Origin of Life Flashcards
When was earth created
4.6 billion years ago
When did life being
3.5 billion years ago
Pre-Cambrian period
-makes up 90% of Geological Time Scale
- made up of Hadean, Archeon, and Proterozoic eons
Order Eons chronologically
Hadeon (4.6-4bya) - Archeon (4-2.5 bya) - Proterozoic (2.5-541 mya)
Hadean Eon
-time before a reliable (fossil) record of life
- temps are extremely hot
- no oxygen
- ejected debris following giant impact collision between early earth and an ancient planet called theia is thought to have formed the moon
Archeon Eon
- volcanic activity was considerably higher than today, with numerous lava eruptions
- without oxygen
- beginning of life on earth and evidence of cyanobacteria
- life was limited to simple-celled organisms lacking nuclei (prokaryotes)
- earths crust had cooled to allow formation of continents
- earliest identifiable fossils (stromatolites)
Proterozoic Eon
- appearance of oxygen to just before the proliferation of complex life (such as corals)
- bacteria began producing oxygen, leading to the sudden rise of life forms
- eukaryotes cells emerge, including some forms of soft-bodied multicellular organisms
Describe how stromatolites formed
- form in shallow water
- column shaped structures made up of layers of sedimentary rock, created by mats of cyanobacteria living on top of stromatolite
- cyanobacteria continue to reproduce on upper surface of mats as these cells depend on light for photosynthesis
- sediments begin to settle and accumulate on top of cyanobacteria, block sunlight, cyanobacteria slowly move to top of this sediment layer, trapped sediment within stromatolite will harden into rock
- tiny living things, like bacteria and algae, grew together in layers on the bottom of shallow water
Describe how banded iron formations are created
- consists of layers of iron oxides (either magnetite or hematite) separated by layers of chert, jasper or quartz
- each layer is usually narrow
- rock has a distinctively banded appearance because of differently colored lighter (chert, jasper, quartz) and darker iron-rich layers
- iron and oxygen in seawater combine to form iron oxide, which settles to the ocean floor as layers of sediment.
Describe how red beds are formed
- huge deposits of iron-rich sediment
- once in air, 02 could react with iron in sediments on the earths surface, which produced rust-colored sedimentary rock known as red beds
- first appeared in geologic records 2 bya
Explain how stromatolites, banded iron formations, and red beds are geological evidence of free oxygen on early earth during Pre-Cambrian period
-stromatolites needed oxygen to survive, their presence suggests oxygen was available in the environment
-iron formations created when iron in seawater combined with oxygen
-red beds are rock with a reddish color due to the presence of iron oxide, which forms when iron reacts with oxygen
Explain how stromatolites led to the existence of banded iron formations and red beds
-stromatolites were formed by tiny living organisms, like bacteria and algae, which released oxygen during their life processes
-oxygen combined with iron in the seawater, forming banded iron formations as layers of iron-rich rocks settled on the ocean floor
-oxygen continued to build up in the atmosphere, it reacted with iron in the land, leading to the formation of red beds with iron oxide-rich rocks.
Phanerozoic Eon
- represents the period of earths history with advanced life forms
- Paleozoic, Mesozoic, and Cenozoic eras
Paleozoic Era
-542 to 251 million years ago
- longest period of Phanerozoic Eon
- composition of air was very similar to current atmosphere (80% nitrogen and 20% oxygen)
- formation of Pangaea
- Cambrian explosion
Cambrian Explosion
535 to 525 million years ago
- most intense burst of evolution ever know
-earliest fossil appearance of many major groups of living animals