PowerPoint Presentation

Geologic Time and Earth’s

Biological History

Designed to meet South Carolina

Department of Education

2005 Science Academic Standards

 What is the Geologic Time Scale? (slide 4) Standard 8-2.4

`Epochs, Eons, Eras, and Periods (slide 4)

 How was the time scale and it‟s divisions created? (slide 5)

 A complete Geologic Time Scale with references to S.C. (slides 6-7)

Table of Contents

 Principles of the Geologic Time Scale (slide 8)

 Principles of Superposition, Horizontality and Original lateral continuity

 Principle of biologic succession (slide 9)

 Charles Lyell, the Principle of cross-cutting relations & Inclusion principle (slide 10)

 Charles Darwin

 Relative Age Dating using unconformities (slide 10) Standard 8-2.6

 Relative Age dating using cross-cutting relations and index fossils (slide 11)

 Absolute Age dating (slide 13)

 Isotopes and radiometric dating

 Carbon dating (slide 14)

 How old is old? (slide 16)

 Breakdown of geologic time periods

 Are we now living in the Anthropocene Era? (slide 17)

Table of Contents, cont. (2 of 2)

 The Earth through time (slide 19) Standard 8-2.5

 Ordovician and Silurian

 Devonian, Mississippian, Pennsylvanian (slide 21)

 Permian and Triassic (slide 22)

 Jurassic and Cretaceous (slide 23)

 Triassic and Quaternary (slide 24)

 Adaptation (slide 25) Standard 8-2.1

 Punctuated events through time (slide 26) Standard 8-2.3

 Comet impact

 Climate shift

 Volcanism

 Extinction (slide 29) Standard 8-2.7

 The study of fossils and fossil types (slide 30) Standard 8-2.2

 South Carolina Standards (slide 32)

What is the Geologic Time Scale?

What does the time scale represent?

 The geologic time scale divides up the history of the earth based on life-forms that

have existed during specific times since the creation of the planet. These divisions are

called geochronologic units (geo: rock, chronology: time).

 Most of these life-forms are found as fossils, which are the remains or traces of an

organism from the geologic past that has been preserved in sediment or rock. Without

fossils, scientists may not have concluded that the earth has a history that long precedes

mankind.

 The Geologic Time Scale is divided by the following divisions:

Standard 8-2.4: Recognize the relationship among the units—era, epoch, and period—into which the geologic time scale is

divided.

 Eons: Longest subdivision; based on the abundance of certain fossils

 Eras: Next to longest subdivision; marked by major changes in the fossil record

 Periods: Based on types of life existing at the time

 Epochs: Shortest subdivision; marked by differences in life forms and can

vary from continent to continent.

Table of Contents

What is the Geologic Time Scale, continued?

 Due to the fact that early geologists had no way of knowing how the discoveries of

the Earth were going to develop, geologist over time have put the time scale together

piece by piece. Units were named as they were discovered. Sometimes unit names

were borrowed from local geography, from a person, or from the type of rock that

dominated the unit.

 The earliest time of the Earth is called the Hadean and refers to a period of time for which we

have no rock record, and the Archean followed, which corresponds to the ages of the oldest known

rocks on earth. These, with the Proterozoic Eon are called the Precambrian Eon. The remainder of

geologic time, including present day, belongs to the Phanerozoic Eon.

 While the units making up the time scale are called geochronologic units, the actual rocks formed

during those specific time intervals are called chronostratigraphic units. The actual rock record of a

period is called a system, so rocks from the Cambrian Period are of the Cambrian system.

Examples

 Cambrian: From the Latin name for Wales. Named for exposures of

strata found in a type-section in Wales by British geologist Adam Sedgwick.

