Marine Biology Lecture Notes Review

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Flashcards covering the history of marine science, ocean floor features, currents, marine biology adaptations, habitat types, and human impacts based on the course transcript.

Last updated 10:46 PM on 6/8/26
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56 Terms

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Aristotle

Early scientist known for his early natural history observations.

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Carl Linnaeus

Scientist who developed the foundations for taxonomy and classification.

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Coral Reef Subsidence Theory

Charles Darwin's theory that volcanic islands sink from cooling and tectonic shifts while coral grows upward.

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Alfred Russel Wallace

Scientist who studied biogeography and identified the Wallace Line.

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Azoic Theory

Proposed by Edward Forbes, it stated that no life could exist below a specific depth limit.

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HMS Challenger Expedition

The first global oceanographic expedition.

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Sylvia Earle

Known as "Her Deepness," she is a pioneer in deep sea exploration.

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Ring of Fire

A region around the Pacific Ocean characterized by high marine biodiversity, deep-sea trenches, island formation, and hydrothermal vents.

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Continental shelf

A shallow, gently sloping region extending from the coast that is the most biologically productive region of the ocean.

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Continental slope

A steep drop-off connecting the shallow shelf to the deep ocean floor, often containing submarine canyons.

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Mid-ocean ridges

Underwater mountain ranges at divergent plate boundaries where new oceanic crust is formed via magma welling up.

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Divergent boundaries

Tectonic plates that pull apart, leading to seafloor spreading and mid-ocean ridges.

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Convergent boundaries

Plates that collide, causing subduction where dense oceanic crust slides into the mantle, creating trenches.

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Transform boundaries

Tectonic plates that grind past one another horizontally, such as the San Andreas Fault.

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Magnetic striping

Evidence for seafloor spreading consisting of alternating bands of normal and reversed magnetic polarity.

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Coriolis Effect

The deflection of moving water or air caused by Earth's rotation, deflecting to the right in the Northern Hemisphere and the left in the Southern Hemisphere.

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Gyres

Large circular current systems that rotate clockwise in the Northern Hemisphere and counter-clockwise in the Southern Hemisphere.

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Upwelling

A process driven by wind and the Coriolis effect where surface water is pushed away, allowing deep, cold, nutrient-rich water to rise.

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Downwelling

The sinking of surface water that transports oxygen downward but results in lower nutrients at the surface.

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Thermohaline Circulation

Density-driven deep ocean circulation controlled by temperature and salinity, also known as the global conveyor belt.

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Tsunamis

Long, low, and fast-moving waves caused by earthquakes or volcanic eruptions characterized by a long wavelength and low wave height.

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Semidiurnal tides

Common tidal pattern consisting of two high tides and two low tides of approximately equal height per day.

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Spring tides

Tides with the greatest tidal range occurring when the Sun and Moon are aligned.

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Neap tides

Tides with the smallest tidal range occurring when the Sun and Moon are at right angles.

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Oxygen Minimum Zones (OMZ)

Low O2 areas at depth caused by high bacterial respiration and weak circulation.

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Photic zone

The upper 200m200\,m of the ocean water column where enough light penetrates for photosynthesis to occur.

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Chemosynthesis

The process used by bacteria at hydrothermal vents to produce energy from chemicals like hydrogen sulfide instead of sunlight.

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Ocean Acidification

The process of atmospheric CO2CO_2 dissolving into the ocean to form carbonic acid, lowering pH and reducing carbonate ions needed for calcification.

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Poikilotherms

Organisms that conform their internal temperature to the surrounding environment.

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Homeotherms

Organisms like marine mammals and birds that regulate their own internal body temperature.

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Countercurrent Heat Exchange (CCHE)

An adaptation where heat from outgoing arterial blood is transferred to incoming venous blood to retain warmth.

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Osmoconformers

Invertebrates that conform their internal osmolarity to the environment to lower energy costs.

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Osmoregulators

Organisms like bony fish that maintain a constant internal osmolarity regardless of the environment.

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Reynolds Number (ReRe)

A ratio of inertial forces to viscous forces; Re<1Re < 1 means viscous forces dominate (water feels thick), and Re>1000Re > 1000 means inertial forces dominate.

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Plankton

Organisms that drift with currents and cannot swim against them.

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Phytoplankton

Photosynthetic primary producers that form the base of the marine food web.

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Coccolithophores

Nanoplankton characterized by calcium carbonate (CaCO3CaCO_3) scales.

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Diatoms

Phytoplankton with silica (SiO2SiO_2) cell walls called frustules, major producers in upwelling zones.

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Dinoflagellates

Phytoplankton with two flagella, some of which are bioluminescent or cause harmful algal blooms (Red Tides).

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Holoplankton

Organisms that remain plankton for their entire life cycle, such as copepods.

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Meroplankton

Organisms that are only planktonic during their larval stage, such as crab or fish larvae.

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Nekton

Active swimmers capable of overcoming ocean currents, such as fish, squid, and whales.

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Countershading

A camouflage adaptation with a dark top and light underside that blends in when seen from above or below.

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Net Primary Productivity (NPP)

The rate at which energy is stored after respiration, calculated as NPP=GPPRNPP = GPP - R.

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Compensation depth

The depth at which the rate of photosynthesis equals the rate of respiration (P=RP = R).

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Suspension feeders

Organisms that filter food from the water, categorized as active (pumping water) or passive (relying on currents).

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Deposit feeders

Organisms that consume organic matter from the sediment.

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Bioturbation

The mixing of sediments by organisms while they are feeding or burrowing.

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Spartina

Salt-tolerant marsh grasses that stabilize habitats by trapping sediment and protecting against erosion.

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Aerenchyma tissue

Specialized air spaces in salt marsh plants that transport oxygen to roots in anoxic mud.

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Desiccation

Stress caused when an organism loses water faster than it can replace it, common in the high intertidal zone.

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Keystone Species

A species with a disproportionate impact on its ecosystem, such as the PiasterochraceusPiaster\,ochraceus sea star in rocky intertidal zones.

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Trophic Cascade

An ecological phenomenon where predators at high trophic levels affect the abundance of organisms at lower levels (e.g., sea otters protecting kelp by eating urchins).

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Zooxanthellae

Symbiotic photosynthetic algae (Symbiodiniaceae) that live inside coral polyps and provide energy.

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Bycatch

The unintended capture of non-target species during fishing, such as turtles or dolphins.

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Pacific Decadal Oscillation (PDO)

A long-term (decades-long) oceanic temperature shift that influences fish population trends.