Lecture 3 - Speciation II, History of Life on Earth, Intro to Animal Diversity, Invertebrates I Flashcards
How old is earth?
4.5 billion years
How long has life existed on earth?
How long has human civilization been around?
~ 3.8 billion years
.0003% of history of life
How is the history of life conceptualized/organized?
Eras - Separated by catastrophic extinction boundaries
Periods - Subdivide eras
Differences in fossils in successive layers of rock
Pre-Cambrian
- Super eon
- origin of life
- first 4 billion years of earths existence
Precambrian to cambrian transition
- “explosion” of new life forms
- just over .5 billion years ago
Physical events that have contributed to nature and timing of evolutionary changes among organisms (5)
- Continental drift
- atmospheric oxygen concentrations
- climate
- volcanoes
- extraterrestrial events (ex. meteorites)
Continental Drift
- Earths crust consists of several plates 40km thick, floating on fluid layer of magma
- Heat creates convection currents which exert pressure on plates
- Move apart or together
- Formation, size and position of continents
- Oceanic circulation patterns, global climate, sea levels
Himalayan Mountains
Ex: of continental drift
- Tallest range in world
- Created by Indian and Eurasian continental plates colliding
- Collision caused plates to buckle and get pushed upwards
- Himalayas continue to rise more than one cm a year
Super-Continents
List them:
- Caused by continental drift
- Most recent super-continent was Pangaea
- Believe that in 250 million years all continents will reform as one again
- Ur
- Kenorland
- Columbia
- Rodinia
- Panhotia, Gondwana
- Pangaea
- Next super continent
Fossil Configuration and Continental drift
- Fossil patterns in different continents show how they were connected
Continental Shift and Species Survival
What doe is affect? (3)
- Shifting affects:
1. oceanic circulation patterns
2. global climates
3. sea levels - Major drops in sea levels have usually been accompanied by massive extinctions, especially of marine organisms
Atmospheric Oxygen Concentrations
timeline
- have changed over time
- 2 major increases in oxygen
- 1 major decrease
Timeline:
- ~2 billion years ago: 1st photosynthetic bacteria
- 750 mya - first increase
- ~400 mya - second increase
- 250 mya - decrease = great dying
First oxygen increase
What did it allow?
- certain bacteria evolve ability to use water in photosynthesis. Oxygen released as a waste
- Prokaryotes could evolve aerobic respiration
- Advantages - aerobic metabolism proceeds more rapidly and harvests more energy than anaerobic
- aerobes replaced most anaerobes
- made possible: larger cells and more complex multicellular organisms
Second Oxygen Increase
What did it allow?
- oxygen increased during carboniferous and permian periods
- evolution of large vascular plants in lowland swamps
- oxygen was 50% higher than today
- allowed evolution of giant flying insects that wouldn’t survive in today’s atmosphere
Drop in Oxygen
- drying of swamps cause rapid drop in oxygen concentrations
- “the great dying”
- mass extinction of 96% of earth’s species
diversification of flowering plants helped gradually rebuild oxygen concentrations
Climate Change
- Earth was often considerably warmer than today
- Sometimes colder with extensive claciation
- Range of average temps has spanned 10c or 18F
- cold periods separated by long periods of milder climates
- Short period of major climatic shifts: 5 - 10k years
- Rapid climate changes typically lead to extinctions
Volcanoes
- Many volcanic eruptions when the continents came together to form Pangaea in Permian period
- occurred as continents drifted apart during the late Triassic and end of Cretaceous periods
- Large volcanic eruptions inject ash ans sulfur dioxide into atmosphere –> leads to Sulphurous acid that blocks sunlight
- Causes drop in temperature glaciations
- potentially responsible for several mass-extinctions
- Likely contributed to drying of swamps and killing of plants that caused “great dying”
Extraterrestrial Events
- Collision with large meteorites cause of mass extinctions
Ex:
- End of mesozoic period - end of dinosaurs
- 180km crater located in mexico
- = 100 million megatons of high explosives
- plume of debrisheated atmosphere, ignited fires, blocked sunlight
- settling debris formed iridium rich layer
Date of Lower sea levels and glaciation mass ext.
444 million yrs ago
Date of “great dying”
251 million yrs ago
Date of Yucatan meteorite
65.5 million yrs ago
When was the first life?
When were the first eukaryotes?
Precambrian Era
- first evolved about 3.5 - 3.8 billion years ago
- mostly microscopic prokaryotes
- Eukaryotes evolved part way through
- 1.5-2.1 billion years ago
2 Major Events that set the stage for rapid diversification of Life that occurs upon entry into Cambrian period
- Evolution of Eukaryotes
2. Increasing oxygen levels