Extinctions 1 Flashcards
What is extinction?
An expected process that is natural and shows change through time.
Extinction rate should match rate of new biodiversity. Balance of biodiversity.
What causes change from Paleozoic to Mezosoic?
Incoming of distinct new species usually defines a new period, but the change between Permian to Jurrasic is so huge they made a whole new era (mesozoic)
They (without realizing it) were identifying mass extinction and evolution.
What effect would plate tectonics have on biodiversity over time?
Biodiversity is number of species NOT individuals on the planet.
Plate tectonics: the more fragmented, the higher the biodiversity on the planet! Due to climatic variation, variable food supply, barriers to migration and changes in oceanic circulation.
How would global biodiversity change through time
- Supercontienent Rodina (750Ma) fragments. First high diveristy biota after the snowball.
- Fragmentation continues through lower paleozoic and biodiversity increases.
- Upper paleozoic fragmentation goes in reverse. ie. formation of old red sandstone in late devonian (diversity drops with series of extinction pulses)
- Formation of Pangea (end of permian) massive drop in global biodiversity
- Fragmentation of pangea during mesozoic and diversity increases again (with a few hiccups)
- Today continents are rich and randomly dispersed.
What are sudden changes referred to as?
Mass extinction events.
Other extinction events/changes are ‘first order’ which dont account for the large rapid drops.
What classifies a mass extinction event?
30% of all species extinct. Broad range of ecologies
Short sudden. Gradualists say 0.5-1million years, catastrophists say between 1-100 years.
Can be classified by severity
Major (50% families, 96% species)
Intermeidate (30 families, 50 spcies)
Minor (10 families, 30 species)
What are the last five major mass extinctions recognized in the last 500MA
Late ordovician Late Devonian Late Permian Lake Triassic Cretaceous/Paleogene
possibly entering the 6th
What are the causes of mass extinctions?
- biologial/competition/predation/pathogens being introduced. creatures occupying the same niche. i.e. newzealand ground dwelling bird fauna.
- Earth based, related to place movement (climate/ocean cirucation and volcanic activity)
- Comets and extra-terrestrial impacts
- Combo of many factors is most reliable cause.
What are the fragments of odovician continents?
Gondwanaland (africa and south america)
Laurentia (north america)
Avalonia (southern britain, atlantic canada, coastal USA)
Baltica (NW eurasia)
Gondwanaland is moving towards south pole and ice begins to grow on it where north african sahara desert is.
What was the ordovician like?
Tropical paradise with high biodiversity. Greenhouse planet.
Ancient ecosystmes were not primitive.
extinction starts in last stage of ordovician, the Hirnantian. where 85% of all species perished. starts 445ma
What are oxygen isotopes and how are they used?
O16-18. Used to read glacial periods.
o16 is the lightest, it is what is evaporated from oceans to create rain. When it is cold, instead of going back to oceans the rain stays on land in the form of ice. This increases relative 018 in the oceans! Recorded in brachiopods (shell structures)
oxygen is not radioactive, just a stable isotope that can be counted relatively.
have you looked at examinable required reading on website???
What is the 1st pulse of the ordovician extinction? hirnantian glaciation
445 Ma, tropical fauna’s hit hard first, 50/70 tabulate nd rugose corals are extinct. Golder water creatures migrate northwards and tropical creatures had nowhere to go! Glaciation caused a rapid drop in sea level too (seen as erosion surface in ordivician sediements)
Deep canyons in river systems. water on land tries to come to equilibrium with level of the sea!
Water is withdrawn from the shelf, so its colder and loss of habitat.
What is the 2nd pulse of ordovician extinction?
hirnantian glaciation
End of glacial period. Sea levels and temperatures RISE.
Not as severe as the 1st, but those who had adapted to the cold now die off.
Why didn’t Gondwanaland get ice earlier if it sat on the south pole for longer?
Closure of Iapetus Ocean - The Caledonides Mountain building Period.
- Development of Appalachian and Caledonian mountain belts when Avalonia and Baltica collide (later collide with Launentia).
The ocean was removed by subduction, same process for andes mountains (edge of continental margin)
Ocean closes through silurian and finally closes in Devonian forming Laurussia (euramerica) . Ocean suture line runs through northern england and ireland.
The EROSION OF THE RISING MOUNTAIN CHAIN would drawdown co2 to cause silicate weathering, and a possible drop in volcanic activity.
net drawdown of co2 cause rapid glaciation
What is the Niarbyl Fault Ilse of Man?
Suture line between laurenia and avalonia. Visible representation of closing iapetus ocean. Has been heavily eroded.
Same thing happened in north america explaining paleozoic fossils.