Early Earth and Green-worldEarth has been call the Blue Planet, but it would be just as accurate to call it the Green Planet... • Early Earth and chemical evolution pp: 15-36 • Evident
Trang 1Early Earth and Green-world
Earth has been call the Blue Planet, but it would
be just as accurate to call it the Green Planet
Trang 2• Early Earth and chemical evolution (pp: 15-36)
• Evident of life style: stromatolites
• Oxygen and Ozone formation
• Evolution of land plant (pp: 546-551)
• Quiz
Trang 3Early Earth and Original of Life
• chemical evolution :
+ pattern component: Early in Earth history, simple chemical compounds combine to form more complex carbon – containing substance that accumulated in the Ocean.
carbon – containing substance that accumulated in the Ocean.
+ process component: Complex carbon containing
compounds formed because energy in sunlight and extremely hot water was converted to chemical
energy in the form of new chemical bonds.
Trang 4Original atmosphere on the Earth
The planet: bombarded
Atmosphere: hydrogen, carbon dioxide…but no free oxygen
Trang 5Water and the fitness of environment
• The polarity of water molecular results in hydrogen bonding.
• Water is the solvent of life.
• Organisms depend on the cohesion of water molecules
• Water moderate temperature on the Earth.
• Oceans and lakes don’t
freeze because ice floats
Trang 6Chemical evolution hypothesis
Trang 7Carbon & molecular diversity of life
• Almost molecules found in organisms contain this atom.
• Variation in carbon skeletons contributes to the diversity of
organic molecules.
• Functional groups contribute to molecular diversity of life.
Trang 8The important of oxygen
• Need for respiration of living organism
• Made ozone layer.
• Filter UV
Trang 9Evidences of life: stromatolites
Stromatolites at 3.5 billion
years old
Stromatolite: precipitate sediment (stone, rock) with microorganism
Trang 10alternating layers of CaCo3 and gelatinous material
Str in 2.4 billion year old rock Str In modern life
Trang 11Organic or inorganic compounds in deposit
• Morphology of known microoganism that still exist today.
• Compeare structure of ancient and new stromatolites.
• Ratio C 13 and C 12 inside stromatolites
Trang 12C13 in inorganic limestone and organic life stone
Trang 13• 3 5 Bya ago,
photosynthetic organisms release O2 to
atmosphere.
• 2.5 Bya ago, enough O2
accumulated
• O2 formed O3 layer
Trang 14Early life evolved without protective
atmospheric ozone layer
• Prokaryote: 3.5 – 2.2 Bya.
• Eukaryotic life: 2.1 Bya.
• Multicellular Eukaryotic: 1.2 Bya.
• Plants, fungi, animal: 500 Mya.
Trang 15Green plant
thylakoids
arrangement
photosynthetic pigments
arrangement
similar cell
wall, sperm,
peroxisome
chloroplast
synthesize
starch
Trang 16Evolution of land plant
First
evidence
of land
plant:
Cuticle,
spore,
sporangia
Morphological innovation:
stomata, vascular tissue, leave
Extensive coal – forming swaps
Both wet and dry
environments blanketed with green plants for the first time
Diversification
of flowering plants
Trang 17Morphological diversity in land plant
Non-vascular plants
Seedless-vascular plants
Seed plants
Lack vascular tissue
to conduct water
and support (moss)
Have vascular tissue but do not make seed (fern)
Have vascular tissue and make seed
(flowering plant)