fYidex Fossi/s
Fossils аге the preserved remains of living things from 10,000 уеагs ago ог mоге.
Usually fossils form when organisms аге quickly buried in sediments апd then аге replaced
Ьу stone and minerals over time. This leaves behind an impression, model, ог remains of an
arganism ог its activity. There аге fossils of animals, plants, fungi, and еvеп tiny fossils of
bacteria and microscopic organisms. Paleontologists аге the scientists who study fossils
and excavate (dig) them from the ground. Fossils help scientists to learn about what life
was like in Earth's past- before humans. Fossils have also helped scientists learn about the
climate апd еvеп where the continents were in the past оп Earth. We call the history of the
Earth geologic time.
Fossils сап Ье found underground where they have to Ье excavated (dug up), ог they
сап Ье found оп the surface due to moving tectonic plates and erosion. Fossils form in
sedimentary rock. When sediments like реЬЫеs, sand, and soil аге deposited оп the
ground Ьу wind, water, ог gravity they сгеаtе а layer. Over time many layers build up like
the layers of а cake. These layers of sedimentary rock аге called strata. The law of
superposition states that the bottom layer in strata is the oldest and the top layer of
strata is the youngest. So as you dig down in strata the layers are getting older and older.
The same thing is true for fossils found in the rock
layers. lf you find two fossils and one fossil is above the
other fossil in the rock strata, the one оп top is younger
than the lower fossil. The law of superposition helps us
to find the relative ages of different fossils- which
fossils are older and younger.
Certain fossils help scientists know what time period а layer of rock came from just Ьу
looking at it. This allows scientists to Ье more accurate with their relative dating. These
fossils аге called index fossils. А fossil has to meet three criteria iп order to Ье
cansidered an index fossil. An index fossil is а fossil that is abundant. Abundant meons it
is easy to find. An index fossil also need to Ье widespread which means it is found all
over the world. Lastly, an index fossil n eeds to Ье short-lived which means it only existed
for а short period of time. Let's look at an example of an index fossil. Ап example of an
index fossil is an ammonite shell. Ammonites were organisms that lived in shallow ports of
осеапs all over the world. They looked like octopi with spiral shells. There were many
different varieties that evolved quickly and lived fог а short period of time. lf we find n
ammonite fossil we know that the rock layer it is iп is hundreds of millions of years old.
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The exact kind of ammonite found will give а more exact date.
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. Fossils are the preserved remains of living things.
They show us how life, landscapes, and climate have changed over time and how
living things responded to those changes.
sedimentary rocks
fossils arent formed from igneous rocks because igneous rocks are formed from lava
or magma
a layer or series of layers of rock in the ground
Radiometric dating is more accurate than relative dating because it provides
an exact date rather than a range of dates.
A useful index fossil must be distinctive or easily recognizable,
abundant, and have a wide geographic distribution and a short
range through time. yes it would because they are cool
because it would break
the shark eggs are older because they were found below the flowering plant fossils.
Microfossils, which are fossils of microscopic organisms, are also useful index
fossils.
A useful index fossil must be distinctive or easily
recognizable, abundant, and have a wide geographic
distribution and a short range through time. yes
yes
no
no