 Devonian: Named after significant outcrops first discovered near

Devonshire, England

 Jurassic: Named for representative strata first seen in the Jura Mountains

by German geologist Humboldt in 1795)

 Cretaceous: From the Latin “creta” meaning chalk by a Belgian geologist

Table of Contents

GEOLOGIC TIME SCALE

MYA ERA PERIOD EPOCH PLATE TECTONICS LIFE

0.01

Cenozoic

“Age of

Mammals”

Quaternary

Holocene Beaches and barrier islands form

-Mastadons become extinct

-Human culture flourishes

-Accelerating extinction of many

species

1.8 Pleistocene Ice sheets form

-Modern humans develop

-Asians arrive and settle the

Americas

5.3

Tertiary

Pliocene

-Volcanic activity in North

America and Africa

-Grand Canyon forms

Hominids develop

23.8 Miocene Sandhills form in S.C.

Horses, mastadons, mammoths,

tigers, and camels live in South

Carolina

33.7 Oligocene

Appalachians uplift; erosion

increases

Cats, dogs, and apes appear

54.8 Eocene

Sea levels rise; deposits of marine

sediments – limestone in S.C.;

land bridges form

-Grass spreads widely

-Diverse array of animals develop,

including whales, rhinos, and

elephants

65.0 Paleocene

Earthquakes common; Georgia

Embayment, Cape Fear Arch

forms in Southeast

-First horses appear (size of a cat)

-Tropical plants dominate

144

Mesozoic

“Age of

Reptiles”

Cretaceous

Mass extinction occurs at the end

of the period caused by a

meteorite impact (Dinosaurs,

ammonites and 25% of marine life

become extinct)

-T-Rex develops but number of

dinosaur species decline

-Snakes appear and first primates

appear

-Angiosperms appear

206 Jurassic

Western US: orogeny of Rockies;

North America continues to rotate

away from Africa

-First birds appear

-Golden age of dinosaurs

248 Triassic

-Pangea begins to break apart

-Rocky Mountains and Sierra

Nevada form

First dinosaurs, mammals,

crinoids, and modern echinoids

appear

290 Permian

-Pangea forms

-Appalachians rise

-90% of Earth’s species become

extinct, including trilobites,

blastoids, fish and amphibians

because of heavy volcanism in

Siberia

Table of Contents

320

Carboniferous

Pennsylvanian

Great swamps develop (future

coal deposits

-Reptiles develop from

amphibians

-Flying insects appear

354 Mississippian

Much of North America is under

water

-First seed plants appear

-Sea life flourishes including

coral, brachiopods, blastoids, and

bryozoa

417 Devonian

Acadian Orogeny – SC

metamorphism

-Dominant animals: fish

-Amphibians, evergreens and

ferns appear

443 Silurian Extensive erosion

First land plants appear and land

animals follow

490 Ordovician

-Beginning of the construction of

South Carolina

-Great extinction due to growth of

ice caps including in what is now

northern Africa

-First animals with bones appear

-Dominant animals: marine

invertebrates including corals and

trilobites

540 Cambrian

S.C. near the equator; island arc

continues to move toward North

America

-Explosion of life

-All existing phyla came into

being here

-Life forms in warm seas as

oxygen levels rose enough to

support life

-Dominant animals: trilobites and

brachiopods

4600

Precambrian

(Hadean, Archean, and Proterozoic Ages)

Earth takes 10 million years to

cool: initial atmosphere escapes

into space (H&He) and the core

forms (Fe&Ni)

Volcanic outgassing of water and

carbon dioxide occurred for

millions of years, helping to build

atmosphere and then oceans

At 3 billion years ago, banded

iron formation rocks appear due

to rising oxygen levels in the

atmosphere and sea

No life possible as the Earth

initially forms 4.6 billion years

ago.

Simple, single-celled forms of life

appear 3.8 billion years ago.

They will become more complex

and successful over the next 3

billion years: Prokaryotes then

Eukaryotes

Cyanobacteria begins producing

free oxygen (photosynthesis)

Paleozoic

“Age of

Invertebrates”

Modified after Carolina Rocks, contributed by J. Westmoreland

Table of Contents

Principles Behind Geologic Time

 Nicholas Steno, a Danish physician (1638-1687), described how the position of a rock layer could

be used to show the relative age of the layer. He devised the three main principles that underlie the

interpretation of geologic time:

 The principle of superposition: The layer on the bottom was deposited first and so is the oldest

 The principle of horizontality: All rock layers were originally deposited horizontally.

 The principle of original lateral continuity: Originally deposited layers of rock extend laterally

in all directions until either thinning out or being cut off by a different rock layer.

 These important principles have formed the framework for the geologic area of stratigraphy,

which is the study of layered rock (strata).

 Decades later, other European scientists rediscovered „Steno‟s Laws‟ and began applying them.

