CH 225 Flashcards
(24 cards)
fossil record displays. . .
Macroevolution: evolution above the level of species
Fossil limits
-relative age only
-not all things fossilize
-rare brief spp.
How old is Earth?
~4.6 bya
Steps of Origin of Life
small organic molecules -> macromolecules-> “protocells” -> origin of RNA
Small organic molecules formed by. . .
-atmosphere (h2o vapor and chemicals, no 02)
-near submerged volcanoes and deep sea vents
-meteorites (carbonaceous chondrites)
Abiotic synthesis of macromolecules
small organic molecules polymerized when concentrated in bubbles on ocean’s surface
Protocells
-semi membrane bound vesicles of abiotically produced molecules
-simple reproduction and metabolism
-maintain internal chemical envt
RNA and early natural selection
-1st gen material was probably RNA as ribozymes (catalyze reactions, self splicing, and replication of self and others)
-early protocells w/RNA (better competitors)
Geo record order
-archaean eon
-proterozoic eon
- phanerozoic eon
Phanerozoic eras
-Paleozoic
-Mesozoic
-Cenozoic
Oldest fossil
Stromatolites (rock-like layer of bacteria and sediment)
Where did photosynthesis likely evolve?
Cyanobacteria
Effects of oxygen accumulation in atmosphere
-challenge for some life
-opportunity to use light energy
-new niches to occupy
How did first eukaryotes come to be?
Evolved via internal membrane folding and serial endosymbiosis (mitochondria, chloroplasts)
“Snowball earth” hypothesis
There was extreme glaciation in the time of early eukaryotes and life could only be found at hydrothermal vents
Edicarion biota
Diverse soft bodied organisms
Colonization of land order (500 million years ago)
-plants and fungi
-inverts
-verts
-mammals evolved
Main causes of rise and fall of organisms
-plate tectonics and continental drift
-mass extinction
-adaptive radiation
How many supercontinents have there been?
3
How many major extinctions have there been?
5
Permian extinction (251 mya)
-between Paleozoic and Mesozoic eras
-extinction of ~96% of marine spp.
-volcano driven global warming and drop in ocean O2
Cretaceous Extinction(65.5 mya)
-separates Mesozoic from Cenozoic
-extinctions of half of marine spp. and many terrestrial plants and animals, including most dinosaurs
Current rate of extinction
100 to 1000x typical rate
-35-150 a day
Adaptive radiations
Evolution of diverse spp. from common ancestor as move into newly vacated niches