Chapter 25 - The History of Life

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A collection of flashcards based on major concepts from the lecture notes regarding the history of life on Earth and key evolutionary events.

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61 Terms

1
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What is true about the origin of life?

-It is a hypothesis

-Extremely speculative

-No fossil evidence

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In the 1920s, what hypothesis did A. I. Oparin and J. B. Haldane propose about the early atmosphere?

They hypothesized it was a reducing environment (electron adding); conducive to forming organic compounds.

-Energy for organic compound synthesis was supplied by lightning or UV radiation

-Haldane suggested early oceans were a primordial soup of organic molecules that gave rise to life

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What did Stanley Miller and Harold Urey demonstrate in their 1953 experiments?

They showed abiotic synthesis of organic molecules was possible in a reducing atmosphere.

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What is the endosymbiont theory?

It suggests that mitochondria and chloroplasts were once independent prokaryotes that began living symbiotically within larger cells.

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What major biological event occurred around 3.5-3.2 billion years ago?

The evolution of photosynthesis

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What were stromatolites?

Fossilized bacteria that formed from sedimentary layers on bacterial mats, indicating life existed 4.0 billion years ago.

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How did the first eukaryotes evolve according to the notes?

They evolved from prokaryotes through processes including endosymbiosis.

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What changes did the 'oxygen revolution' cause in Earth's biological communities?

It likely led to the extinction of many prokaryotic organisms that could not survive in an oxygen-rich environment.

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The Domains

Eukaryotic, Archaea, and Bacteria

<p>Eukaryotic, Archaea, and Bacteria</p>
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Which domains are the most closely related?

Eukarya and Archaea are sister taxa

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Conditions on early earth

  1. Abiotic synthesis of small inorganic molecules

  2. Joining of these small molecules into marcromolecules

  3. Packaging of molecules into protocells

  4. Original of self-replicating molecules that made inheritance possible

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What are protocells?

Structures formed from abiotic (non-living) components

Made of lipids, membrane-bound, maintaining internal chemistry

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When was earth formed and what is the name of this period?

About 4.6 billion years ago during the formation of the solar system. This period is known as the Hadean Eon (pre-life).

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The bombardment by rocks and ice likely vaporized water during the Hadean Eon preventing what from happening?

Formation of seas

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During the Hadean Era, what was the atmosphere on earth like?

Atmosphere likely contained water vapor and chemicals released by volcanoes (nitrogen, nitrogen oxides, CO2, methane, ammonia, hydrogen)

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In 1953, Stanley Miller and Harold Urey showed that what was possible?

Abiotic (non-living) synthesis of organic molecules in a reducing atmosphere is possible

<p>Abiotic (non-living) synthesis of organic molecules in a reducing atmosphere is possible</p>
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How was the Miller and Urey experiment conducted?

-Used conditions similar to what Oparin and Haldane hypothesized

-Created a variety of acids and other compounds

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What abiotic (non-living) molecules were created in the Miller and Urey experiment?

  1. Amino acids

  1. Long chain Hydrocarbons

  1. Formaldehyde 

  2. Hydrogen cyanide

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Other hypotheses

-Hydrothermal vents: The first organic compounds may have been synthesized near volcanoes or deep-see vents (“Black Smokers” or Alkaline vents)

-Panspermia: The first organic compounds may have been transported by means space dusts, comets, or meteorites.

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RNA monomers can be produced spontaneously from what?

Simple molecules

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Small organic molecules __________ when they are concentrated on hot sand, clay, or rock

polymerize (combine into larger molecule)

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The first genetic material was likely ___?

RNA not dna

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RNA is central to ______ _________ and can function as an enzyme-like catalyst (ribozymes)

protein synthesis

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What are ribozymes and what can they do?

catalytic RNA molecules that function as enzymes Can make complementary copies of short stretches of RNA

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What way are protocells thought to have formed?

Formed from fluid-filled vesicles with a membrane-like structure

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What can lipids and other organic molecules do in water?

They can spontaneously self-assemble to form vesicles with a lipid bilayer

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What is montmorillonite and what does it do?

Montmorillonite is a clay mineral from volcanic ash that can catalyze the formation of RNA and other organic molecules, providing a surface for the assembly of protocells.

<p>Montmorillonite is a clay mineral from volcanic ash that can catalyze the formation of RNA and other organic molecules, providing a surface for the assembly of protocells. </p>
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True of false? Vesicle with self-replicating RNA would differ from neighbors that lack it

True

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If vesicles with self-replicating RNA could grow and split and pass on their RNA to their daughters, what would the daughters become?

They would become protocells

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Inherited features specified by the RNA would be acted on by natural selection. True or false?

True

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Most atmospheric oxygen is of biological origin, produced during what?

During the water splitting step of photosynthesis

Early photosynthesis evolved 3.5-3.2 billion years ago

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How were red bands of rock created?

