Fossils: A Link to the Past
By Diana Dell
Fossils
are the remains or records of ancient living things. Fossils may be a whole animal preserved in ice, a bone or tooth
hardened by minerals, an insect encased in amber, a footprint, or the outline
of a leaf.
The
remains of most organisms decay or are consumed by other animals. However, if the body sinks into muddy
riverbeds, or a tar pit, or is quickly covered by the blowing winds of a desert
storm, a fossil may form. Hard parts,
such as wood, shells, bones and teeth decay less easily than soft parts, such
as skin and muscles. Therefore, hard
parts are more likely to be preserved.
Almost
all fossils are formed in sedimentary rock, or rock that has built up in layers
from small particles. These rocks lie
beneath about three-fourths of the land surface of the Earth. Most sedimentary rocks contain fossils. Fossils of animals that lived in different
time periods are found in different layers of rock. Generally speaking, fossils found in deeper layers are older than
fossils found in layers closer to the surface.
A
scientist who studies fossils is called a paleontologist. Paleontologists have learned about the
Earth’s changing geography from studying fossils. From this study, paleontologists have created a geologic time
chart, which divides the earth’s history in to eras.
Much
has been learned through the discovery and study of dinosaur fossils. When dinosaurs lived, the earth was much
different from the way it is today.
Dinosaurs probably lived in an almost tropical climate. Scientist believe this is true because of
the fossils of giant ferns and other swamp type plants that have been found in
the same areas as dinosaur fossils.
A
long series of fossils from animals and plants found in succeeding layer of the
Earth’s crust tells a story about the diversity of life long ago. Fossils help scientists trace the
development of life from ancient times to present day. For example, some scientists believe that
present day reptiles, such as lizards, are the relatives of prehistoric
dinosaurs. Other scientists believe
that dinosaurs are related to present day birds. Sea lilies are relatives of prehistoric sea animals called crinoids. Trilobites are related to present-day crabs
and lobsters. As these examples
illustrate, fossils link the past to the present.