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Q1: What does it mean that water has a high heat capacity?
It can absorb or release large amounts of heat with only small temperature changes.
Q2: How does water’s high heat capacity help moderate Earth’s climate?
Oceans store heat in the day/summer and release it slowly at night/winter, reducing temperature extremes.
Q3: What is latent heat of fusion?
The heat absorbed or released when water freezes or melts without a temperature change.
Q4: How does latent heat of fusion help stabilize Earth’s temperature?
Freezing and melting of water absorb or release heat, buffering temperature swings in polar and temperate zones.
Q5: What is latent heat of vaporization?
The energy absorbed or released during evaporation or condensation without temperature change.
Q6: How does latent heat of vaporization moderate climate?
Evaporation cools the ocean surface, and condensation releases that heat in the atmosphere, redistributing energy globally.
Q7: What type of bond holds hydrogen and oxygen together within one water molecule?
Covalent bond (intramolecular force).
Q8: What type of bond forms between different water molecules?
: Hydrogen bond (intermolecular force).
Q9: What is the freezing point of pure water?
0°C (32°F).
What is the freezing point of seawater with salinity of 35‰?
About -1.9°C (28.6°F).
Q11: What are the 3 major depth layers of the ocean?
Surface (mixed) layer, Pycnocline/Thermocline (middle), Deep layer.
Q12: Which layer is warmest?
The surface (mixed) layer.
Q13: Which layer is coldest?
The deep layer.
Q14: Where is the strongest pycnocline found globally?
In tropical regions, where warm surface water sits above cold deep water.
Q: What are the two main sources of salts in the ocean?
A: 1) Weathering and erosion of rocks on land (ions carried to the ocean by rivers)
2) Hydrothermal vents and volcanic outgassing adding ions from Earth’s crust
Q: What process on land contributes salts to the ocean?
A: Chemical weathering and erosion of continental rocks
Q: What process under the sea adds salts to the ocean?
A: Hydrothermal vent activity and submarine volcanism
Q: What are the seven most abundant ions dissolved in seawater?
A: Chloride (Cl⁻), Sodium (Na⁺), Sulfate (SO₄²⁻), Magnesium (Mg²⁺), Calcium (Ca²⁺), Potassium (K⁺), Bicarbonate (HCO₃⁻)
Q: Which two ions make up about 85% of seawater’s salinity?
A: Sodium (Na⁺) and Chloride (Cl⁻)
Q: What is the definition of “residence time” in ocean chemistry?
A: The average time an element or ion stays dissolved in seawater before being removed
Q: How is residence time calculated?
A: Residence time = (Amount of substance in ocean) ÷ (Rate of input or removal)
Q: What does a long residence time mean for an ion’s distribution?
A: It’s well-mixed and has a relatively constant concentration throughout the ocean
Q: What are conservative elements/ions?
A: Elements that have long residence times and constant ratios throughout the ocean
Q: Give two examples of conservative ions in seawater.
A: Sodium (Na⁺) and Chloride (Cl⁻)
Q: What are non-conservative elements/ions?
A: Elements whose concentrations vary with location and biological activity, due to short residence times
Q: Give two examples of non-conservative ions in seawater.
A: Nitrate (NO₃⁻) and Phosphate (PO₄³⁻)
Q: What is the average pH of modern seawater?
A: About 8.1 (slightly basic or alkaline)
Q: Is seawater acidic or basic?
A: Slightly basic
Q: How much is seawater pH expected to change in the next few decades?
A: A drop of about 0.3 to 0.4 pH units
Q: How does the expected future pH change compare to the change from the 1700s to 1900s?
A: The ocean’s pH dropped about 0.1 units between the 1700s and 1900s, so the current rate is 3–4× faster
Q: What causes the ocean’s pH to drop (acidification)?
A: Increased CO₂ absorption from the atmosphere forming carbonic acid (H₂CO₃) in seawater
Q: Why is ocean acidification especially harmful to calcifying organisms?
A: It decreases carbonate ion (CO₃²⁻) concentration, making it harder to form calcium carbonate shells and skeletons
Q: Give examples of calcifying marine organisms affected by ocean acidification.
