Introduction to Marine Biology and the Marine Environment

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Vocabulary practice flashcards covering ocean geology, water properties, ocean circulation, taxonomy, and marine biodiversity based on introductory marine biology lecture materials.

Last updated 7:47 PM on 10/9/26
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62 Terms

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Marine Biology

A branch of oceanography (marine science) involving the scientific study of plants and animals that live in the ocean and shoreline, or are dependent on the oceans, and how they interact with the environment.

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Oceanography

The interdisciplinary science that applies all sciences and engineering to study the oceans, including marine organisms, ecosystem dynamics, ocean currents, waves, plate tectonics, seafloor geology, and chemical and physical seawater properties.

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<p>Anton Dohrn Zoological Station</p>

Anton Dohrn Zoological Station

The first marine biological institute, founded in Naples in 1872 by German Darwinist Anton Dohrn to provide permanent access to laboratories, equipment, services, chemicals, and scientific books.

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Continental Drift

The hypothesis proposed in 1912 by Alfred Wegener stating that continental landmasses are not fixed in place, but constantly move across the globe at a slow pace.

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Oceanic Crust

The type of Earth crust underlying ocean basins that is younger, thinner, darker, denser, and basaltic compared to continental crust.

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Continental Crust

The type of Earth crust forming continental landmasses that is older, thicker, brighter, less dense, and granitic compared to oceanic crust.

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Subduction

A plate tectonic process occurring when dense oceanic crust collides with continental or another oceanic crust, sliding underneath into the mantle where it breaks and melts, provoking earthquakes and volcanic eruptions.

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Submarine Canyon

A steep-sided valley cutting into the continental shelf and continental slope, often terminating on the deep-sea floor in a fan-shaped wedge of sediment.

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Challenger Expedition

An 1872 scientific expedition that traveled 69,00069{,}000 nautical miles with specialized laboratories and dredges, collecting thousands of unknown species and publishing results across 50 volumes over 19 years.

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Specific Heat

The amount of heat energy required to change the temperature of 1 g1\,\text{g} of a substance by 1∘C1^\circ\text{C}. Water has a specific heat approximately 3,3003{,}300 times higher than air, allowing large water bodies to maintain relatively stable temperatures.

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Salinity

The total amount of dissolved salts in seawater, measured in grams of salt per kilogram of water (g/kg\text{g/kg}, ppt\text{ppt}, or psu\text{psu}), averaging about 35 psu35\,\text{psu} in the open ocean.

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Halocline

A vertical oceanic zone below the well-mixed surface layer where salinity changes rapidly with increasing depth.

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<p>Thermocline</p>

Thermocline

A distinct thermal layer in the water column in which temperature declines more rapidly with depth than in the layers directly above or below it.

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Ocean Acidification

The chemical process where excess atmospheric carbon dioxide (CO2\text{CO}_2) dissolves into seawater to form carbonic acid (H2CO3\text{H}_2\text{CO}_3), releasing hydrogen ions (H+\text{H}^+) that lower ocean pH and dissolve calcium carbonate (CaCO3\text{CaCO}_3) structures.

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Photic Zone

The uppermost layer of the ocean, extending from 0 m0\,\text{m} to approximately 200 m200\,\text{m} depth, where sufficient solar light penetrates to allow photosynthesis to occur.

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Coriolis Effect

The apparent deflection in the path of moving fluids or objects caused by Earth's rotation, bending paths toward the right in the Northern Hemisphere and toward the left in the Southern Hemisphere.

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Ocean Gyre

A large-scale circular flow pattern of surface ocean currents flowing around the perimeter of an ocean basin, generated by wind systems, continental boundaries, and the Coriolis effect.

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<p>Ekman Spiral</p>

Ekman Spiral

The spiraling pattern of water flow with depth in which wind deflects surface currents by up to 45∘45^\circ, and each succeeding deeper water layer moves at a slower speed and a greater angle until wind influence ceases at roughly 200 m200\,\text{m}.

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Sverdrup (Sv)

A unit of ocean volume transport equal to a flow rate of 1×106 m3/s1\times 10^6\,\text{m}^3/\text{s} (1 million cubic meters per second1\text{ million cubic meters per second}), named after oceanographer Harald Sverdrup.

