Origin of Life: Prokaryotes and Eukaryotes Flashcards
(57 cards)
What requirements does somthing need to be alive?
Name all 6
- Organization
- Metabolism
- Response to stimuli
- Homeostasis
- Adaptions
- Reproduction
What are the three major eons in the geological record?
Archaean
Proterozoic
Phanerozoic (We are here)
- Plaeozoic
- Mesozoic
- Cenozoic
What are some uses for fossils?
- Calibrate phylogenies.
- Record extinct species that show how new groups of organisms can arise via the gradual modification of preexisting organisms (transitional fossils), e.g. the descent of birds from dinosaurs.
- Link evolutionary events (e.g. mass extinctions) with geological and environmental changes on Earth.
What are some factors that cause bias and incompleteness in the fossil record?
- Fossilization requires burial in sediment, but sediments accumulate episodically and discontinuously, and fossils typically preserve only the hard parts of organisms
- Most organisms were never fossilized, and even those that were fossilized are rarely discovered by humans
What factors increase the chances of an organism becoming fossilized
- Existed for a long time.
- Was abundant and widespread.
- Hard rather than soft-bodied.
- Aquatic rather than terrestrial.
- Inshore marine rather than offshore marine.
- Decomposing organisms were absent.
Mold fossils
Mold fossils form when a hollow space (impression) remains after the organism decays or dissolves.
- A cast fossil forms when minerals fill the hollow space (mold), creating a solid replica.
Replacement (Petrified) Fossils
In replacement (petrified) fossils the original tissues of the organism are replaced by minerals, preserving the detailed structure of the organism
Trace Fossils
Trace fossils provide evidence of an organism’s behaviour, such as tracks, burrows, or feces
Preserved Fossils
Preserved fossils retain much of the original organic material of the organism (carbon films, amber, tar or peat, and frozen).
Relative Dating
Fossils
Sedimentary strata reveal the relative ages of fossils.
- stratum = layer
Relative dating does not indicate how long ago a fossil was created.
- Does not provide the absolute age of a fossil, but can tell which fossil came 1st, 2nd, etc.
Challenges
- Common to have gaps in a sedimentary sequence.
- Inconsistent sediment deposition; erosion of uplifted strata.
- Sediments can be tipped or even inverted by major land movements.
- Overcome by use of widespread, common index (= indicator) fossils.
- Index fossils help to “read” incomplete or scrambled layers
Absolute Dating (Radiometric Dating)
Radioactive decay of isotopes of various elements provides a means of determining the age of fossils or rocks.
− Radioactive isotopes decay from one form to another at a known constant rate.
Example: carbon-12 (^12C) and
carbon-14 (^14C).
True or False
The fossil record shows that most species that have ever lived are now extinct.
True
> 99% of all species that ever lived are now extinct.
- The causes of extinction are varied, but it generally occurs when a species cannot adapt to changes in the species’ environment.
At times, the rate of extinction increased dramatically and caused mass extinctions.
- Mass extinctions are the result of disruptive global environmental changes.
- The history of life is characterized by five mass extinctions that changed the evolution of Earth’s biota during the Phanerozoic
How many mass extinction events have happend?
5
In each of the five mass extinctions, more than 50% of Earth’s species became extinct.
- Two of the notable mass extinctions are the Permian extinction and the Cretaceous extinction.
Permian Mass Extinction
The Permian mass extinction defines the boundary between the Paleozoic and Mesozoic eras 252 million years ago
- The Permian mass extinction was rapid, occurring over <5 million years, and it is Earth’s most severe extinction event.
- The “Great Dying” is Earth’s most severe known extinction event.
- Extinction of ~60% of all biological families, 81% of all marine species, especially marine invertebrates, and 70% of terrestrial vertebrate species.
What caused the Permian mass extinction?
The causes of the Permian mass extinction are uncertain.
- Much of the fossil evidence from this period was lost to the recycling of continental crusts via plate tectonics.
The best-supported hypothesis for the cause of the Permian mass extinction was catastrophic environmental change caused by volcanic activity.
- Extensive volcanism in what is now Siberia released large amounts of toxic and greenhouse gases (CO2, SO2, H2S) that triggered global warming and ocean acidification.
Other theories include:
- Gradual environmental changes (at sea)
- The formation of Pangaea (reduced shorelines and temperature gradient)
Cretaceous Mass Extinction
The Cretaceous mass extinction 66 million years ago separates the Mesozoic from the Cenozoic
- THIS IS THE DINOSAUR ONE
Only ~20% of all families went extinct but included:
- ~50% of marine species, e.g. ammonites (cephalopod molluscs).
