(85).Possil.

Vocabulary

amber

body fossil

cast

fossilization

index fossil

microfossil

mold

permineralization

trace fossil

Introduction

Throughout human history, people have discovered fossils and wondered what they are and what they represent. In ancient times, fossils inspired legends of monsters and other strange creatures. The Chinese writer, Chang Qu, 2,000 years ago reported the discovery of “dragon bones,” which were probably dinosaur fossils. Look at the two photos in the Figure below and try to trace the origin of the creature on the left.

[Figure 1]

The griffin, a mythical creature with a lion’s body and an eagle’s head and wings (left), was probably based on skeletons of Protoceratops (right) that were discovered by nomads in Central Asia.

[Figure 2]

Ammonites (left) and elephant skull (right).

Ancient Greeks named ammonites after the ram god Ammon since they look like the coiled horns of a ram. Legends of the Cyclops may be based on fossilized elephant skulls found in Crete and other Mediterranean islands (Figure above). Can you see why?

Many of the real creatures whose bones became fossilized were no less marvelous than the mythical creatures they inspired (Figure below).

[Figure 3]

(a) The giant pterosaur Quetzalcoatlus had a wingspan of up to 12 meters (39 feet). (b) Argentinosaurus had an estimated weight of 80,000 kg, equal to the weight of seven elephants! Other fossils, such as the trilobite Kolihapeltis ch (c) impress us with their bizarre forms. These suture marks on an ammonite fossil (d) display a delicate beauty.

How Fossils Form

A fossil is any remains or traces of an ancient organism. Fossils include body fossils, left behind when the soft parts have decayed away, and trace fossils, such as burrows, tracks, or fossilized coprolites (feces) (Figure below). Collections of fossils that are found together are known as fossil assemblages.

[Figure 4]

Coprolite from a meat-eating dinosaur.

The process of a once-living organism becoming a fossil is called fossilization. Fossilization is very rare: Only a tiny percentage of the organisms that have ever lived become fossils.

Why do you think only a tiny percentage of living organisms become fossils after death? Think about an antelope that dies on the African plain (Figure below).

[Figure 5]

Hyenas eating an antelope. Will the antelope in this photo become a fossil?

Most of its body is eaten by hyenas and other scavengers and the remaining flesh is devoured by insects and bacteria. Only bones are left behind. As the years go by, the bones are scattered and fragmented into small pieces, eventually turning into dust. The remaining nutrients return to the soil. This antelope will not be preserved as a fossil.

Is it more likely that a marine organism will become a fossil? When clams, oysters, and other shellfish die, the soft parts quickly decay, and the shells are scattered. In shallow water, wave action grinds them into sand-sized pieces. The shells are also attacked by worms, sponges, and other animals (Figurebelow).

[Figure 6]

Shell that has been attacked by a boring sponge.

How about a soft bodied organism? Will a creature without hard shells or bones become a fossil? There is virtually no fossil record of soft bodied organisms such as jellyfish, worms, or slugs. Insects, which are by far the most common land animals, are only rarely found as fossils (Figure below).

[Figure 7]

A rare insect fossil.

Despite these problems, there is a rich fossil record. How does an organism become fossilized?

Usually it’s only the hard parts that are fossilized. The fossil record consists almost entirely of the shells, bones, or other hard parts of animals. Mammal teeth are much more resistant than other bones, so a large portion of the mammal fossil record consists of teeth. The shells of marine creatures are common also.

Quick burial is essential because most decay and fragmentation occurs at the surface. Marine animals that die near a river delta may be rapidly buried by river sediments. A storm at sea may shift sediment on the ocean floor, covering a body and helping to preserve its skeletal remains (Figure below).

[Figure 8]

This fish was quickly buried in sediment to become a fossil.

Quick burial is rare on land, so fossils of land animals and plants are less common than marine fossils. Land organisms can be buried by mudslides, volcanic ash, or covered by sand in a sandstorm (Figurebelow). Skeletons can be covered by mud in lakes, swamps, or bogs.

[Figure 9]

People buried by the extremely hot eruption of ash and gases at Mt. Vesuvius in 79 AD.

Unusual circumstances may lead to the preservation of a variety of fossils, as at the La Brea Tar Pits in Los Angeles, California (Figure below).

[Figure 10]

Although the animals trapped in the Ta Brea Tar Pits probably suffered a slow, miserable death, their bones were preserved perfectly by the sticky tar.

In spite of the difficulties of preservation, billions of fossils have been discovered, examined, and identified by thousands of scientists. The fossil record is our best clue to the history of life on Earth, and an important indicator of past climates and geological conditions as well.

Exceptional Preservation

Some rock beds contain exceptional fossils or fossil assemblages. Two of the most famous examples of soft organism preservation are from the 505 million-year-old Burgess Shale in Canada (Figure below). The 145 million-year-old Solnhofen Limestone in Germany has fossils of soft body parts that are not normally preserved (Figure below).