Abraham Gottlob Werner became famous for his proposal that all rocks came from the ocean

environment. He and his followers were called “Neptunists.” An opposing view (by Voisins)

argued that all rocks of the earth came from volcanic environments. These scientist were called

“plutonists.”

Older

Younger

Geologist studying the stratigraphy in

the Copper Basin, Idaho. These rock

layers were deposited horizontally,

and uplifted later so they are now

tilted at an angle (along the red arrow).

(Photo contributed by K. McCarney-Castle)

Table of Contents

 James Hutton, a Scottish physician and geologist (1726-1797), thought the surface of the earth

was an ever-changing environment and “the past history of our globe must be explained by what

can be seen to be happening now.” This theory was called “uniformitarianism,” which was later

catch-phrased as “the present is the key to the past.”

 William Smith was a surveyor who was in charge of mapping a large part of England. He was

the first to understand that certain rock units could be identified by the particular assemblages of

fossils they contained. Using this information, he was able to correlate strata with the same fossils

for many miles, giving rise to the principle of biologic succession.

 The principle of biologic succession: Each age in the earth‟s history is unique such that

fossil remains will be unique. This permits vertical and horizontal correlation of the rock

layers based on fossil species.

Even though these two outcrops are

separated by a large distance, the same

rock layer can be correlated with the

other because of the presence of the

same shark teeth. This lets scientists

know that the two layer were deposited

at the same time, even if the surrounding

rocks look dissimilar from each other.

300 km

Rock Outcrop 1

Rock Outcrop 2

Principles Behind Geologic Time, continued

Table of Contents

 During the early 1800‟s, English Geologist, Charles Lyell published a book called “Principles of

Geology,” which became a very important volume in Great Britain. It included all of Hutton‟s

ideas, and presented his own contemporary ideas such as:

 The principle of cross-cutting relationships: A rock feature that cuts across another feature

must be younger than the rock that it cuts.

 Inclusion principle: Small fragments of one type of rock but embedded in a second type of

rock must have formed first, and were included when the second rock was forming.

 The theory of natural selection was credited to Darwin (along with Alfred Russel Wallace) and

he went on to write the famous “Origin of Species.” Darwin‟s two goals in that work were:

1. To convince the world that evolution had occurred and organisms had changed over

geologic time

2. The mechanism for this evolution was natural selection.

 Charles Darwin (1809-1882) was an unpaid naturalist who signed up for a 5-yr

expedition around the world aboard the H.M.S. Beagle. On this trip, he realized

two major points. In spite of all species reproducing, no one species overwhelmed

the Earth, concluding that not all individuals produced in a generation survive. He

also found that individuals of the same kind differ from one another and concluded

that those with the most favorable variations would have the best chance of

surviving to create the next generation.

Principles Behind Geologic Time, continued

Table of Contents

Standard 8-2.6: Infer the relative age of rocks and fossils from index fossils and the ordering of the rock layers.

 “Relative age” means the age of one object compared to the age of another, not the exact age of

an object. This method can only be used when the rock layers are in their original sequence.

 All six of the original stratigraphic principles may be applied to determine the age of a rock.

This process is called age dating. Correlation of strata by rock unit type (lithology) or fossil type

(biology) using species, composition, or texture leads scientists to extrapolate relationships over

large areas of land. Because rock layers can be “matched up,” we can guess that they were

formed during the same period, so they usually are the same age.

 Using the principles of original horizontality and superposition, we can conclude that oldest

rock is always on the bottom because is was deposited 1

 Deciphering the sequence of a rock outcrop is sometimes complicated by a features within the

rock record called unconformities, which are specific contacts between rock layers. There are

three types of unconformities that help us determine relative ages of rock layers:

1. Angular: Horizontal beds are uplifted and tilted or

eroded followed by new deposition of horizontal

beds. The figure to the right is an angular

unconconformity.

2. Disconformity: Episodes of erosion or non-

deposition between layers

3. Nonconformity: Sediment is deposited on top of

eroded volcanic or metamorphic rock (indicates

very long passage of time)

Relative Age Dating

Wikipedia (public domain)

Tilted bed of

sedimentary rock

Horizontal bed of

sedimentary rock

Table of Contents

Relative Age dating with index fossils

 Biostratigraphy is the correlation of stratigraphic units based on fossil content.

