Lecture 22: History of Life on Earth (and Mass Extinctions)
Reading – P. 426-431, 433-444 Quiz 8 review Midterm 2 review Extra Credit Opportunities!
• 0.5% added to your overall class score if you complete the final evaluation. This is part of a trial for a new student evaluation form for UCI. Complete by 5p.m. on Fri Dec 7th.
• 0.5% added to your overall class score if you complete a survey about new ALP classrooms. I’ll send an e-mail about this later this week, including a link to the Information Sheet about the education study. Learning Outcomes
• Be aware of the theories of where life might have begun
• Be able to explain how the biosphere affected and in turn was affected by atmospheric oxygen levels
• Be aware of some of the major events in evolution of life and a rough idea of when these events occurred in relation to each other and the age of the Earth (I won’t ask about specific dates)
• Be able to describe/explain some causes of mass extinctions
• Be able to explain the causes of current loss of biodiversity and characteristics of endangered species
• Be able to give examples of how the Earth system influences the biosphere and how the biosphere influences the Earth Hadean Eon (4.54 – 3.85 Gyrs) Archean Eon (3.85 – 2.5 Gyrs) Origin of life on Earth: What we know
• Life maybe developed on Earth ~3.9 billion years ago • Earliest organism probably even simpler than bacteria • Unknown where/how life formed
1. ‘Primordial soup’ 2. Deep-sea hydrothermal vents
3. Organic molecules http://www.youtube.com/watch?v=D69hGvCsWgA from space (unlikely) History of life on Earth: Archean
3.5 – 1.5 billion years ago • Simple life forms (prokaryotes = no nucleus) were only life forms on Earth for ~ 2 billion years
• O2 levels very low so organisms limited to fermentation rather than respiration to release energy - less efficient so cells were small and simple History of life on Earth: Proterozoic
1.5 – 0.6 billion years ago
• Once O2 started building up then energy restrictions could be overcome and more complex, larger eukaryotes could develop
~ 600 million years ago (shortly after Snowball Earth events) • Earliest evidence of multicellular animals resembling jellyfish, soft corals and flatworms History of life on Earth: Phanerozoic
~570 million years ago • Cambrian explosion • Major increase in diversity • First internal and external skeletons • Why did this ‘explosion’ occur? – Sexual reproduction?
– Continued build-up of O2 allowed formation of carbonate skeletons? History of life on Earth: Phanerozoic
~500 million years ago • Life started to develop on land • For life to exist on land need: – Structural support – Ability to transfer water within the organism and keep from dehydrating – Ability to exchange gases with air instead of water – Moist environment for reproductive system Life on land: Plants
• Evolved from green algae • Earliest plants were seedless, reproduced using spores e.g. mosses, ferns • Conifers evolved – had seeds which allowed plants to spread to more diverse habitats • Flowering plants evolved – developed flowers to attract pollinators, increasing their reproductive success Life on land: Animals • First animals to move from ocean to land probably were insects e.g. millipedes. Still most numerous and diverse animal group.
• First animals with backbones were fish. Later moved onto the land where their fins could act as limbs.
• Evolved into amphibians – limited to moist environments
• Amphibians → reptiles → mammals and birds
Mudskipper – amphibious fish iClicker Question: Putting it all together Can you put the images below in order from oldest to most recent? C
A
A) B-A-C B) C-B-A C) A-C-B D) C-A-B
BB Life on Earth: Mass Extinctions • Change in the number of species = origination rate - extinction rate • If enough species become extinct over a period of time we call this a mass extinction
The ‘Big 5’ mass extinctions Mass Extinctions: Possible Causes
What do you think could cause a mass extinction event?
(Can you think of at least 3?) Mass Extinctions: Possible Causes 1. Impact event 2. Extensive volcanism
3. Rapid and significant climate change Mass Extinctions: Impact events
• Tunguska, Siberia • 1908 • Approx 60m meteor/comet fragment exploded 5-10km above surface • Equivalent to 5-30 Megatons (1000 x Hiroshima bomb) • Flattened 770 square miles of forest (80 million) trees) http://www.youtube.com/watch?v=dpmXyJrs7iU Mass Extinctions: Volcanism
Red = areas of igneous rocks Yellow dots = corresponding hotspots Cretaceous-Tertiary Mass Extinction When: 65 million years ago What: 80-90% of total species (land and ocean) anything over 25kg didn’t survive omnivores, insectivores, carrion-eaters survived Duration: extremely rapid (tens thousands of years or less) What might have caused the mass extinction at 65 Myrs that killed the dinosaurs? a) Impact event b) Extensive volcanism c) Rapid climate change d) Some combination of the above Dekkan Traps, India 500,000 km2 of basalt up to 2km thick Permian-Triassic Mass Extinction
When: 252 million years ago What: 70% land species 96% marine species 95% of all life on Earth at that time Duration: Uncertain still but potentially several short events (10- 100kyrs) over time, took 10 million years for life to recover after Siberian Traps, Russia 4-7 million km2 of basalt up to 4km thick in places
Lava erupted through coal beds releasing extra CO2 Global temperature rose by over 6 oC Oceans stopped circulating (no oxygen) A 6th Mass Extinction Today? • Humans activities are resulting in loss of biodiversity mostly due to: – Hunting/over-harvesting – Deforestation and desertification (habitat loss) – Pollution – Introduced/invasive species – Continued climate change in future decades • Background extinction rate before humans = ~ 15 per year • Today, in tropical forest, extinction rate = ~ 27,000 per year iClicker Question
Which species do you think is least likely to go extinct?
A C
B D A 6th Mass Extinction Today? • Humans activities are resulting in loss of biodiversity mostly due to: – Hunting/over-harvesting – Deforestation and desertification (habitat loss) – Pollution – Introduced/invasive species – Continued climate change in future decades • Species most vulnerable to extinction are – long-lived, large, low reproduction rates (so slow recovery), require large territories and high food supplies, highly specialized Future of life?
What will life look like millions of years from now? Must consider:
• Environment – controlled by plate tectonics, atmosphere composition, climate i.e. likely niches and habitats • What things will be left after the current extinction event to continue to evolve? What ecological niches will be empty? • How quickly the process of evolution will change a species?
https://www.youtube.com/watch?v=w0kzMmcTS8I& list=PL019H6clyzKb-fTn4WM5ypMym0rbNKHcr On Wednesday – Biogeochemical Cycles
Reading = P. 456-461, 464-468, 473