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Terrestrial Planets
smaller rocky, denser, with solid surfaces and relatively few moons
Mercury, Venus, Earth, Mars
Jovian Planets
large outer planets
Jupiter and Saturn (gas giants), Uranus and Neptune (Ice giants)
Asteroids
rocky/metallic small bodies
Comets
ice-rich bodies that can form tails near the sun
Kuiper Belt
lies beyond Neptune
Oort Cloud
proposed distant comet reservoir
Inner nebula
too hot for many ices to condense
Colder Nebula
permitted more solid material and the growth of larger cores
Nebular Theory
a gas and dust cloud collapsed gravitationally, spun faster as angular momentum was conserved, and flattened into a disk
the sun formed in the center. cooling enabled condensation of solids; accretion formed planetesimals, embryos, and planets
Evidence of the Nebular Theory
mostly aligned, same-direction planetary orbits; differences between inner and outer planets; disks around young stars
Condensation
formation of solids from gas
Accretion
Growth by accumulation
Differentiation
internal separation by density
Parts of the Earth
crust, mantle, outer core, inner core
Crust
thin solid exterior
Mantle
slowly deforming solid rock
Outer core
liquid metal
Inner core
solid metal
Plate Tectonics
divergent boundaries separate, convergent boundaries collide/subduct, transform boundaries slide past
Hadean Earth
the oldest geologic eon of Earth’s history.
Giant-impact hypothesis
debris from a collision between early Earth and a large impactor formed the Moon
Prokaryotes
lack a membrane-bound nucleus
Eukaryotes
has a membrane-bound nucleus
Definition of Life
a working definition of life is a self-sustaining chemical system capable for Darwinian evolution. Viruses are a boundary case because they depend on hosts to produce
Three domains
Bacteria, Archaea, Eukarya
Cell membrane
regulated exchange
DNA
stores hereditary information
Ribosomes
build proteins
Mitochondria
participate in aerobic ATP production
Metabolism
all cellular chemistry
Catabolism
breaks molecules down
Anabolism
build molecules
Phototrophs
use light for energy
Chemotrophs
use chemical reactions
Autotrophs
use inorganic carbon
Heterotrophs
use organic Carbon
Oxygenic Photosynthesis
6CO2 + 6H2O + light -> C6H12O6 + 6O2
biological process where plants, algae and cyanobacteria use light energy to split water molecules, producing chemical energy (ATP and NADPH), organic carbon, and molecular oxygen (O2) as a byproduct
Aerobic Respiration
reverses the overall reactant/product relationship and releases usable energy
DNA Base pairs
A-T and C-G.
DNA Replication
copies DNA
DNA Transcription
makes RNA
DNA Translation
builds proteins
Mutation
creates heritable variation
Natural selection
changes trait frequencies through differences in reproductive success; genetic drift changes allele frequencies randomly
Thermofiles
thrive in heat
Psychrophiles
thrive in the cold
Halophiles
thrive in salt
Acidophiles
thrive in acidity
Piezophiles
thrive at high pressure
Extremophiles
expand our ideas about potentially habitable environments but do not prove alien life exists
Evidence for evolution:
fossils, DNA relationships, comparative anatomy, biogeography, and observed changes, Evolution explains diversification, not the initial origin of life
Abiogenesis
means life emerging from nonliving chemistry.
Biosignature
a possible sign of life, not necessarily definitive proof
Primordial soup:
organic molecules accumulate and react in water-rich environments,
Hydrothermal vents
chemical gradients and mineral surfaces may facilitate complex chemistry
RNA world
RNA may once have served both information and catalytic roles
Miller-Urey experiment
produced organic compounds from simple starting chemicals under simulated conditions; it did NOT produce living organisms
Protocells
are membrane-line chemical compartments that may have preceded modern cells
Great Oxidation Event
2.4 billion years ago
major increase in atmospheric oxygen
Humans and chimpanzees
humans and living chimpanzees share a common ancestry; human evolution was branching, not a single ladder. Artificial life models life-like systems but is not automatically biological life.
Accretion vs Differentiation
growing a plant vs separating its internal materials
Relative vs Radiometric dating
ordering events vs assigning numerical ages
Positive vs Negative feedback
amplifying vs opposing an initial change
Autotroph vs Phototroph
carbon source vs energy spruce
Evolution vs Abiogenesis
changes in existing life vs initial emergence of life
Miller-Urey vs RNA world
an experiment producing organics vs a hypothesis about early replicating/catalytic chemistry
Natural selection vs drift
differential reproduction vs random changes
Habitability
depends on suitable conditions for liquid water, energy sources, necessary elements, and environmental stability
Natural greenhouse gases
they abosrob/reemit infrared radiation and help keep Earth warm. More greenhouse gases can enhance warming.