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THE EVOLUTION OF EXTINCT ANIMALS
THE EVOLUTION OF EXTINCT ANIMALS
Introduction
Have you ever wondered what other extinct animals have lived on earth in addition to dinosaurs?
Have you ever wondered how and when such enormously successful animals went extinct? This
lab will introduce you to many other extinct animals and help you understand why extinctions
are important historical events to study. This lab was developed by Phil Novack-Gottshall at Benedictine University.
Part I. Pick your group of extinct animals
Most animal species that have ever lived are now extinct! Use the last page of this activity to
choose one of the extinct (or mostly extinct) groups of animals to focus on for this activity. What group of extinct animals are you studying for this activity? Pterosauria
1.
Use the internet to find reputable sources that describe the biology of your chosen group.
Briefly describe how the animals lived
. (For example, did they live underwater or on land?
Could they crawl or walk or swim or fly, or where they immobile? Did they eat plants, other
animals, microscopic algae, or microscopic organisms in mud?) Make sure to write down
what sources you used for this information. (8 points)
Pterosauria were a group of flying reptiles. They were as small as a sparrow, to as big as an airplane. Due to their many different beaks, they probably took advantage of a whole bunch of different food sources. It definitely ate a large amount of fish due to it being able to fly and glide in. They were the biggest flying reptiles to like. https://ucmp.berkeley.edu/diapsids/pterosauria.html
2.
Draw (or print and attach) a picture of a typical animal in your group. Remember to include a scale bar, and label key features or body parts. Also label the symmetry (5 points)
Part II. Introduction to the geological timescale
Since the 1700s, geologists (scientists who study
the earth, including rocks, earthquakes, volcanoes,
streams, and fossils) have used fossils to develop
the geological timescale. It wasn't until the 20
th
century, however, that they were able to add
specific dates. Figure 1 shows a recent geological
timescale, with the last 542-million years of
history divided into three eras (Paleozoic,
Mesozoic, and Cenozoic Eras), each further
subdivided into a series of periods.
3.
According to the timescale, what Era and
Period are you living in today? (In other
words, what intervals are the most recent?) (2
points)
The Cenozoic and the Neogene and further in the
Quaternary.
Paleontologists (biologists and geologists who
study the fossil record of life) have discovered
that there have been five major mass extinctions
in the history, which
have had enormous impact
on life by quickly killing enormous numbers of
animals and plants around the world. We now
recognize that all of these mass extinctions were
caused by major environmental catastrophes. The
most famous example was the Late Cretaceous
mass extinction
, caused by a meteorite that
crashed to Earth 66 million years ago. It threw so much ash into the atmosphere that the earth felt
like nighttime for many years, preventing algae,
plants, and animals from being able to get enough
food to survive.
The Late Permian mass
extinction
was the most devastating of all
extinctions. It was caused by enormous volcanic
eruptions that released so much carbon dioxide that
earth's atmosphere heated up dramatically by
global warming.
These two mass extinctions so dramatically affected life on earth that they are used to define the
boundaries surrounding the Paleozoic (etymologically, "ancient life"), Mesozoic ("middle life"),
and Cenozoic ("recent life") Eras.
4.
Which occurred first, the Late Permian or the Late Cretaceous mass extinction? How many
mass extinctions have occurred in the last 542 million years?
(1 point)
Figure 1. Geological timescale. Numbers on the left note when each era started and ended (in millions of years ago, m.y.a.). The Paleozoic, Mesozoic, and Cenozoic Eras correspond to the three eras of animal life, and they are subdivided into various periods, listed on the right. The Carboniferous Period sometimes is divided into the Mississippian and Pennsylvanian Periods, and the most recent two periods are similarly treated variably, sometimes with the Quaternary Period falling after the Neogene Period. The five mass extinctions are noted with arrows on the right of the timescale.
There have occurred 5 extinctions in the last 542 million years. The Late Permian happened
before the Late Cretaceous.
Part III. Diversity curves and the Paleobiology Database
The Paleobiology Database (PBDB)
is a very powerful online resource for fossil research that
allows scientists and the public to access information on fossil collections around the world and
throughout geological time. For today's activity, we will use the Navigator interface to view the
its data. This should be familiar from last week’s lab, but here are some instructions again on
how to use the database. Delving into the Database
Open the PBDB Navigator and spend some time getting comfortable with how it works: https://paleobiodb.org/navigator/
The Navigator consists of three parts:
1)
Map (
CENTER
) showing continents with dots representing fossil data. The color of these dots represents their geologic age. If you click on the dots, you can see all of the information on each fossil locality and the plants, animals, and other fossil life that occur there.