Oxygen dissolved into the water, reacted with iron, and precipitated out as iron oxide resulting in the build up in sediment, forming red bands of rock containing iron ore

<p>Oxygen dissolved into the water, reacted with iron, and precipitated out as iron oxide resulting in the build up in sediment, forming red bands of rock containing iron ore</p>
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Once all of the dissolved iron precipitated, oxygen began saturating what?

The lakes and seas

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Only after the saturation of bodies of water with oxygen, what happened around 2.7 billion years ago?

Oxygen began to build up in the atmosphere

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Aerobic vs anaerobic 

Refers to processes or organisms that require oxygen (aerobic) versus those that do not need oxygen to survive and can thrive in oxygen-free environments (anaerobic).

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<p>What is the Oxygen Revolution and what did it do?</p>

What is the Oxygen Revolution and what did it do?

-2.7-2.4 billion years ago, atmosphere oxygen levels increased from 0.001% to around 10% of the present level

-Likely caused the extinction of many prokaryotes

-However, some groups survived and adapted using aerobic cellular respiration to harvest energy

-Also, some survived by being confined to anaerobic habitats, led to divergence of many anaerobic prokaryotes 

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How old are the oldest eukaryotic fossils?

1.8 billion years old

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Eukaryotes contains what that prokaryotes do not?

-Nuclear envelope

-Mitochondria

-Endoplasmic reticulum (ER)

-Chloroplasts

-Lysosomes

-Golgi apparatus

-Cytoskeleton

-Rod-shaped chromosomes

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Endosymbiotic Theory

The Endosymbiotic Theory posits that eukaryotic cells originated through a symbiotic relationship between different species of small independent prokaryotes, becoming mitochondria and chloroplasts, living as symbionts within other larger cells; essential organelles in eukaryotic cells.

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Ancestors of mitochondria and plastids likely entered their host as what?

undigested prey or internal parasites

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Evidence of Endosymbiotic theory

1.Mitochondria and chloroplast inner membranes are similar to plasma membranes of prokaryotes

2.”Cell” division and DNA structure is similar in these organelles and related prokaryotes 

3.Transcribe and translate their own DNA

4.Ribosomes are more similar to prokaryotic than eukaryotic ribosomes

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Endosymbiosis in action in Paulinella chromatophora

-Cercazoan (amoeba)

-Around 60 Mya developed an endosymbiosis with a cyanobaterium

-New origin of a chloroplast-like structure known as the chromatophore

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Multicellular organisms can only be found in what domain?

Domain Eukarya (excluding: Euglenozoans, Forams, Diatoms, Ciliates, Amoebas)

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True or false? The evolution of eukaryotic cells allowed for a greater range of unicellular forms

True

<p>True</p>
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Larger and more diverse multicellular eukaryotes emerged in what period?

Example: soft-bodied organisms (most preserved impressions)

Ediacaran Biota - 635 to 540 Mya

<p>Ediacaran Biota - 635 to 540 Mya</p>
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<p>Second wave of diversification occurs (based on fossil record)</p><p>-Evolution of hard bodied animals and evidence of predator-prey interactions (larger size, claws, vs. spines, body armor)</p><p>-Linked to higher atmospheric oxygen levels, ozone, CaCO3</p>

Second wave of diversification occurs (based on fossil record)

-Evolution of hard bodied animals and evidence of predator-prey interactions (larger size, claws, vs. spines, body armor)

-Linked to higher atmospheric oxygen levels, ozone, CaCO3

Cambrian explosion - around 535 Mya 

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When did fungi, plants, and animals begin to colonize land?

What happened?

-Around 500 mya

-Associated with adaptations that made it possible to reproduce on land and resist desiccation (moisture loss)

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What animals were the first to colonize land?

Arthopods (marine animals) around 450 Mya followed by Tetrapods (four limbed vertebrates) around 365 mya

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What is a common cause of mass extinctions?

What most happen for it to be considered a mass extinctions?

-Global environmental disruptions leading to a significant loss of species.

-50% or more of marine species became extinct

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How many mass extinction events have occurred?

Five major events recognized in Earth's history.

<p>Five major events recognized in Earth's history. </p>
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<p><strong>End Ordovician</strong></p>

End Ordovician

Years: around 440 Mya

Extinction: 85% of marine species 

What happened: Supercontinent (Gondwana) moves to South Pole. Glacial and interglacial episodes caused sea levels to rise and fall
dramatically, moving shorelines repeatedly. Continental
erosion changed atmosphere and ocean chemistry. Cooling climate especially hazardous to organisms adapted to warmer temperatures. Glaciation caused loss of intercontinental waterways and continental shelves

