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Biosphere, Lithosphere, Hydrosphere, Atmosphere
Earth’s Spheres
Lithosphere
the solid (or molten) Earth
Hydrosphere
liquid Earth (cryosphere is the frozen Earth)
Element
a substance that cannot be broken down into simpler substances by chemical means; same number of PROTONS in nucleus, so same ATOMIC NUMBER
Isotope
Atoms of an element with different numbers of neutrons (and hence different atomic masses); some are radioactive
Different isotopes of an element will behave very similarly but have crucial
differences in fractionation and chemical reaction rates
Are isotopes of the same element similar or different? How?
Ion
Electrically charged (positive or negative) molecules or atom
Carbon
basic building block of organic molecules, 4 bonds
Hydrogen
Smallest and most abundant element, fills out organic molecules because it only needs one bond
Oxygen
Two bonds – Strong oxidizer (really wants to steal electrons)
Nitrogen
3 bonds – key element in protein structure
Phosphorus
Key element in cellular energy (ATP) and in DNA
Sulfur
Important component in amino acids (proteins)
Calcium
Mineral that serves a structural role
Iron
Used in proteins, often for transferring electrons
Covalent bonds
strong bonds formed by sharing of electrons; can be equal sharing (nonpolar) or unequal sharing (polar)
Ionic bonds
Strong bonds formed when one atom transfers its electrons to another; The two ions (positive and negative) are then strongly attracted to each other
Dipole (hydrogen) bonds
Weak bonds formed between polar molecules
Water molecule
Can break apart into OH- (hydroxide) and H+ (hydrogen) ions. Neutral is pH of 7.
Acidity
in water; refers to the relative balance of H+ and OH- (high H+ is acidic)
Organic Molecules
Made of carbon atoms covalently bonded to other carbon atoms or hydrogen, nitrogen, oxygen, and other elements; the primary structural and functional elements of
organisms
Carbohydrates, lipids (fats), proteins, nucleic
acids (DNA), hydrocarbons
Organic molecules include
Inorganic Molecules
molecules without carbon-carbon bonds
Carbohydrates
Carbon, hydrogen, and oxygen; includes sugars like glucose
Lipids (fats & oils)
Long chains of carbon and hydrogen, and a short region with one or more oxygen atoms; form most cellular membranes and also used as energy storage
Hydrocarbons
organic molecules comprised entirely of Carbon & Hydrogen; Includes methane, ethane, propane, etc.
Macromolecules
combinations of small organic molecules
Polysaccharides
polymers (chains) of simple sugars (e.g. starch & cellulose)
Proteins
polymers of amino acids (nitrogen-containing organic molecules); there are 20 different amino acids, 100-1000 amino acids linked in a chain. Fold in on themselves into complex three-dimensional structures and mediate most of the organism’s functions
Nucleic acids
polymers of nucleotides
Nucleotides
small molecules that contain a 5-C sugar, a phosphate (PO4) group, and a nitrogenous base
DNA
a nucleic acid formed of 4 nucleotides (A,T,G,C)
prokaryotes; fermentation
The earliest forms of life on Earth were ____ that got their energy from _____
low; alcohol and CO2
Fermentation has a ____ energy yield and gives off ______ and ____ as waste products
Prokaryote
single-celled organisms that lack cellular organelles (nucleus, mitochondria, etc.); bacteria and archaebacteria, including cyanobacteria
Cyanobacteria
led to the rise of oxygen
Eukaryotes
Organisms that have membrane-enclosed structures in their cells (e.g. nucleus, mitochondria, chloroplast); include protists, fungi, plants, animals.
True
T/F: Biogeochemical cycles often involve organisms interacting with the abiotic (non-living) portion of their environment
Rocks and Soil
Continually created, maintained, changed and destroyed over the last 4.6
billion years due to physical, chemical, and biological processes
Tectonic, Hydrologic, Rock, Biogeochemical
Geologic cycles
Tectonic Geological Cycles
formation of mountains, continents, etc.
Rock Geologic Cycles
Weathering
Gravity pulled heavy materials to center, creating a dense core (nickel & iron) with high pressure then a lesser dense mantle and a lighter rocky crust
How did Earth become formed?
Continental crust is the thickest. Oceanic crust is the densest
Is oceanic or continental crust more thick? Which one is more dense?
Plate tectonics
By Alfred Wegner; Earth’s crust is broken into different plates that float on top of mantle and their movement is driven by convection currents in the upper mantle.
Plate Boundaries
areas where plates come together
The Hydrologic Cycle
The transfer of water from oceans to the atmosphere to the land and back
to the oceans; driven by solar energy
Precipitation above a watershed directly affects water levels throughout that watershed; Water flows in the watershed transport nutrients (and pollutants) across the watershed
Why do we care about watersheds?
Catchments
small drainage basins within a larger watershed
True
T/F: Water falling outside of the watershed will not be transported into the watershed