A: Corals, mollusks (clams, oysters), foraminifera, and coccolithophores
Q: What is an autotroph?
A: An organism that produces its own food using energy from sunlight or chemical reactions.
Q: What is a heterotroph?
A: An organism that obtains its food by consuming other organisms.
Q: What are the four DNA base letters?
A: Adenine (A), Thymine (T), Cytosine (C), and Guanine (G).
Q: What are proteins used for in cells?
A: Building cell structures and performing chemical reactions (enzymes).
Q: What is found at trophic level 1 in a trophic pyramid?
A: Primary producers (autotrophs) such as phytoplankton.
Q: What is found at trophic level 2 in a trophic pyramid?
A: Primary consumers (herbivores or zooplankton) that eat the primary producers.
Q: What are the three domains of life?
A: Bacteria, Archaea, and Eukarya.
Q: What are the two main categories of plankton?
A: Phytoplankton and zooplankton
Q: What are two examples of algal primary producers?
A: Diatoms and dinoflagellates
Q: Which domain of life do algae belong to?
A: Eukarya
Q: What three nutrients most often limit ocean productivity?
A: Nitrogen, phosphorus, and iron
Q: What is the typical maximum depth of the euphotic zone?
A: About 200 meters
Q: What mainly limits photosynthesis in high-latitude regions?
A: Lack of sunlight
Q: Where are high-nutrient, high-productivity regions found?
A: Coastal upwelling zones and continental shelf areas
Q: What does the term “Cambrian Explosion” refer to?
A: A rapid diversification of animal life about 540 million years ago, when most major animal phyla first appeared in the fossil record.
Q: List the nine animal phyla (in order of increasing complexity) with examples.
A:
1⃣ Porifera – Sponges
2⃣ Cnidaria – Jellyfish, corals, anemones
3⃣ Platyhelminthes – Flatworms
4⃣ Nematoda – Roundworms
5⃣ Annelida – Segmented worms
6⃣ Mollusca – Snails, clams, octopuses
7⃣ Arthropoda – Crabs, shrimp, lobsters
8⃣ Echinodermata – Sea stars, sea urchins
9⃣ Chordata – Fish, mammals, birds
Q: What is the difference between ectothermic and endothermic marine organisms?
A:
Ectothermic: Body temperature depends on environment (e.g., most fish, invertebrates).
Endothermic: Maintain constant internal temperature (e.g., whales, seals, seabirds).
Q: What does “isotonic” mean in the context of marine organisms?
A: Their internal fluids have the same salinity (osmotic pressure) as seawater, preventing net gain or loss of water.
Q: Why can rocky intertidal environments host diverse and abundant life?
A: They provide stable surfaces for attachment, nutrient availability, and shelter from predators, allowing many species to coexist.
Q: Why are sand and muddy beaches inhospitable for abundant life?
A: They are unstable, constantly shifting, and provide few surfaces for attachment, making survival difficult.
Q: What factors have contributed to the decline of the Great Barrier Reef?
A: Climate change (warming oceans), coral bleaching, ocean acidification, pollution, and overfishing.
Q: What is the deep scattering layer (DSL)?
A: A layer in the ocean where zooplankton and fish migrate daily, reflecting sonar signals.
Q: At what depths do deep scattering layer communities live?
A: Roughly 200–1000 meters, migrating upward at night to feed.
Q: What communities are found at mid-ocean ridges?
A: Hydrothermal vent communities.
Q: What are the primary producers that fuel mid-ocean ridge ecosystems?
A: Chemosynthetic bacteria that use chemicals from vent fluids.
Q: What are some characteristic animals at hydrothermal vents?
A: Tube worms, giant clams, vent crabs, and shrimp.
Q: What is symbiosis?
A: A close ecological relationship between two different species.
Q: What is mutualism? Give an example.
A: Both species benefit; e.g., coral and zooxanthellae.
Q: What is commensalism? Give an example.
A: One species benefits, the other is unaffected; e.g., barnacles on whales.
Q: What is parasitism? Give an example.
A: One species benefits, the other is harmed; e.g., parasitic copepods on fish.