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Some brachiopods have prominent spines, but these are usually broken off and are found as separate fossils. Fossils come in various forms--from bones and shells to carbon imprints to footprints and burrows. Bryozoans Among the most abundant fossils in the world, bryozoans are lokking widespread today, both in marine and freshwater environments, living at all latitudes and depths ranging downward to at least 27, feet 8, meters.

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Like the familiar snail, most gastropods except for slugs have a single coiled shell. Familiar invertebrates living today include insects, snails, clams, and corals. During their long history, trilobites evolved a multitude of forms.

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Unlike multicellular animals, which accomplish basic life functions such as lookibg, feeding, digestion, and reproduction through a wide range of specialized cells, fusulinids and other single-celled organisms have to carry on these same functions within the confines of a single cell. These crinoids, from the Niobrara Chalk of western Kansas, lived during the later part of the Cretaceous Period fig.

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Fossils of these and other types of invertebrates are frequently found in Kansas rocks. Stem pieces, which may be round, elliptical, pentagonal, or star-shaped with a hole in their centers, are abundant in eastern Kansas limestones and shales. Trilobites had a hard external skeleton, or carapace, that consisted of three main parts: a head, the cephalon, which is typically crescent shaped; a middle region called the thorax, made up of 2 to 61 overlapping segments; and a tail, the pygidium, in which the segments were fused fig.

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Hard parts hold up better lookiing decay and destruction than such soft tissue as muscles and organs. Brachiopods are one of the most common fossils in the Pennsylvanian rocks in eastern Kansas and are common in the younger Permian rocks. Because their fossils are so common in Cambrian rocks, the Cambrian Period is sometimes called the age of trilobites.

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The coarser sediment, such as sand, settled out first, while the finer-grained clay- and silt-sized particles were carried farther out to sea. Inside the bivalve's hard shell, the body consists of two lobes, one lining each valve. Shale, on the other hand, is composed of compacted clay- and silt-sized particles too small to be seen without a microscope.

Fusulinids were single-celled organisms, about the size and shape of a grain of wheat. A listing of these guidebooks can be accessed from the KGS online bibliography or by contacting the Publications and Sales posssible Figure Common fossil gastropods from Kansas. The calcium carbonate ooze that collected on the sea floors made a perfect burial ground.

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Collecting Fossils in Kansas As mentioned in the introduction, many Kansas outcrops contain invertebrate fossils, and those in the Smoky Hills region of north-central Kansas and in the eastern third of Kansas, from the Flint Hills to the Missouri border, are especially fossiliferous. Fusulinids Fusulinids were small, marine organisms that populated the seas worldwide during the Pennsylvanian and Permian periods.

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Their fossil record extends back approximately million years to the early part of the Cambrian Period and indicates that trilobites evolved rapidly in the shallow seas of this time. The earliest fusulinids were smaller than the head of a pin, and somewhat spherical.

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Complete trilobite carapaces are uncommon because the skeletal parts were usually scattered by currents, scavengers, or other processes. Ammonoids are loooing common fossils in the Cretaceous outcrops of central and western Kansas and less common in eastern Kansas, where smaller fossils occasionally are found in Pennsylvanian and Permian outcrops fig.

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Tabulate and rugose corals are common in the rocks of eastern Kansas. Fossils and Fossilization Fossils are the remains or evidence of ancient life. The earliest fossil corals come from the Middle Cambrian, about million years ago.

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Rugose corals may be either solitary or colonial. Thus, for example, we find many more clams than worms in the fossil record. Crinoids Crinoids are echinoderms, animals with rough, spiny surfaces and a special kind of radial symmetry based on five or multiples of five.

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The shells of fossil gastropods vary enormously. Bryozoans are sometimes confused with corals, which are also colonial. Trilobites appear to have died out completely near the end of the Permian Period, just before the huge extinction that marked the end of the Paleozoic Era. Fusulinid fossils are found on all continents except Antarctica and are common in the Permian and Pennsylvanian rocks of eastern Kansas.

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Internally, ammonoid shells were divided into many chambers by a series of intricately folded walls. Bryozoans, however, are more complex organisms than corals and generally do not build reefs.

The largest--inoceramid clams from western Kansas--are as much as 6 feet 1. Instead, most are eaten, attacked by bacteria, fragmented, crushed, or dissolved or worn away by water movement--to name some common fates. Fusulinids became extinct during the mass extinction at the end of the Permian Period.

Some bivalves, such as oysters, do not have symmetrical valves. In Kansas, they are fairly common in Pennsylvanian and Permian rocks. The name brachiopod comes from the Latin words for arm brachio and foot pod and refers to a paired, internal structure, which specialists fr thought was used for locomotion.

Sandstone and shale, on the other hand, are made up of sediment that eroded from other rocks. From shell fragments in a chunk of gravel to spectacular specimens in museum displays, Kansas fossils contain important evidence about the history of life on earth. Fragmented or whole, fossils provide vital information about earth and its inhabitants millions, even fof, of years ago.

Crinoids have lived in the world's oceans since at least the beginning of the Ordovician Period. Sandstone, as its name suggests, is made up of sand grains, bonded together by natural cement. A muscular structure called a foot, present in most bivalves, is used for locomotion and burrowing. Still, the odds are decidedly possiblee preservation as a fossil.

In lookiny of their abundance in many Cretaceous rocks worldwide, brachiopods are almost never found in the Cretaceous rocks of Kansas.

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Some had enormous eyes; others were blind. Brachiopod shells come in a variety of shapes and sizes fig. Fossil bivalves come in many different shapes and sizes and have a wide range of external markings.

Rugose comes from the Latin word for wrinkled. Two groups of corals were important inhabitants of the Pennsylvanian and Permian seas--tabulate and rugose corals.