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Origin of Life.

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Presentation on theme: "Origin of Life."— Presentation transcript:

1 Origin of Life

2 Eons – largest time division
Eons determined by major changes in the Earth Most recent Eon started with the appearance of multicellular animals = Phanerozoic Eon Three Eons make up what was previously know as the Precambrian Period 1) Proterozoic 2) Archean 3) Hadean

3 I. WHEN Did Life Evolve? A) Earth molten for Hadean Eon (4.5 – 3.9 bya) B) cooled by 3.9 billion years ago C) Solid rock formation began Archean Eon 3.9 bya

4 II. First life likely formed in water
A) water vapor condenses and falls as rain B) Creates oceans C) salts added over billions of years as material eroded from continents D) water protects from U-V radiation

5 III. First cell = anaerobic conditions
A) Early Archean rock dark-colored = unoxidized B) Formed before free O2 available C) oxidized (rusted) sediment appears 2.2 billion years ago in Proterozoic Eon D) Free oxygen produced by living cells doing .… photosynthesis E) Therefore, life must have evolved before 2.2 bya

6 IV. How did the first cell form?
A) Spontaneous formation of monomers and macromolecules from chemicals in environment **** Only possible if no free O2 B) cell membranes form C) nucleic acids pass on Genetic infromation

7 V. Monomer Synthesis A. we created organic monomers from non-living chemicals B.Miller and Urey - created “Early Earth Apparatus” C. Archaean atmosphere D. electrodes produce “lightning” E. primordial pond in the bottom

8 F. Results: 12 of 20 most common amino acids synthesized + monomers
Showed monomers can form from non-living source next step: polymerization

9 VI. Requirements for polymerization
A. energy source: 1. lightning 2. geothermal vents B. concentration: to bring materials together 1. tide pools/evaporation 2. clay

10 clay a. Forms platelets b. platelets are: very small flat
with negative charge on surface

11 VII. Cell membrane formation
A) phospholipids amphipathic hydrophobic & hydrophilic B) form spheres in water C) hydrophobic ends protected on inside D) First cell membrane?

12 VIII. Protobionts/protocells
A) fatty acid spheres form naturally B) Macromolecules & enzymes inside C) reactions occur inside D) Grow E) divide F)selectively permiable G) digest starch H) store & release energy

13 Experiments by Sidney W. Fox and Sidney w
Experiments by Sidney W. Fox and Sidney w. Fox and Aleksandr Oparin have demonstrated that protobionts form spontaneously. They formed liposomes and microspheres, which have membrane structure similar to the phospholipid bilayer found in cells may be formed spontaneously, in conditions similar to the environment thought to exist on an early Earth. These experiments formed

14 I. Are Protobionts Alive?
1)No 2) they can’t replicate themselves (pass on their traits to offspring)

15 IX. Replication A) process by which organisms make genetic copies of themselves asexual reproduction 2) sexual reproduction

16 X. Origin of Heredity A) many different types of protobionts
B) those best able to accumulate organic molecules, grow, and divide become most common C) but “competition” is useless unless traits can be passed on/inherited D) need polymers that can replicate themselves: DNA and RNA

17 XI. Nucleic acid reproduction
A) RNA can assemble on its own (Zn catalyst) B) Can replicate (make more copies) C) Can pass on genetic info when cell divides D) RNA world Hypothesis

18 XII. Earliest Life Forms 3.5 bya
3.4 byo, South Africa A) prokaryotic bacteria B) anaerobic: live without O2 C) fermenters: use organic molecules for energy modern

19 XIII. The First Energy Crunch
A) organic molecules become scarce B) competitive advantage goes to – C) organisms that can make their own food Photosynthesis D) done by primitive cyanobacteria

20 Photosynthesis 1) light-absorbing pigments (like chlorophyll) already present 2) chlorophyll rings form spontaneously 3) mutation causes e- to jump out 4) leads to Anaerobic cyclic psyn Makes only a little ATP (no glucose)

21 Aerobic Non-cyclic Photosynthesis
some cyanobacteria evolved to use H2O as e- source O2 released as a by-product Advantage: glucose produced = storable energy Problem: O2 toxic to anaerobic cells 6CO H2O carbon dioxide water C6H12O O2 sugar oxygen energy from sunlight

22 Indirect (non-fossil) evidence
Build up of oxygen Indirect (non-fossil) evidence for the presence of cyanobacteria ~ 3.5 bya

23 BIFs (Banded Iron Formations)
Indirect evidence for the presence of cyanobacteria ~ 3.5 bya Precambrian, Australia

24 Banded Iron Formations Created
iron dissolves in anaerobic water when iron bonds to O2 it becomes solid Iron oxide deposited in red layers When dissolved iron used up : 1) cyanobacteria die 2) dark, un-oxidized layers build up

25 Why are BIFs Banded? When runoff added more Fe to the water the entire process stared over again.

26 What Likely Happened O2 made by cyanobacteria at ocean surface
O2 toxic to them but not if the O2 was removed by bonding with iron (Fe) Oceans contained dissolved iron

27 BIFs began forming 3.5 bya = 1st free O2
ended about 1.8 bya = constant free O2

28 Earliest (Undisputed) Fossils = Stromatolites
2.2 byo Michigan

29 Stromatolites dome-shaped, layered structures Up to 3.5 byo
consist of layers of bacteria upper layers aerobic, photosynthetic lower layers anaerobic produce abundant oxygen how do we know?

30 They are still alive today in special environments, notably Shark Bay, Australia
Tide In Tide Out

31 Formation of Stromatolites
Cyanobacteria form a mat on top of sediment A new layer of sediment is deposited on top 1 cm Bacteria grow up through new layer

32 Stromatolites provide evidence for the
occurrence of cyanobacteria in the fossil record. Modern Ancient

33 Aerobic Bacteria some bacteria evolved antioxidants
allowed them to survive rising O2 levels by 1.8 bya some evolved to use O2… = aerobic respiration Obligate anaerobe bacteria restricted to refuges or go extinct

34 The rise of cyanobacteria & build up of oxygen in atmosphere had three significant effects:
Aerobic photoautotrophs became producers that fuel the food chains of surface world The first mass extinction oxygen-rich atmosphere set stage for the multicellular life (aerobic respiration)

35 Eukaryotic Cells First well established fossils 1.7 bya
Mid-Proterozoic eon Early protists unicellular with nucleus 100x larger than bacteria

36

37 Origin of Nucleus & E. R. In-folding of cell membrane
Similar to bacterial psyn membrane Surrounded DNA Formed ER

38 Endomembrane system and nuclear envelope are continuous

39 ‘In eukaryotes the organelles of the endomembrane system include: the nuclear membrane, the endoplasmic reticulum, the Golgi apparatus, lysosomes, vesicles, endosomes and the cell membrane. The system is defined more accurately as the set of membranes that form a single functional and developmental unit, either being connected directly, or exchanging material through vesicle transport.’

40 Origin of Mitochondria & Chloroplasts
Endosymbiotic theory Eukaryotic cells take in bacteria as endosymbionts Aerobic Bacteria become mitochondria Cyanobacteria become chloroplasts

41 Evidence for Endosymbiotic T
1) Two membrane layers of A) Outer membrane like host cell B) Inner membrane like a bacteria

42

43 2) Mito. & chloro. have their own DNA
Circular Chromosome Different genes than nucleus

44 3) Mito. & Chloro have own ribosomes &
Make own proteins Ribosomes like bacteria

45 4) Mito & Chloro grow and reproduce on own


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