Biostratigraphically useful species are known as index fossils (or guide fossils) because they can be

used as guides for recognition of chronostratigraphic units.

 Index fossils are widespread, have short temporal durations resulting from rapid life spans, are

abundant throughout their geographic and geologic ranges, and are easily recognized (unique).

 Relative ages can also be determined using Lyell‟s

principle of cross-cutting relationships. In the figure to

the right, both the gray and the yellow horizontal strata

needed to be in place for the pink layer to cut them,

therefore, the pink layer is the youngest. (Image from Plummer/

McGeary, 7

edition, 1996)

 Trilobites are a commonly used index fossil because they

are easy to recognize. We know exactly when certain

species became extinct, such that we can compare rock

layers that contain trilobites with a second rock layer and,

based on position, determine if the second rock layer is

younger. The photo to the right is a trilobite from the

Mississippian period (photo courtesy of K. McCarney-Castle)

 Fossils found in many rock layers have lived for long

periods of time and cannot be used as index fossils.

Table of Contents

Absolute Age Dating

 Absolute ages, or geochronometric ages, of rock can be assigned to the geologic time scale on the

basis of properties of atoms that make up the minerals of a rock. Unlike relative dating, which

relies on sequencing of rock layers (i.e. younger vs. older), absolute dating can produce an actual

age in years.

 The number of neutrons in a nucleus of an atom determines the isotope of the element, just like

the number of protons determines the identity of an element.

 Some isotopes are unstable and break down into other isotopes through a process called

radioactive decay. Radioactive decay is characterized by beta decay, where a neutron changes into

a proton by giving off an electron, and alpha decay, when isotopes give off 2 protons and 2

neutrons in the form of an alpha particle and changes into a new product. The original isotope is

called the parent and the new isotope product is called the daughter.

Note: Radioactive isotopes can be found in the rock record because radioactive

isotopes are incorporated into the crystals of igneous rock as it cools.

 What is a Half-Life?

 Each radioactive parent isotope decays to its daughter product at a specific and measurable

rate. This measurement is reported in half-lives. The half-life of an isotope is the time it

takes for ½ of the parent atoms in the isotope to decay.

 If an isotope has a half-life of 4000 years, then after 4000 years ½ of the parent isotope

remains. After another 4000 years, ½ of ½ remains, or ¼ of the original amount of parent

isotope. In another 4000 years (12,000 years total), ½ more of the remaining amount decays,

so after 3 half-lives, there only remains 1/8 (½ of ½ of ½) of the original parent isotope.

 If a scientist knows the half-life of the parent and measures the proportion of parent

isotope to daughter isotope, he/she can calculate the absolute age of the rock. This valuable

method is called radiometric dating.

Table of Contents

12.5%

6.25%

100%

50%

25%

50%

75% 87.5%

93.75%

Scientists used the proportion of parent

material remaining to the proportion of

daughter material produced in order to

predict the age of the rock. During each half-

life, only one-half of the parent material

decays to the daughter product.

DECAY

PARENT DAUGHTER

Radioactive Decay

Radiocarbon Dating

 Radiocarbon dating is a common method used to date anything that was once alive (including

plants) and up to 70,000 years old.

 All living things take in carbon from the environment in the form of carbon-12 and carbon-14.

When an organism dies, carbon intake stops and the carbon-14 begins to decay at a known rate.

Scientists can determine how much C-14 remains in an organism by measuring radiation emitted

by the C-14 isotopes.

 Carbon dating can be used on wood, plants, humans, and even old paper made out of papyrus.

 The half-life of C-14 is 5,730 years. Because of this, it should not be used with material older than

~70,000 years or 12 half-lives.

 Isotopes with very long half-lives are not suitable for dating rocks younger than ~1 million years

because there are too few daughter atoms to be measured accurately.

 Experimental error limits measurements to those rocks younger than about 12 half-lives of the

isotope used.

