Ch25 Flashcards
Protocells
-may have been fluid-filled vesicles w/ membrane-like structures
-may have been vesicles w/ RNA capable of replication
Abiotic synthesis
creation of organic molecules from non-life
Chemical/physical processes on early earth may have produced simple cells in these stages:
-abiotic synthesis
-joining of these small molecules
-packaging molecules into protocells
-origin of self-replicating molecules
Earths atmosphere likely contained
-water
-chemicals released by volcanic eruptions (N, nitrogen oxides, CO2, methane, ammonia, H, HS
A. I. Oparin and J.B.S Haldane (1920s)
hypothesized that the early atmosphere was reducing the environment
Stanley Miller and Harold Urey(1953)
-did experiments that showed that the abiotic synthesis of organic molecules in a reducing atmosphere is possible
-demonstarted that organic molecules have formed with various possible atmosphere
RNA monomers
have produced spontaneously from simple molecules
First genetic material
probably RNA
RNA
could have been the template for DNA
Ribozymes
-RNA molecules
-found to catalyze many diff. reactions
-can make complementary copies of short stretched of RNA
Natural selection
produced self-replicating RNA molecules
Sedimentary rocks
deposited into strata
-richest source of fossils
Fossil record
-favors species that: existed for a long time, were abundant/widespread, and had hard parts
Tiktaalik
-early terrestrial vertebrate
-filled hole from the jump from water to land
Radiometric dating
-can determine absolute ages of fossils
-good for fossils up to 75,000 years old
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Parent isotope decays into daughter isotope at a constant rate
Half-life
time required for half the parent isotope to decay
Geologic record
-divided into the Archaean, Proterozoic, and Phanerozioc eons
-major boundaries between geological divisions correspond to extinction events in fossil record
Key events in life’s history
- origins of single celled and multicelled organisms
-colonization of land
Phanerozoic
-encompasses multicellular eukaryotic life
-broken down into Paleozoic, Mesozoic, and Cenozoic
-(please more coffee)
order for geologic record
-Phanerozic
Cenozoic
Mesozoic
Paleozoic
-Proterozoic
-Archaean
Stromatolites
-rocks formed by the accumulation of sedimentary players on bacterial mats
-oldest known fossils
-date back to 3.5 billion years ago
possible order for earth formation
-origin of solar system and earth
-prokaryotes
-atmosphere oxygen
-single-celled eukaryotes
-multicellular eukaryotes
-animals
-humans
O2
-produced by oxygenic photosynthesis reacted w/ dissolved iron and precipitated out to form banded iron formations
-2.7 billion years ago, oxygen accumulated in atmosphere