exam 3 ch 18.1 Flashcards
the longest eon transition to an oxygenated atmosphere and multicellular eukaryotes evolve
proterozoic eon
Atmospheric free oxygen (as a byproduct of photosynthetic
cyanobacteria) levels increased permanently
2.4-2.0 GA the great oxygenation event
Oxygen combined with dissolved iron in oceans to form iron oxides, that
precipitated out, forming alternating layers of iron oxides and chert.
banded iron formations (BIF’s )
First fossil evidence that fungi may have diverged from other life.
-Evidence from basalt from South Africa contains filamentous fossils, that form mycelium-like structures
2.4 Ga Paleoproterozoic Fungi:
-Free oxygen (as a byproduct of photosynthesis) reacted with the methane in the atmosphere
(converting it to CO2) causing a global glaciation
2.3–2.2 Ga Proterozoic snowball Earth event:
-The first known major extinction wiped out 99% of life on Earth
2.4–2.0 Ga The Oxygen Catastrophe:
Enzyme that reduces molecular oxygen into water
Cytochrome oxidase:
8,000 mi from north to south landmass consisting of
major parts of all current continents resulting in major mountain building events
2.1 to 1.8 Ga Columbia (Nuna) Supercontinent:
First possible fossil evidence of multicellular eukaryotic
life
2.1 Ga Multicellular eukaryotes:
First definitive fossil thylakoids
1.75Ga
Membrane-bound compartments found in chloroplasts and cyanobacteria that are responsible for the light-
dependent reactions of photosynthesis
Thylakoids:
Definitive multicellular eukaryote fossils.
1.63 Ga:
The stromatolites reach their peak ~1.2 Ga, evidence for eukaryotes with plastids
1.6-1.0 Ga Mesoproterozoic:
Organelles found in plant and algae cells that are responsible for photosynthesis.
Plastids:
Cyanobacteria evolved into
Plastids.