Table of Contents

Parent Daughter half-life Mineral or Material

Uranium238 Lead 206 4.56 BY Zircon, Uraninite, Pitchblende

Uranium 235 Lead 207 704 MY Zircon, Uraninite, Pitchblende

Potassium 40 Argon 40 1.251 BY Muscovite, biotite, hornblende, K-feldspar,

volcanic rock, glauconite, conodonts

Rubidium 87 Sr 87 48.8 BY K-mica, K-feldspar, Biotite, Metamorphics

Thorium 230 Lead 206 75 KY Ocean sediments

Thorium 232 Lead 208 1.39 BY Zircon, Uraninite, Pitchblende

Carbon 14 Nitrogen 14 5730 yr Wood, bone, shell

Commonly used radioactive isotopes

Uranium-Lead decay series (U-Pb series)

 Unlike carbon-14 dating, uranium dating cannot be used to date formerly living things;

however, it is the most commonly used method in igneous rock dating because of the abundance

of zircon minerals.

 The subscripts of 235 and 238 are the atomic mass numbers of the element. Though each

isotope has 92 protons in its nucleus, U-235 has 143 neutrons and U-238 has 146 neutrons.

 Igneous rocks, or the magma from which it was formed, often intrudes overlying sedimentary

rocks. By dating the magma, one can get at least a minimum age for the sedimentary rock.

KY- thousand years. MY- million years. BY- billion years

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 From the time of Hutton, scientists were convinced that the earth was much older than the 6000

years predicted by the religious scholars.

 Charles Lyell tried to estimate the age of the earth through the amount of evolution

exhibited by marine mollusks in a specific time system.

 Another method was to estimate the rate of deposition for sedimentary rocks.

 Sir Edmund Halley proposed to estimate the age of the earth using salt content of the

oceans, assuming that the oceans were once non-saline and that salt addition to the oceans

corresponded in some linear fashion with time.

 Lord Kelvin estimated the age of the Earth at 24-40 million years. He proposed that the

Earth has been cooling since it formed, and he calculated the rate of cooling using principles of

heat conduction.

 It wasn‟t until Henri Becquerel discovered radioactivity in 1896 and Madame Curie isolated

radium 2 years later that people realized that the Earth had it‟s own source of heat. Thus it

became one of the most useful tools for future scientists.

 The oldest rocks found so far on Earth (based on zircon grains from Australia) have

been dated at 4.1-4.2 billion years.

 Meteorites have also been dated at 4.6 billion years. Meteorites are considered to be

remnants of a plant or asteroid that originally formed at the same time as the Earth, so

that the Earth‟s age is currently estimated to be 4.6 billion years.

 The oldest fossils are preserved remains of stromatolites, which are layers of lithified

blue-green algae, dating to approximately 3.5 billion years before present.

How Old is Old?

Table of Contents

Eons:

Precambrian: Earliest span of time

Phanerozoic: Everything since

Eras:

Paleozoic

Mesozoic

Cenozoic

Periods:

Cambrian

Ordovician

Silurian

Devonian

Carboniferous

(Missipp. & Pennsylvanian)

Permian

Triassic

Jurassic

Cretaceous

Paleogene

Neogene

Quaternary

Epochs:

Paleocene

Eocene

Oligocene

Miocene

Pliocene

Pleistocene

Holocene

We are living in the Phanerozoic Eon, Cenozoic Era, Quaternary

Period, Holocene Epoch……..BUT

Paleozoic

“Age of

Invertebrates”

Mesozoic

“Age of Reptiles”

Cenozoic

“Age of

Mammals”

Table of Contents

A new concept has been gaining

momentum since it‟s introduction by

Paul Crutzen in 2000. He proposed that

the Holocene Epoch is over and a new

geological epoch called the Anthropocene

has begun.

Mans‟ impact on the Earth‟s climate and

ecosystems since the Industrial

Revolution is quite evident. Support for

this theory comes from data derived from

glacial ice cores showing the growth in

greenhouse gases starting from the

1800‟s.

Does this justify a new Epoch on the

Geological Time Scale? Some scientists

question this, however, there is no doubt

that there has been a shift in Earth‟s

atmosphere and biosphere as we emerge

from the most recent ice age which ended

approximately 10,000 years ago.

This is strong indication that

geologic time is not a thing of the

past!

Photo used with permission from the cover of GSA

Today, Geological Society of America, Vol. 18, 2, Feb.

2008.

Table of Contents

The Earth Through Time

Standard 8-2.5: Illustrate the vast diversity of life that has been present on Earth over time by using the geologic time scale.

 No life possible as the Earth initially forms 4.6

billion years ago.