2)
Geologic time scale (
BOTTOM
) showing the major eras and periods (and their subdivisions called stages). If you click on the timescale, the map will show you the location of all known fossil localities from that time interval.
3)
Tool bar (
LEFT
) showing the tools you can use to explore the database. These include:
zoom in/out on the map
reconstructs plate tectonic configurations for time interval you are exploring narrow down which taxonomic group is plotted on map
create a diversity curve for the occurrences currently plotted on map
download the data (lat/long, geologic age, etc.) for the occurrences plotted on map
Need help?
Here’s a Youtube video to help you get started: www.youtube.com/watch?v=db2He3p-Jco
5.
On the PBDB Navigator homepage, look under the map to the geological timescale. Are the oldest rocks to the left or to the right on this timescale? Explain how you know this. (3 points)
The oldest rocks are to the left since we know that the Neogene is close to our time and that is on the right
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Diversity curves graph the history of life
Diversity curves allow paleontologists to graph how many different kinds of fossil animals (or
plants or protists) existed on earth during different geological time intervals. They are especially
important for telling us (a) when a group of animals first evolved
on earth, (b) when that group
diversified
(increased in diversity) and became common on earth, and (c) when that group went
extinct
. Let's make a diversity curve for the group of extinct animals you chose in Part I above.
6.
Type the name of your animal group in the search box on the top-right corner of the PBDB
Navigator window. (Make sure to spell it exactly correctly!) When you see the name in the
drop-down box, select it.
You will now see the dots change on the map, showing you where fossils of these animals
have been discovered. Each color corresponds to a unique color on the geological timescale
on the bottom of the page. (The pictures on the right will show you a cartoon drawing of
major subgroups of your chosen group.)
7.
Make a diversity curve for your group by clicking the tool on the left side. You will see
a new window show up. (The
default settings are fine to use.)
Save this image (using the
tools on the right side of the
diversity window). Print the
diversity curve and attach it to
this activity. Make sure to
write the name of the group
of animals on your diversity
curve!
8.
The y-axis plots diversity
, the number of different kinds of animals that occur in the fossil
record during each time interval. (Technically, the graph is plotting genus diversity, or the
number of groups of closely related species in different genera.)
9.
What is the largest diversity observed at any one time in the history of your animal group? (In other words, what is the largest value on the y-axis?) (2 points) About 40 animal groups
10. The first time you see a value on the diversity curve is generally when your animal group first evolved. During what geologic time period did your extinct animal group first appear in
the fossil record? (2 points) During the Mid-Triassic
11.
Did this period occur during the Paleozoic, Mesozoic, or Cenozoic Era? (2 points)
This occurred during the Mesozoic
12.
During what time period did your animal group go extinct? (If your group is not extinct yet, then write that it is not yet extinct.) (2 points)
They went extinct during the late Cretaceous mass extinctions.
13.
During what period(s) was your animal group most diverse? During what era(s) was it most diverse? (2 points)
It was most diverse in the Cretaceous, Mesozoic.
14.
Some people think extinct animals were evolutionary failures because they are extinct today,
or nearly so. Some also claim they were never successful or common animals on earth.
Based
on the diversity curve, is it fair to claim that your extinct group was a failure? Why or why
not? (For comparison, primates have existed for just 16 million years and our species for
only 250,000 years.) (8 points) I think it was widely successful for its time as it lasted almost
200 million years and had good diversity. It was the extinction that really put them away.
You may notice that diversity curves sometimes rise quickly. These are intervals when the
animal group was common and successful on earth, usually because the environmental
conditions needed for these animals to survive (such as food, climate, and other conditions)
were widely available on earth. Other times you may see diversity drop quickly. These may
have been intervals when the group suffered extinctions because the necessary conditions
were not present.
15. Let's analyze how your group was affected by the five major mass extinction in earth history.
For each mass extinction, explain whether it (a) had not yet originated, (b) was not affected
by the extinction (meaning it did not have a major drop in diversity at this time), (c) was
heavily affected by the extinction (meaning diversity drops significantly at this time), or (d) it
went extinct before the mass extinction.
a.
Late Ordovician mass extinction: They were not around at the time
b.
