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A comprehensive set of vocabulary flashcards covering key terms and definitions from the “Life in the Ocean” lecture, designed to reinforce concepts on oceanic biology, chemistry, and ecology.
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Microbe
Microscopic organism (bacteria, archaea, viruses) that dominates ocean biomass and drives most primary production.
Primary Production
Creation of organic compounds from inorganic substances using an external energy source (light or chemical).
Autotroph
Organism that produces its own food from inorganic compounds (e.g., via photosynthesis or chemosynthesis).
Heterotroph
Organism that must consume organic compounds for energy; occupies higher levels of the food chain.
Photosynthesis
Light-driven reaction converting CO₂ and H₂O into glucose and O₂; occurs in the ocean’s photic zone.
Chemosynthesis
Production of organic matter using chemical energy from oxidation of substances like H₂S; common at hydrothermal vents.
Photic Zone
Upper sunlit layer of the ocean where light supports photosynthesis.
Aphotic Zone
Deep ocean layer where light is insufficient for photosynthesis.
Compensation Depth
Depth where photosynthetic O₂ production equals respiratory O₂ consumption (P = R).
Limiting Nutrient
Essential element present in too low a concentration to support maximum biological growth (e.g., N, P, Fe, Si).
Nitrogen Cycle
Biogeochemical movement of nitrogen among seawater, organisms, and sediments (nitrate, nitrite, ammonium forms).
Phosphorus Cycle
Circulation of phosphorus (mostly as phosphate) between organisms and seawater; driven by decomposition and excretion.
Silica
Dissolved SiO₄⁴⁻ ion used by diatoms and radiolarians to build siliceous tests; often a limiting nutrient.
Iron
Trace metal required for photosynthesis; delivered mainly by dust and runoff; limiting in many ocean regions.
Organic Compound
Molecule built on carbon chains or rings (e.g., methane, glucose, lipids, proteins, DNA).
Respiration
Process in which organisms oxidize glucose with O₂ to release energy, producing CO₂ and H₂O.
Detritivore
Organism that feeds exclusively on detritus (waste particles).
Decomposer
Microbe (archaea, bacteria, fungi) that breaks down dead organic matter, recycling nutrients.
Diel Vertical Migration
Daily movement of plankton to deeper water by day and surface water by night, transporting nutrients.
Upwelling
Vertical movement of deep, nutrient-rich water to the surface, fueling high primary productivity.
Biomass
Total mass of living organisms in a given area; in plankton, controlled by productivity versus predation.
Chlorophyll Concentration
Satellite-measured proxy for phytoplankton biomass and productivity.
Plankton
Organisms that drift with currents and cannot swim effectively against them.
Picoplankton
Plankton < 2 µm in size.
Nanoplankton
Plankton 2–20 µm in size.
Microplankton
Plankton 20–200 µm in size.
Mesoplankton
Plankton 0.2–20 mm in size.
Macroplankton
Plankton 20–200 mm in size.
Megaplankton
Plankton > 200 mm in size.
Phytoplankton
Photosynthetic planktonic organisms (plants & algae) forming the base of marine food webs.
Diatom
Silica-shelled phytoplankton responsible for large share of oceanic primary production; forms siliceous ooze.
Dinoflagellate
Flagellated phytoplankton; some species cause harmful algal blooms (HABs).
Coccolithophore
Calcium-carbonate-shelled phytoplankton; contributes to calcareous ooze.
Cyanobacteria
Photosynthetic bacteria; genus Prochlorococcus may account for up to 80 % of photosynthesis in low-nutrient areas.
Sargassum
Genus of floating macroalgae forming surface mats that create unique habitats.
Holoplankton
Organisms that remain plankton for their entire life cycle (e.g., copepods, krill, pteropods).
Meroplankton
Larval stages of organisms that later become nektonic or benthic (e.g., fish, mollusk larvae).
Copepod
Small crustacean mesoplankton; together with krill and amphipods forms 60–70 % of zooplankton biomass.
Krill (Euphausiid)
Shrimp-like crustacean mesoplankton crucial to food webs, especially in polar regions.
Foraminifer
Calcareous-shelled protozoan microplankton; important in marine sediments (calcareous ooze).
Radiolarian
Silica-shelled protozoan microplankton; contributor to siliceous ooze.
Gelatinous Plankton
Soft-bodied holoplankton such as jellyfish, comb jellies, and salps (some bioluminescent).
Prochlorococcus
Tiny cyanobacterium dominating primary production in nutrient-poor open oceans.
HAB (Harmful Algal Bloom)
Rapid proliferation of toxic or nuisance phytoplankton (e.g., Alexandrium, Pseudo-nitzschia).
Nekton
Active swimmers capable of overcoming currents (fish, mammals, squid, birds, reptiles).
Taxonomic Ranking
Hierarchical biological classification: Domain, Kingdom, Phylum, Class, Order, Family, Genus, Species.
Archaea
Single-celled prokaryotes distinct from bacteria; many are obligate anaerobes, some are chemosynthetic.
Eukarya
Domain of organisms with membrane-bound nuclei, including protists, fungi, plants, and animals.
Thermocline
Ocean layer of rapid temperature change with depth, separating warm surface from cold deep water.
Pycnocline
Ocean layer of rapid density change, often controlled by variations in temperature and salinity.