[Figure 11]

(a) The Burgess shale contains soft-bodied fossils. (b) Anomalocaris, meaning “abnormal shrimp” is now extinct. The image is of a fossil. (c) The famous Archeopteryx fossil from the Solnhofen Limestone has distinct feathers and was one of the earliest birds.

Types of Fossilization

Most fossils are preserved by one of five processes outlined in the Figure below.

[Figure 12]

Five types of fossils: (a) Insect preserved in amber, (b) petrified wood (permineralization), (c) cast and mold of a clam shell, (d) pyritized ammonite, and (e) compression fossil of a fern.

Preserved Remains

Most uncommon is the preservation of soft-tissue original material. Insects have been preserved perfectly in amber, which is ancient tree sap. Mammoths and a Neanderthal hunter were frozen in glaciers, allowing scientists the rare opportunity to examine their skin, hair, and organs. Scientists collect DNA from these remains and compare the DNA sequences to those of modern counterparts.

Permineralization

The most common method of fossilization is permineralization. After a bone, wood fragment, or shell is buried in sediment, mineral-rich water moves through the sediment. This water deposits minerals into empty spaces and produces a fossil. Fossil dinosaur bones, petrified wood, and many marine fossils were formed by permineralization.

Molds and Casts

When the original bone or shell dissolves and leaves behind an empty space in the shape of the material, the depression is called a mold. The space is later filled with other sediments to form a matching cast within the mold that is the shape of the original organism or part. Many mollusks (clams, snails, octopi, and squid) are found as molds and casts because their shells dissolve easily.

Replacement

The original shell or bone dissolves and is replaced by a different mineral. For example, calcite shells may be replaced by dolomite, quartz, or pyrite. If a fossil that has been replace by quartz is surrounded by a calcite matrix, mildly acidic water may dissolve the calcite and leave behind an exquisitely preserved quartz fossil.

Compression

Some fossils form when their remains are compressed by high pressure, leaving behind a dark imprint. Compression is most common for fossils of leaves and ferns, but can occur with other organisms.

Clues from Fossils

Fossils are our best form of evidence about Earth history, including the history of life. Along with other geological evidence from rocks and structures, fossils even give us clues about past climates, the motions of plates, and other major geological events.

History of Life on Earth

That life on Earth has changed over time is well illustrated by the fossil record. Fossils in relatively young rocks resemble animals and plants that are living today. In general, fossils in older rocks are less similar to modern organisms. The history of life will be discussed in the "Earth's History" chapter.

Environment of Deposition

By knowing something about the type of organism the fossil was, geologists can determine whether the region was terrestrial (on land) or marine (underwater) or even if the water was shallow or deep. The rock may give clues to whether the rate of sedimentation was slow or rapid. The amount of wear and fragmentation of a fossil allows scientists to learn about what happened to the region after the organism died; for example, whether it was exposed to wave action.

Geologic History

The presence of marine organisms in a rock indicates that the region where the rock was deposited was once marine. Sometimes fossils of marine organisms are found on tall mountains indicating that rocks that formed on the seabed were uplifted (Figure below).

[Figure 13]

The summit of Mt. Everest, the world’s tallest mountain, is limestone that formed in an ancient sea.

Climate

By knowing something about the climate a type of organism lives in now, geologists can use fossils to decipher the climate at the time the fossil was deposited. For example, coal beds form in tropical environments but ancient coal beds are found in Antarctica. Geologists know that at that time the climate on the Antarctic continent was much warmer. Recall from the chapter about plate tectonics that Wegener used the presence of coal beds in Antarctica as one of the lines of evidence for continental drift.

Index Fossils

An index fossil can be used to identify a specific period of time. Organisms that make good index fossils are distinctive, widespread, and lived briefly. Their presence in a rock layer can be used to identify that period of time over a large area.

KQED: Science on the SPOT: Lupe the Mammoth Comes to Life

The fossil of a juvenile mammoth found near downtown San Jose California reveals an enormous amount about these majestic creatures: what they looked like, how they lived, and what the environment of the Bay Area was like so long ago. Learn more in the video below:

 

 

Lesson Summary

Fossils are the remains of ancient life. Body fossils are the remains of the organism itself; trace fossils are burrows, tracks, feces, or other evidence of activity.

Fossilization is a very rare process. The chances of becoming a fossil are enhanced by quick burial and the presence of hard parts, such as bones or shells.

Fossils form in five ways: by preservation of the remains, permineralization, molds and casts, replacement, and compression.

Types of organisms that make good index fossils are widespread but only existed for a short period of time. Index fossils help scientists to determine the approximate age of a rock layer and to match that layer up with other rock layers.

Fossils give clues about the history of life on Earth, environments, climate, geologic history, and other events of geological importance.