x) Normal
y) Reversed
z) Bipolar
x) rotary drilling
y) gravity coring
z) piston coring
x) mercury
y) DDT
z) PCBs
x) natural origin
y) future impact
z) human origin
y) predators
z) wave energy
x) asthenosphere
y) lithosphere
z) mesosphere
x) hydrogenous
y) cosmogenous
z) lithogenous
x) biomagnification
y) bioconcentration
z) bioaccumulation
x) carbon dioxide
y) water vapor
z) methane
x) for toxic chemical regulation
y) for food
z) for protection
x) paleomagnetism
y) paleogeography
z) magnetodynamics
x) oxygen
y) iron
z) calcium carbonate
x) the application of a dispersant to an oil spill
y) the use of bacteria and fungi to break down oil from a spill
z) passing water through scrubbers that remove the oil
x) More available nutrients along the continental margins.
y) Sunlight penetration is deeper at the continental margins.
z) There are fewer species along the continental margin
x) because the Pacific Ocean is larger
y) because the Atlantic Ocean is too cold
z) because of plate tectonics
x) rift valley
y) volcanic island arc
z) hotspot volcano
x) dinoflagellate
y) diatom
z) coccolithophore
x) chemical pollution
y) non-point source pollution
z) sewage sludge
x) ancient temperatures
y) proxy data
z) Milankovitch cycle
x) because the nutrients are not in a usable form for the zooxanthellae
y) because turbidity increases due to planktonic algal growth
z) because the nutrients are toxic pollutants to coral
x) Because older crust is covered up by younger sediment deposited in the ocean.
y) Because all of the older oceanic crust has risen above sea level and is now part of the continents.
z) Because the oldest crust is destroyed at subduction zones.
x) abyssal plain
y) continental rise
z) continental shelf
x) entanglement of animals
y) accumulation of toxic chemicals that are then ingested
z) persistence in the environment
x) decrease
y) increase
z) stay the same
x) because biomass is correlated with primary productivity
y) because the majority of sediment is on the continental shelf
z) because all benthic organisms rely on ocean currents