 Simple, single-celled forms of life appear 3.8

billion years ago, becoming more complex and

successful over the next 3 billion years:

Prokaryotes then Eukaryotes

 Cyanobacteria begins producing free oxygen

(photosynthesis)

 Land masses gather to make up a continent

called “Rodinia”

Cambrian:

 Explosion of life

 All existing phyla come into being at this time

 Life forms in warm seas as oxygen levels rise

enough to support life

 Dominant animals: Marine invertebrates

(trilobites and brachiopods)

 Supercontinent Gondwana forms near the South

Pole (note position of present-day Florida)

The Proterozoic:

PaleoMaps used with permission from Christopher Scotese and are under

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Ordovician:

Silurian:

 The 1

animals with bones appear, though

dominant animals are still trilobites, brachiopods

and corals

 The beginning of the construction of South

Carolina

 A very cold time in Earth‟s history: there was a

great extinction due to ice caps in present-day

Africa

 Four main continents: Gondwana, Baltica,

Siberia and Laurentia

 First land plants appear and land animals follow

 Laurentia collides with Baltica and closes

Iapetus Sea.

 Coral reefs expand and land plants begin to

colonize barren land.

 First millipede fossils and sea scorpions

(Euryptides) found in this period

PaleoMaps used with permission from Christopher

Scotese and are under copyright of C.R. Scotese, 2002

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Devonian (Age of the Fish)

Mississippian:

 First seed plants appear

 Much of North America is

covered by shallow seas and sea

life flourishes (bryoza, brachipods,

blastoids)

Pennsylvanian:

 Modern North America begins

to form

 Ice covers the southern

hemisphere and coal swamps

formed along equator.

 Lizards and winged insects first

appear.

 Pre-Pangea forms. Dominant animal:

fish

 Oceans still freshwater and fish

migrate from southern hemisphere to

North America.

 Present-day Arctic Canada was at the

equator and hardwoods began to grow.

 Amphibians, evergreens and ferns

appear

 The Acadian Orogeny, leading to S.C.

metamorphism

PaleoMaps used with permission from Christopher Scotese and are under

Table of Contents

Permian:

 Last period of the Paleozoic

 Pangea forms. Reptiles spread

across continents.

 The Appalachians rise

 90% of Earth‟s species become

extinct due to volcanism in Siberia.

This marks the end of trilobites,

ammonoids, blastoids, and most

fish.

Triassic:

 First dinosaurs appear

 First mammals- small rodents appear

 Life and fauna re-diversify

 Rocky Mountains form.

 First turtle fossil from this period

 Pangea breaks apart

PaleoMaps used with permission from Christopher Scotese and are under

Table of Contents

Jurassic:

 Pangea still breaking apart

 Dinosaurs flourish “Golden age of

dinosaurs”

 First birds appear

 North America continues to rotate away

from Africa

Cretaceous:

 T-Rex develops

 First snakes and primates appear

 Deciduous trees and grasses

common

 First flowering plants

 Mass extinction marks the end of

the Mesozoic Era, with the demise

of dinoaurs and 25% of all marine

life.

PaleoMaps used with permission from Christopher Scotese and are under copyright of

C.R. Scotese, 2002

Table of Contents

Tertiary:

 First horses appear and tropical

plants dominate (Paleocene)

 Grasses spread and whales, rhinos,

elephants and other large mammals

develop. Sea level rises and

limestone deposits form in S.C.

(Eocene)

 Dogs, cats, and apes appear

(Oligocene)

 Horses, mastadons, camels, and

tigers roam free in S.C. (Miocene)

 Hominids develop and the Grand

Canyon forms (Pliocene)

Quaternary:

 Modern humans develop and ice

sheets are predominant- Ice age

(Pleistocene)

 Holocene Humans flourish

(Holocene)

PaleoMaps used with permission from Christopher Scotese and are under

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Standard 8-2.1: Explain how biological adaptations of populations enhance their survival in a particular

environment.

Adaptation and ‘Survival of the Fittest’

 Some populations, whether mammals, amphibians, or reptiles are better adapted to living

conditions than others, even within the same species, so they are better at surviving than others.

Because their chances of surviving are increased, their chances of reproducing offspring are better,

and their offspring will possess the same strong traits. This is the basis for natural selection over

long periods of time.

