Geologic Time and Earth’s
Biological History
Designed to meet South Carolina
Department of Education2005 Science Academic Standards

Table of Contents
 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)
 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)2

Table of Contents, cont. (2 of 2)
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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)

3What is the Geologic Time Scale?
Standard 8-2.4: Recognize the relationship among the units—era, epoch, and period—into which the geologic time scale isdivided.

What does the time scale represent?

 The geologic time scale divides up the history of the earth based on life-forms thathave existed during specific times since the creation of the planet. These divisions arecalled geochronologic units (geo: rock, chronology: time).
 Most of these life-forms are found as fossils, which are the remains or traces of anorganism 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: 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 canvary from continent to continent.
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4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.
Examples Cambrian: From the Latin name for Wales. Named for exposures ofstrata 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
 The earliest time of the Earth is called the Hadean and refers to a period of time for which wehave 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 ofgeologic 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 aperiod is called a system, so rocks from the Cambrian Period are of the Cambrian system.
Table of Contents 5

GEOLOGIC TIME SCALE
MYA

ERA

PERIOD

PLATE TECTONICS

LIFE

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 theAmericas5.3

Pliocene-Volcanic activity in North
America and Africa-Grand Canyon forms

Hominids develop

MioceneSandhills form in S.C.

Horses, mastadons, mammoths,
tigers, and camels live in South
Carolina

Oligocene

Appalachians uplift; erosion
increases

Cats, dogs, and apes appear

54.8

EoceneSea levels rise; deposits of marine
sediments – limestone in S.C.;
land bridges form

-Grass spreads widely-Diverse array of animals develop,
including whales, rhinos, andelephants

65.0

Paleocene

Earthquakes common; Georgia
Embayment, Cape Fear Arch
forms in Southeast-First horses appear (size of a cat)
-Tropical plants dominate

Cretaceous

Mass extinction occurs at the endof the period caused by ameteorite impact (Dinosaurs,
ammonites and 25% of marine life
become extinct)-T-Rex develops but number ofdinosaur species decline-Snakes appear and first primatesappear-Angiosperms appear

Jurassic

Western US: orogeny of Rockies;
North America continues to rotate
away from Africa-First birds appear-Golden age of dinosaurs

Triassic-Pangea begins to break apart-Rocky Mountains and Sierra
Nevada form

First dinosaurs, mammals,
crinoids, and modern echinoids
appear-Pangea forms-Appalachians rise

-90% of Earth’s species become
extinct, including trilobites,
blastoids, fish and amphibians
because of heavy volcanism inSiberia
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0.01

EPOCH

Quaternary

23.8

Cenozoic“Age of
Mammals”

33.7

Tertiary

144

206

248

290

Mesozoic“Age of
Reptiles”

PermianCarboniferous

320

354

417

443

490

540

4600

Paleozoic“Age ofInvertebrates”

PennsylvanianGreat swamps develop (futurecoal deposits-Reptiles develop fromamphibians-Flying insects appear

Mississippian

Much of North America is underwater-First seed plants appear-Sea life flourishes including
coral, brachiopods, blastoids, andbryozoa

Devonian

Acadian Orogeny – SC
metamorphism-Dominant animals: fish
-Amphibians, evergreens andferns appear

Silurian

Extensive erosion

First land plants appear and land
animals follow

Ordovician-Beginning of the construction ofSouth Carolina-Great extinction due to growth ofice caps including in what is now
northern Africa-First animals with bones appear-Dominant animals: marine
invertebrates including corals andtrilobites

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 asoxygen levels rose enough to
support life
-Dominant animals: trilobites andbrachiopods

Earth takes 10 million years tocool: initial atmosphere escapes
into space (H&He) and the core
forms (Fe&Ni)
Volcanic outgassing of water andcarbon dioxide occurred formillions 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 theatmosphere and sea

No life possible as the Earthinitially 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 thenEukaryotes
Cyanobacteria begins producing
free oxygen (photosynthesis)

Cambrian

Precambrian(Hadean, Archean, and Proterozoic Ages)

Modified after Carolina Rocks, contributed by J. Westmoreland

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7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 theinterpretation 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).
Geologist studying the stratigraphy in

Younger the Copper Basin, Idaho. These rockOlderlayers were deposited horizontally,
and uplifted later so they are now
tilted at an angle (along the red arrow).
(Photo contributed by K. McCarney-Castle) 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
Table of Contents 8“plutonists.”

Principles Behind Geologic Time, continued 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 latercatch-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 offossils 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 thatfossil remains will be unique. This permits vertical and horizontal correlation of the rocklayers based on fossil species.
Rock Outcrop 1

Rock Outcrop 2
300 kmEven though these two outcrops are
separated by a large distance, the samerock layer can be correlated with theother because of the presence of thesame shark teeth. This lets scientists
know that the two layer were depositedat the same time, even if the surroundingrocks look dissimilar from each other.
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9Principles Behind Geologic Time, continued During the early 1800‟s, English Geologist, Charles Lyell published a book called “Principles ofGeology,” which became a very important volume in Great Britain. It included all of Hutton‟sideas, and presented his own contemporary ideas such as:
 The principle of cross-cutting relationships: A rock feature that cuts across another featuremust be younger than the rock that it cuts.
 Inclusion principle: Small fragments of one type of rock but embedded in a second type ofrock must have formed first, and were included when the second rock was forming.
 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 overwhelmedthe 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 ofsurviving to create the next generation.
 The theory of natural selection was credited to Darwin (along with Alfred Russel Wallace) andhe 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 overgeologic time
2. The mechanism for this evolution was natural selection.

