged to a 3 to 4 foot-long
proto-anthracosaur, a rare, primitive amphibian that lived 330
million years ago (Mississippian) and was found in Keokuk County.
 Seed-fern
leaves and scale-tree trunk
The fossil foliage of seed ferns (small fossils) was found in
Dallas County, and the scale-tree (Lepidodendron, large
fossil) in Muscatine County. About 310 million years ago, these
plants were common in the coastal swamps that produced Iowa's
coal deposits (Pennsylvanian).
Photographs by Paul VanDorpe
Photo setups by Patricia Lohmann
Adapted from Iowa Geology 1993, No. 18, Iowa
Department of Natural Resources
|