 Natural selection refers to the process where over long periods of time, helpful variations can

appear in a species while “unfavorable” one disappear. For example, a group of frogs living on the

rocky side of an island may, over time, adapt a gray skin color to help blend in with their rocky

environment in while a group of frogs living on the more lush, vegetated side of the island may

develop a green skin color to blend in with their particular environment. Even though the frogs are

of the same species, they are able to incorporate different traits to help them survive in their

environments.

 The theory of natural selection, sometimes referred to as „Survival of the fittest,‟ started with

Charles Darwin‟s 5-year trip around the world on the HMS Beagle. During this time, he noticed

variations within the same species, especially in the Galapagos Turtles, and noted that some of the

variations were favorable and some were not. He concluded that not all members of a species

survive, which is why the world is not overpopulated by any one species. The practicality of their

adaptation must be a determining factor for who survives and who does not. He published his

findings on his return to England and wrote the classic work “The Origin of Species.”

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Standard 8-2.3: Explain how Earth’s history has been influenced by catastrophes (including the impact of an asteroid or

comet, climatic changes, and volcanic activity) that have affected the conditions on Earth and the diversity of its life-forms.

Punctuated Events Through Geologic Time

 Environmental changes on earth are usually an indicator of a species extinction (or a

species addition). These changes can be brought about by an asteroid or comet impact,

volcanic activity, or climatic changes like the onset of ice ages.

1. Impact:

 The most well-known extinction is the extinction of the dinosaurs. Scientists think

that this mass extinction was caused by a large comet that impacted the earth in present-

day Mexico, causing a massive quantity of dust to rise up into the atmosphere, possibly

blocking out the sun and affecting the oxygen levels Earth. Many plants died, and the

animals that depended on those plant for life died as well. In addition, it may have

become very cold in a short period of time.

 It took millions of years for the earth to recover, and when it did, the large dinosaurs

were gone forever.

 Certain species of birds, however, did survive and began to flourish. Birds are

thought to be direct descendants of dinosaurs.

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2. Climate Changes

 Climate has always been a constantly changing phenomenon. The earliest atmosphere was

devoid of free oxygen, and it wasn‟t until the earliest life forms evolved that the present-day

atmosphere began to form approximately 600 million years ago.

 During the Paleozoic, warm shallow seas and tropical climates were common. Life forms that

could not adapt to these conditions disappeared.

 Throughout the Mesozoic era, plate movement shifted the continents and only the animals and

plants with the greatest ability to adapt could survive the extreme changes in temperatures that

occurred as a consequence. Plants with seed coverings and animals with constant internal

temperatures (warm-blooded) lived during this era.

 Climate continued to change during the Cenozoic and continues to change to this day, as issues

of “Global Warming” have been on the fore-front for over a decade. It was only ~12,000 years ago

that the world was in an “ice age” mode. Also, many mountain ranges formed during this era,

causing climate differences due to elevation changes.

 Ice ages have occurred many times in Earth‟s history. Climate shifts like these may be caused by

magnetic polar reversals or variation in the tilt of the earth (called Milankovitch cycles). Obviously,

not all life can adapt to the extreme cold. Also, not all animals can adapt to the warming climate at

the end of an ice age, which probably contributed to the extinction of the wooly mammoth.

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3. Volcanic Activity

 Significant volcanic activity, which produced ash clouds in the air and lava flows on the Earth‟s

surface, was common during the Precambrian. It was extremely hot, and most life forms could not

exist in these conditions.

 Volcanism is a common byproduct of tectonic plate collision. If one plate collides with another

and is pulled underneath it, a subduction zone is formed underneath the plates and a volcanic arc

forms on the Earth‟s surface. During the Paleozoic and Mesozoic, continents were regularly

colliding with each other and volcanism was common. Plate boundaries are still the most common

sites of volcanoes today.

 If volcanism is significant enough to produce mass

quantities of ash and volatile gases, wind can carry

these into the upper atmosphere all around the world,

potentially enveloping the earth in semi-darkness and

reducing insulation on earth. Obviously, this would

have an effect on all living things on Earth.

 A cause and effect phenomenon, catastrophic events

impact life on Earth, whether through an extinction or

creation of new traits for adaptation to already

existing plants and animals.