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10Relative Age DatingStandard 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 ofan 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 overlarge areas of land. Because rock layers can be “matched up,” we can guess that they wereformed 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 1st.
 Deciphering the sequence of a rock outcrop is sometimes complicated by a features within therock record called unconformities, which are specific contacts between rock layers. There arethree types of unconformities that help us determine relative ages of rock layers:
1. Angular: Horizontal beds are uplifted and tilted oreroded followed by new deposition of horizontal
beds.
The figure to the right is an angular
unconconformity.

Horizontal bed of
sedimentary rock

2. Disconformity:
Episodes of erosion or nondeposition between layers
3. Nonconformity: Sediment is deposited on top oferoded volcanic or metamorphic rock (indicatesvery long passage of time)

Tilted bed of
sedimentary rock

Wikipedia (public domain)

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 Relative ages can also be determined using Lyell‟sprinciple 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, 7th edition, 1996)

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 beused as guides for recognition of chronostratigraphic units.
 Index fossils are widespread, have short temporal durations resulting from rapid life spans, areabundant throughout their geographic and geologic ranges, and are easily recognized (unique).
 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 rocklayers that contain trilobites with a second rock layer and,based on position, determine if the second rock layer isyounger. The photo to the right is a trilobite from theMississippian 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.
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12

Absolute Age Dating
 Absolute ages, or geochronometric ages, of rock can be assigned to the geologic time scale on thebasis 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 likethe 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 iscalled the parent and the new isotope product is called the daughter.
 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 ittakes 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.
Note: Radioactive isotopes can be found in the rock record because radioactive
isotopes are incorporated into the crystals of igneous rock as it cools.

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13

Radioactive Decay
100%

50%
75%

87.5%

93.75%

50%
25%

PARENT

DECAY

12.5%

6.25%

Scientists used the proportion of parent
material remaining to the proportion ofdaughter material produced in order topredict the age of the rock. During each halflife, only one-half of the parent material
decays to the daughter product.

DAUGHTER 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 theisotope used.

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.
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14Commonly used radioactive isotopes
ParentDaughterhalf-life

Mineral or Material

Uranium238

Lead 206

4.56 BY

Zircon, Uraninite, Pitchblende

Uranium 235

Lead 207

704 MY

Zircon, Uraninite, PitchblendePotassium 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 145730 yr

Wood, bone, shell

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

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 abundanceof zircon minerals.
 The subscripts of 235 and 238 are the atomic mass numbers of the element. Though eachisotope 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 sedimentaryrocks. By dating the magma, one can get at least a minimum age for the sedimentary rock.
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15

How Old is Old?
 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 theoceans, assuming that the oceans were once non-saline and that salt addition to the oceanscorresponded 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 ofheat 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 itbecame one of the most useful tools for future scientists.

 The oldest rocks found so far on Earth (based on zircon grains from Australia) havebeen dated at 4.1-4.2 billion years.
 Meteorites have also been dated at 4.6 billion years. Meteorites are considered to beremnants of a plant or asteroid that originally formed at the same time as the Earth, sothat 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.
Table of Contents 16

Eons:
Precambrian: Earliest span of time
Phanerozoic: Everything since
Eras:
Paleozoic
Mesozoic
Cenozoic
Paleozoic“Age ofInvertebrates”

Periods:
CambrianOrdovician
Silurian
Devonian
Carboniferous(Missipp. & Pennsylvanian)Mesozoic“Age of Reptiles”

Cenozoic“Age of
Mammals”

PermianTriassic
Jurassic
Cretaceous
Paleogene
NeogeneQuaternary

We are living in the Phanerozoic Eon, Cenozoic Era, Quaternary
Period, Holocene Epoch……..BUT

Epochs:Paleocene
EoceneOligocene
MiocenePliocene
Pleistocene
Holocene

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17

A new concept has been gaining
momentum since it‟s introduction by
Paul Crutzen in 2000. He proposed thatthe Holocene Epoch is over and a newgeological epoch called the Anthropocene
has begun.
Mans‟ impact on the Earth‟s climate andecosystems
since
the
Industrial
Revolution is quite evident. Support forthis theory comes from data derived fromglacial ice cores showing the growth ingreenhouse gases starting from the1800‟s.
Does this justify a new Epoch on the
Geological Time Scale? Some scientists
question this, however, there is no doubtthat 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 thatgeologic 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 18

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.

