Early Earth & the Origin of Life (Ch. 26)
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Transcript of Early Earth & the Origin of Life (Ch. 26)
Early Earth & the Origin of Life (Ch. 26)
*The history of living organisms and the history of Earth are inextricably linked:
Formation and subsequent breakup
of Pangaea affected biotic diversity
The first photosynthetic organism released oxygen into the air and altered Earth’s atmosphere
Homo sapiens have changed the land, water, and air on a scale and at a rate unprecedented for a single species
Figure 2. Sea level is changing. Observing stations from around the world report year-to-year changes in sea level. The reports are combined to produce a global average time series. The year 1976 is arbitrarily chosen as zero for display purpose.
Figure 1. Global warming revealed. Air temperature measured at weather stations on continents and sea temperature measured along ship tracks on the oceans are combined to produce a global mean temperature each year. This 150-year time series constitutes the direct, instrumental record of global warming.
History of Life on Earth: Life on Earth originated between 3.5 and 4.0
billion years ago
Because of the relatively simple structure of prokaryotes, it is assumed that the earliest organism were prokaryotes
*this is supported by fossil evidence (spherical & filamentous prokaryotes recovered from 3.5 billion year old stromatolites in Australia and Africa)
Major Episodes in the History of Life:
first prokaryotes- 3.5 to 4.0 billion
years ago
photosynthetic bacteria- 2.5 billion
years ago
first eukaryotes- 2 billion years ago
~The oldest unequivocal remains of a diversity of microorganisms occur in the 2.0 BYO Gunflint Chert of the Canadian Shield
~This fauna includes not only bacteria and cyanobacteria but also ammonia consuming Kakabekia and some things that ressemble green algae and
fungus-like organisms
plants evolved from green algae
fungi and animals arose from different groups of heterotrophic unicellular organisms
first animals (soft-bodied invertebrates)- 700 million years ago
first terrestrial colonization by plants and
fungi- 475 million years ago
plants transformed the landscape and created new opportunities for all
forms of life
Prebiotic Chemical Evolution: Earth’s ancient environment was
different from today:-very little atmospheric oxygen
-lightning, volcanic activity, meteorite, bombardment, UV radiation all more intense
Chemical evolution may have occurred in four stages:
1) abiotic synthesis of monomers
2) joining of monomers into polymers (e.g. proteins, nucleic acid)
3) formation of protobionts (droplets
formed from clusters of molecules)
4) origin of heredity (likely that RNA was first)
Oparin / Haldane hypothesis (1920s): the reducing atmosphere and greater UV radiation on primitive Earth favored reactions that built complex organic molecules from simple monomers as building blocks
Miller / Urey experiment:
Simulated conditions on early Earth by
constructing an apparatus containing H2O, H2,
CH4, and NH3.
Results:• They produced amino acids and other organic
molecules.• Additional follow-up experiments have produced all
20 amino acids, ATP, some sugars, lipids and purine and pyrimidine bases of RNA and DNA.
Protobionts: collections of abiotically produced molecules able to maintain an internal environment different from their surroundings and exhibiting some life properties such as metabolism and excitability
(experimental evidence suggests spontaneous formation of protobionts)
possible formation
of protobionts;self-repliating RNA as early
“genes”
Origin of Life - Different Hypotheses:
*No one knows how life actually began on Earth; experiments indicate key steps that could have occurred.
Panspermia: some organic compounds may have reached Earth by way of meteorites and comets
meteorite
Sea floor / Deep-sea vents: hot water and minerals emitted from deep sea vents may have provided energy and chemicals needed for early protobionts
Simpler hereditary systems (self-replicating molecules) may have preceded nucleic acid genes.
The Major Lineages of Life: the 5 Kingdom System
Living organisms Prokaryotic Eukaryotic
Simple/unicells Multicellular
Autotrophic Heterotrophic
Absorptive Ingestivenutrition nutrition(Animalia) (Fungi)
(Plantae)
(Protista)
(Monera)
How was the atmosphere of the early earth different than it is today?
A. The early earth’s atmosphere contained mostly carbon monoxide
B. The early earth’s atmosphere had more oxygen than it has today
C. The early earth’s atmosphere contained more single celled organisms than it does today
D. The early earth’s atmosphere did not contain oxygen
In the 4-stage hypothesis for the chemical evolution of life,
which of the following is the correct sequence? A. Synthesize monomers; join monomers; form protobionts; system of
heredity
B. Form protobionts; synthesize monomers; join monomers; system of heredity
C. System of heredity; join monomers; synthesize monomers; form protobionts
D. Synthesize monomers; join monomers; system of heredity; form protobionts
What is a protobiont?A. A self-replicating early life form that uses RNA for heredity
B. A group of monomers that join/bond when temporarily bonded to materials such as clay or volcanic rock
C. Early enzymes that were able to join basic amino acids together
D. Collection of abiotically produced molecules that can maintain an internal environment and exhibit some life properties
What is the name of the alternate hypothesis for the “seeding” of organic compounds on earth by meteorites & comets?
A. Deep Sea Vent Hypothesis
B. Panspermia
C. Impact Hypothesis
D. Early Earth “Seeding” Hypothesis
In the 5 Kingdom system used to classify all life, what are the names of the Kingdoms?
A. Bacteria; Plantae; Animalia; Fungi; Protista
B. Bacteria; Plantae; Animalia; Fungi; Monera
C. Plantae; Animalia; Bacteria; Monera; Protista
D. Plantae; Animalia; Fungi; Monera; Protista