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Standard 8-2.7: Summarize the factors, both natural and man-made, that can contribute to the extinction of a species.

Why Extinction?

 Extinction of a species occurs when no more members of a particular species remains. Extinction

through time is very common, and, in fact, nearly 90 percent of all species that ever lived on Earth

are now extinct.

 Organisms that cannot survive a catastrophic or significant change in earth‟s climate usually

become extinct. Extinctions are a way of clearing the path for new kinds of life that is potentially

more advanced. This is a natural part of life‟s process.

 Natural phenomena that can contribute to the extinction of a species include global climate

changes, volcanic explosions, and celestial impacts.

 The influence of humans on the environment do not

include comet impacts or volcanism; however, man has

caused extinctions all the same. Over the past few

hundred years, man has cut rainforests and woodland

forests, destroying natural habitats. Pollution from

industrial plants and vehicles has also affected the air

we breath and contributed to greenhouse gases, which

drive global warming. We are looking at the potential

extinction of many species due to this warming trend.

 In addition to threatening less-adaptive creatures

than ourselves, man is negatively impacting biological

resources that our own species need. Man can adapt to

many things with the help of technology.

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Summarize how scientists study Earth’s past environment and diverse life-forms by examining different types of fossils

(including molds, casts, petrified fossils, preserved and carbonized remains of plants and animals and trace fossils)

The study of Fossils

 A fossil is the preserved remains of an organism that has died. Fossils tell scientists,

called paleontologists, about living things such as their biology and environmental

conditions over earth‟s history through the rock record. In addition, they give clues to

the conditions of the earth (i.e. climate) at the time that the fossil was preserved and

possibly relate changes of an organism over time.

 Definitions of fossil types:

Mold fossils: when sediments bury an organism and the sediment hardens into rock. The

organism decays slowly inside the rock, leaving an cavity in the shape of the organism.

 Cast fossil: The cavity or mold mentioned above can filled in with mud. When the mud

hardens, it takes on the shape of the organism.

 Petrified fossil or permineralized fossil: Minerals like calcium can soak into the buried

remains of an organism. The mineral replaces the remaining bone and changes it into rock.

 Carbonized fossil: When organism parts are pressed between layers of mud or clay that

hardens over time, squeezing the decaying organism away and leaving a carbon imprint in

the rock, since all living things contain carbon.

 Trace fossil: When the mud or sand hardens into rock where a footprint, trail or burrow

was left behind.

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Standard 8-2.2

 The fossil record, like the rock record, is an important record for understanding life on

earth before the dawn of man.

 Extinctions and new life forms are also found within the fossil record.

 Fossils can also show structural similarities and differences in organisms over time

revealing the diversity of life forms on earth. Nearly 90 percent of organisms that have

lived on the earth are now extinct.

Carbon imprint of fish

remains, age unknown

Belemnite fossil (cast), cut

and polished. Related to

present-day squid. Extinct.

Brachiopods in a sandstone matrix and an

individual brachiopod cast. Extinct.

A trilobite cast from the

Mississippian Period. Extinct.

Ammonite fossil

(cast), cut and

polished. Related

to present-day

snail. Extinct.

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Standard 8-2: The student will demonstrate an understanding of Earth‟s biological diversity over

time. (Life Science, Earth Science)

Indicators

8-2.1 Explain how biological adaptations of populations enhance their survival in a

particular environment.

8-2.2 Summarize how scientists study Earth‟s past environment and diverse life-

forms by examining different types of fossils (including molds, casts, petrified fossils,

preserved and carbonized remains of plants and animals, and trace fossils).

8-2.3 Explain how Earth‟s history has been influenced by catastrophes (including the

impact of an asteroid or comet, climatic changes, and volcanic activity) that have

affected the conditions on Earth and the diversity of its life-forms.

8-2.4 Recognize the relationship among the units—era, epoch, and period—into

which the geologic time scale is divided.

8-2.5 Illustrate the vast diversity of life that has been present on Earth over time by

using the geologic time scale.

8-2.6 Infer the relative age of rocks and fossils from index fossils and the ordering of

the rock layers.

8-2.7 Summarize the factors, both natural and man-made, that can contribute to the

extinction of a species.

South Carolina Science Academic Standards:

Grade 8

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