The Proterozoic:
 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 andsuccessful 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)
PaleoMaps used with permission from Christopher Scotese and are undercopyright of C.R. Scotese, 2002

19
Table of Contents 19

Ordovician: The 1st 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 agreat extinction due to ice caps in present-day
Africa Four main continents: Gondwana, Baltica,
Siberia and Laurentia

Silurian: First land plants appear and land animals follow
 Laurentia collides with Baltica and closes
Iapetus Sea.
 Coral reefs expand and land plants begin tocolonize 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

20
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20

Devonian (Age of the Fish)
 Pre-Pangea forms. Dominant animal:fish
 Oceans still freshwater and fish
migrate from southern hemisphere to
North America.
 Present-day Arctic Canada was at theequator and hardwoods began to grow.
 Amphibians, evergreens and ferns
appear The Acadian Orogeny, leading to S.C.
metamorphism
Mississippian: First seed plants appear
 Much of North America iscovered by shallow seas and sea
life flourishes (bryoza, brachipods,
blastoids)

PaleoMaps used with permission from Christopher Scotese and are undercopyright of C.R. Scotese, 2002

Pennsylvanian: Modern North America begins
to form
 Ice covers the southernhemisphere and coal swamps
formed along equator.
 Lizards and winged insects first
appear.

21
Table of Contents21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 mostfish.

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 undercopyright of C.R. Scotese, 2002

Table of Contents

22Jurassic:
 Pangea still breaking apart Dinosaurs flourish “Golden age ofdinosaurs”
 First birds appear

 North America continues to rotate awayfrom 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 demiseof dinoaurs and 25% of all marine
life.
PaleoMaps used with permission from Christopher Scotese and are under copyright of
C.R. Scotese, 2002
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23

Tertiary: First horses appear and tropicalplants dominate (Paleocene) Grasses spread and whales, rhinos,
elephants and other large mammals
develop. Sea level rises andlimestone deposits form in S.C.
(Eocene) Dogs, cats, and apes appear(Oligocene) Horses, mastadons, camels, andtigers 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 undercopyright of C.R. Scotese, 2002

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24Adaptation and ‘Survival of the Fittest’Standard 8-2.1: Explain how biological adaptations of populations enhance their survival in a particularenvironment.

 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 overlong periods of time.
 Natural selection refers to the process where over long periods of time, helpful variations canappear 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 areof the same species, they are able to incorporate different traits to help them survive in theirenvironments.
 The theory of natural selection, sometimes referred to as „Survival of the fittest,‟ started withCharles 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 thevariations 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 theiradaptation 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.”
Table of Contents 25

Punctuated Events Through Geologic Time
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.

 Environmental changes on earth are usually an indicator of a species extinction (or aspecies 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 thinkthat this mass extinction was caused by a large comet that impacted the earth in presentday 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 theanimals that depended on those plant for life died as well. In addition, it may havebecome 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.
thought to be direct descendants of dinosaurs.

Birds areTable of Contents26

2. Climate Changes
 Climate has always been a constantly changing phenomenon. The earliest atmosphere wasdevoid 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 andplants 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 issuesof “Global Warming” have been on the fore-front for over a decade. It was only ~12,000 years agothat 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 bymagnetic 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‟ssurface, was common during the Precambrian. It was extremely hot, and most life forms could notexist in these conditions.
 Volcanism is a common byproduct of tectonic plate collision. If one plate collides with anotherand 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 massquantities of ash and volatile gases, wind can carrythese into the upper atmosphere all around the world,
potentially enveloping the earth in semi-darkness andreducing 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 alreadyexisting plants and animals.
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Why Extinction?

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

 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 Earthare 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 potentiallymore advanced. This is a natural part of life‟s process.
 Natural phenomena that can contribute to the extinction of a species include global climatechanges, volcanic explosions, and celestial impacts.
 The influence of humans on the environment do notinclude comet impacts or volcanism; however, man has
caused extinctions all the same. Over the past few
hundred years, man has cut rainforests and woodlandforests, destroying natural habitats. Pollution fromindustrial 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 biologicalresources that our own species need. Man can adapt tomany things with the help of technology.

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Standard 8-2.2

The study of Fossils

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)

 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 tothe conditions of the earth (i.e. climate) at the time that the fossil was preserved andpossibly 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 mudhardens, 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.
Table of Contents30 The fossil record, like the rock record, is an important record for understanding life onearth 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.

A trilobite cast from theMississippian Period. Extinct.
Carbon imprint of fish
remains, age unknown

Belemnite fossil (cast), cut
and polished. Related topresent-day squid. Extinct.

Brachiopods in a sandstone matrix and an
individual brachiopod cast. Extinct.

Ammonite fossil(cast), cut andpolished. Relatedtopresent-day
snail. Extinct.

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South Carolina Science Academic Standards:
Grade 8
Standard 8-2: The student will demonstrate an understanding of Earth‟s biological diversity overtime. (Life Science, Earth Science)
Indicators
8-2.1
Explain how biological adaptations of populations enhance their survival in aparticular environment.
8-2.2
Summarize how scientists study Earth‟s past environment and diverse lifeforms 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 theimpact of an asteroid or comet, climatic changes, and volcanic activity) that haveaffected 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 byusing 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 theextinction of a species.
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