Late Devonian mass extinction (occurring throughout the end of the Devonian Period
and not just as the very end of the Devonian): They were not around during this time
c.
Late Permian mass extinction: They were not around at this time
d.
Late Triassic mass extinction: They lost some of their diversity, but they held on and
continued to survive
e.
Late Cretaceous mass extinction: This was the extinction that put them away.
16. Which mass extinction was the most catastrophic for your group? Explain your answer. (5
points)
The Late cretaceous was the most catastrophic since it is the one that wiped them out never
to be seen again. Other than this there was one other that almost made them go extinct, but it
was not nearly as bad.
17. If your animal group is extinct today, did its extinction occur during a mass extinction?
Explain your answer. (4 points)
Yes, they went extinct during the late cretaceous extinction since the graph cuts out right after
that.
18. If you went back in a time machine 100 or 400 million years ago, do you think the kinds of
animals (and plants) you would observe on earth would be similar to those living today, or
would life be quite different? Explain your answer. (10 points)
Life would be different. It had much bigger animals such as this group of animals who were
massive reptiles that could fly. Apart from this, the means to survive would be so different from
today it would be unrecognizable. There were different food sources, and probably not as much
variety as there is today.
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LIST OF EXTINCT GROUPS OF ANIMALS
Below is a list of major groups of extinct (or nearly so) animals. Also provided is a guide to pronunciation, the basic kind of animal, and sometimes with a famous genus.
Rugosa (
Rue-go'-suh
, a group of Paleozoic corals)
Tabulata (
Tab'-ewe-la-tuh
, a group of Paleozoic corals)
Lingulata (
Ling'-ewe-lah'-tuh
, a group of primarily Paleozoic brachiopods)
Strophomenata (
Strow'-foe-men'-ah-tuh
, a group of Paleozoic brachiopods)
Hyolithida (
Hi-oh-lith'-ih-duh
, a group of Paleozoic mollusk-like animals)
Rostroconchia (
Ro'-strow-conch'-ee-uh
, a group of Paleozoic mollusks)
Orthocerida (
Ore'-tho-sehr'-ih-duh
, a group of Paleozoic cephalopod mollusks)
Goniatitida (
Gohn'-ee-uh-tid'-uh-duh
, a group of Paleozoic cephalopod mollusks)
Ammonitida (
Amm'-oh-nid'-uh-duh
, a group of Mesozoic cephalopod mollusks)
Belemnitida (
Beh-lem'-nid'-uh-duh
, a group of Mesozoic cephalopod mollusks)
Trilobita (
Try-low-buy'-tuh
, a group of Paleozoic arthropods)
Eurypterida (
You-rip'-tuhr-uh-duh
, a group of Paleozoic arthropods)
Crinoidea (
Cry-noi'-dee-uh
, a group of primarily Paleozoic echinoderms)
Blastoidea (
Blass-toi'-dee-uh
, a group of Paleozoic echinoderms)
Edrioasteroidea (
Ee-dree'-oh-ass'-tuhr-oy'-dee-uh
, a group of Paleozoic echinoderms)
Eocrinoidea (
Ee'-oh-cry-noi'-dee-uh
, a group of Paleozoic echinoderms)
Rhombifera (
Rohm-bih'-fur-uh
, a group of Paleozoic echinoderms)
Eupelycosauria (
You-pell'-ih-co-sar'-ee-uh
, a suborder of Paleozoic vertebrates, including Dimetrodon
)
Dicynodontia (
Die-sigh'-no-don'-tee-uh
, a subgroup of Paleozoic and Mesozoic vertebrates)
Dinosauria (
Dye'-no-sar'-ee-uh
, a group of Mesozoic reptiles)
o
Note that biologists consider birds descendants (living members) of the dinosaurs, and so if you choose this group, you will also have to study the "true bird" group
Aves (
Aye'-vees
) and then subtract out the birds from the larger group Dinosauria to focus just on the "extinct" dinosaurs that were not birds.
Plesiosauria (
Please'-ee-oh-sar'-ee-uh
, a group of Mesozoic reptiles)
Pterosauria (
Terr'-ah-sar'-ee-uh
, a group of Mesozoic reptiles)
Mosasauria (
Moh'-suh-sar'-ee-uh
, a group of Mesozoic reptiles)
Ichthyosauria (
Ick'-thee-oh-sar'-ee-uh
, a group of Mesozoic reptiles)
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