<p>Years: around 440 Mya</p><p>Extinction: 85% of marine species&nbsp;</p><p>What happened:&nbsp;<span>Supercontinent (Gondwana) moves to South Pole. Glacial and interglacial episodes caused sea levels to rise and fall</span><br><span>dramatically, moving shorelines repeatedly. Continental</span><br><span>erosion changed atmosphere and ocean chemistry. Cooling climate especially hazardous to organisms adapted to warmer temperatures. Glaciation caused loss of intercontinental waterways and continental shelves</span></p>
52
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<p><strong>Late Devonion/ Kellwasser Event</strong></p>

Late Devonion/ Kellwasser Event

Years: around 375-360 Mya

Extinction: 75%

What happened: Rapid growth of land plants causes mass consumption of atmospheric carbon dioxide, which causes global cooling. Weathering plant roots release nutrients into the sea,
causing algal blooms and oxygen depletion

<p>Years: around 375-360 Mya</p><p>Extinction: 75%</p><p>What happened: <span>Rapid growth of land plants causes mass consumption of atmospheric carbon dioxide, which causes global cooling. Weathering plant roots release nutrients into the sea,</span><br><span>causing algal blooms and oxygen depletion</span></p>
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<p><strong>End Permian (The Great Dying)</strong></p>

End Permian (The Great Dying)

Years: around 252 Mya

Extinction: 57% and lasted around 60,000 years

What happened: Massive amount of volcanic gas (carbon dioxide, methane, hydrogen sulfide, etc.) released from Siberian Traps.
Volcanic eruption estimated to last for ~1,200 years 

Carbon dioxide levels reach
~2000 ppm (Currently ~423ppm)

NOTE: Enough lava to bury the continental United States in
a kilometer of volcanic rock.

<p>Years: around 252 Mya</p><p>Extinction: 57% and lasted around 60,000 years</p><p>What happened:&nbsp;<span>Massive amount of volcanic gas (carbon dioxide, methane, hydrogen sulfide, etc.) released from Siberian Traps.</span><br><span>Volcanic eruption estimated to last for ~1,200 years&nbsp;</span></p><p><span>Carbon dioxide levels reach</span><br><span>~2000 ppm (Currently ~423ppm)</span></p><p><span>NOTE:&nbsp;Enough lava to bury the continental United States in</span><br><span>a kilometer of volcanic rock.</span></p>
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<p><strong>End Triassic</strong></p>

End Triassic

Years: around 201 Mya

Extinction: 80%

What happened: Underwater volcanic activity cause the mass release of carbon dioxide + hydrogen sulfide into the atmosphere.
Causes global warming and ocean acidification

<p>Years: around 201 Mya</p><p>Extinction: 80%</p><p>What happened: <span>Underwater volcanic activity cause the mass release of carbon dioxide + hydrogen sulfide into the atmosphere.</span><br><span>Causes global warming and ocean acidification</span></p>
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<p><strong>End Cretaceous (K-T extinction)</strong></p>

End Cretaceous (K-T extinction)

Years: around 65.6 Mya

Extinction: 60%

What happened: Large asteroid (6-9 miles wide) hit Earth at speed of 12,000 km/hr. Debris from strike came down for thousands of miles, set forests on fire, and started a nuclear winter (sun blackened out). Events led to the collapse of the food web. Process
took ~32,000 years

<p>Years: around 65.6 Mya</p><p>Extinction: 60%</p><p>What happened: <span>Large asteroid (6-9 miles wide) hit Earth at speed of 12,000 km/hr. Debris from strike came down for thousands of miles, set forests on fire, and started a nuclear winter (sun blackened out). Events led to the collapse of the food web. Process</span><br><span>took ~32,000 years</span></p>
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Consequences of Mass Extinctions

-It can take from 5-10 million years for diversity to recover following a mass extinctions

-Alter ecological communities and the habitats available to organisms 

-Changes the types of organisms found in ecological communities

-Mass extinctions have drastically altered ecological communities 

-Many lineages are lost; elimination of many species

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What is adaptive radiation?

Periods of evolutionary change in which groups of
organisms form many new species whose adaptations
allow them to fill different habitats

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When does large scale adaptive radiations usually occur?

  • Occurred after each of the “big five” 

  • also occur after major evolutionary
    events (ex: photosynthesis)

  • colonization of new
    areas

Example: mammalian radiation following the Cretaceous extinction

<ul><li><p>Occurred after each of the “big five”&nbsp;</p></li><li><p><span>also occur after major evolutionary</span><br><span>events (ex: photosynthesis) </span></p></li><li><p><span>colonization of new</span><br><span>areas</span></p></li></ul><p>Example: mammalian radiation following the Cretaceous extinction </p>
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What is an ecological opportunity?

Availability in new resources

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Morphological Innovation

Evolution of a key trait that allowed descendants
to live in new areas, use new resources, or move in new way

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Plant Evolution

1.Bryophytes (610-500 Mya)

2.Seedless Vascular plants (425-360 Mya)

3.Angiosperms (245-202 Mya)