- Many terrestrial plants and animals.
- Non-avian dinosaurs!
The Cretaceous mass extinction coincides with worldwide geologic deposits from a meteorite impact at Chicxulub, Mexico
- Dust clouds caused by the impact blocked sunlight, disturbing the global climate.
− Strongly supports an impact hypothesis for the cause of the Cretaceous mass extinction.
Adaptive Radiation
The rapid evolution of diversely adapted species from an ancestral species
- Adaptive radiation occurs when a change in the environment makes new ecological niches available
What things might lead to adaptive radiation
Mass Extinctions
- By eliminating so many species, mass extinctions can prepare for adaptive radiation.
- e.g. expansion of large marine predators following the Permian mass extinction
Evolution of novel Characteristics
- The adaptive radiation of photosynthetic prokaryotes, plants, insects, and tetrapods was enabled by novel adaptations.
- e.g. adaptive radiation of birds following the evolution of powered flight
Colonization of new regions
- Adaptive radiation can occur when organisms colonize new environments with little competition.
- e.g. vertebrates (tetrapods) move to terrestrial environments.
How long ago did Earth form
Earth formed approximately 4.6 billion years ago (bya) during the Hadean Eon.
− The surface of Earth during this period was extremely hostile to life until about 3.8 bya.
− There is very limited geological evidence before 3.8 billion years ago, making it difficult to study conditions from that time.
How did life begin?
Chemical and physical processes on early Earth may have led to the formation of simple cells through a hypothesized multi-step process:
1. Abiotic synthesis of small organic molecules.
2. Polymerization of small organic molecules into organic polymers.
3. Formation of protocells.
4. Emergence of self-replicating molecules.
Abiotic synthesis of small organic molecules
The origin of life
The formation of basic organic compounds, such as amino acids, nucleotides, and sugars, from inorganic precursors through abiotic (non-biological) processes.
- The current scientific consensus is that Earth’s primitive atmosphere was weakly reducing or neutral.
- Less CH4 and NH3 than first predicted
- Instead of forming in the atmosphere, abiotic synthesis may have occurred near volcanoes or deep-sea hydrothermal vents where strongly reducing conditions are found.
Two possible sources of organic
molecules on early Earth:
Terrestrial origins: spontaneous organic molecule synthesis driven by energy sources.
- High levels of volcanic activity, lightning, and UV radiation provided the energy needed for chemical reactions.
Extraterrestrial origins: formation of organic molecules in extraterrestrial objects that bombarded early Earth.
- Amino acids and other organic molecules have been detected in comets and meteorites.
Polymerization of small organic molecules into organic polymers
The origin of life
Small organic molecules can undergo polymerization reactions, where they join together to form larger organic molecules or polymers
- This process likely occurred on hot surfaces such as clay, sand, or rock, where evaporation of water concentrated small organic molecules, triggering the spontaneous formation of organic polymers.
Formation of protocells
The origin of life
Free-floating amino acids, proteins, and nucleic acids would not have been able to behave like cells.
- Replication and metabolism are key properties of life and may have appeared together.
- Metabolism needs separation from the environment.
In water, lipids and other organic molecules can spontaneously form hollow vesicles with a lipid bilayer.
- Protocells are simple, cell-like structures that form when organic molecules become enclosed within membrane vesicles.
- Early protocells, fluid-filled vesicles with semi-permeable membranes, allowing selective passage of molecules, are hypothetical precursors to modern cells
Experiments show that lipid vesicles form faster in the presence of volcanic clay.
Lipid vesicles exhibit simple reproduction and metabolism and can maintain an internal chemical environment.
- Vesicles can increase in size and divide independently, i.e. ‘reproduce’.
- RNA and other particles attached to clay are incorporated into protocells.
Emergence of self-replicating molecules
The origin of life
The formation of self-replicating molecules, which could store and transmit information, much like modern DNA or RNA, is a defining feature of life.
- The “RNA world hypothesis” suggests that RNA (ribonucleic acid), not DNA, was the first self-replicating molecule.
- RNA is simpler than DNA and can perform multiple functions:
- Self-replication: RNA can replicate itself, which is essential for passing on genetic information.
- Catalysis: Some RNAs, known as ribozymes, can act like enzymes, speeding up chemical reactions.
Natural selection produced self-replicating RNA molecules.
- RNA molecules that were better at self-replication and catalyzing useful reactions would have been naturally selected. This led to increasingly efficient and complex systems.
- Vesicles containing RNA capable of replication would have been protocells.
- RNA could have provided a template for the later evolution of DNA, a more stable genetic material.