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Thermohaline Circulation

Deep-ocean circulation driven by water density variations caused by differences in temperature (thermo) and salinity (haline), causing cold, dense surface water at polar latitudes to sink and slowly flow globally.

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Upwelling

The upward vertical movement of cold, nutrient-rich water from the deep ocean to the sunlit surface layer, typically induced by offshore wind stress and Ekman transport.

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Spring Tide

A tide with the greatest tidal range, occurring when the gravitational pulls of the Moon and Sun reinforce each other along a straight alignment.

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Neap Tide

A tide with the smallest tidal range, occurring when the Moon and Sun are situated at right angles relative to the Earth.

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Biodiversity

The variability among living organisms from all sources, including terrestrial, marine, and other aquatic ecosystems, encompassing genetic diversity within species, diversity between species, and diversity of ecosystems.

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Binomial Nomenclature

The standardized system of naming species introduced by Carolus Linnaeus in the 1750s, using two Latinized terms consisting of the genus name followed by the specific epithet.

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<p>Domain</p>

Domain

The highest taxonomic rank in biological classification, dividing all living organisms into Bacteria, Archaea, and Eukarya as established by Carl Woese in 1990.

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Autotroph

An organism that synthesizes its own organic food molecules from inorganic substances, predominantly using solar energy through photosynthesis.

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Heterotroph

An organism that cannot synthesize its own food and must obtain organic matter and energy by consuming other organisms.

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Detritivore

A heterotrophic organism that feeds primarily on dead and decomposing particulate organic matter.

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Filter Feeder

A suspension-feeding organism that strains particulate organic matter and small organisms directly out of the surrounding water, either actively via pumping or passively using cilia and mucus.

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<p>Coralligenous</p>

Coralligenous

A Mediterranean biogenic reef-like habitat produced on hard substrata mainly by the accumulation of encrusting, calcified red algae and associated sessile invertebrates.

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<p>Maerl Seabed</p>

Maerl Seabed

A marine benthic habitat composed of unattached, loose accumulations of living and dead branched calcareous red algae forming coarse biogenic gravel.

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Ladder of Life (Scala Naturae)

An early hierarchical biological classification scheme developed by Aristotle that cataloged thousands of species, including approximately 1,4001{,}400 marine organisms.

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Bathysphere

A spherical, steel deep-diving chamber lowered on a cable from a support ship, deployed in 1934 by William Beebe and Otis Barton to set an early ocean depth record of 923 m923\,\text{m} off Bermuda.

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Bathyscaphe Trieste

A free-diving deep-sea submersible vessel designed by Auguste Piccard that descended into the Challenger Deep of the Mariana Trench to a depth of 10,916 m10{,}916\,\text{m} in 1960.

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Aqua-Lung

An open-circuit self-contained underwater breathing apparatus co-invented in 1943 by Jacques-Yves Cousteau and Émile Gagnan, using a demand regulator to deliver compressed air on inhalation.

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Late Heavy Bombardment

A prolonged period of heavy meteoritic and cometary bombardment occurring roughly 3.8×109 years3.8\times 10^9\,\text{years} ago that delivered essential volatile compounds and water to early Earth.

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Hydrostatic Pressure Gradient in Seawater

The steady rate of compressive force increase with oceanic depth, equal to an increase of 1 atm1\,\text{atm} (≈101.3 kPa\approx 101.3\,\text{kPa}) for every 10 m10\,\text{m} of descent.

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Disphotic Zone

The intermediate marine depth stratum between approximately 200 m200\,\text{m} and 1,000 m1{,}000\,\text{m} that receives faint residual daylight insufficient to sustain net photosynthetic primary production.

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Aphotic Zone

The deep ocean layer extending below 1,000 m1{,}000\,\text{m} into absolute darkness, entirely shielded from solar irradiance.

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Mid-Ocean Ridge

An interconnected underwater volcanic mountain belt along divergent plate boundaries where rising magma forms new oceanic crust.

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Island Arc

A curved volcanic chain of islands produced above a subduction zone where one dense oceanic plate plunges underneath another oceanic plate.

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Abyssal Plain

A vast, extraordinarily flat expanse of the deep ocean basin floor typically situated at depths between 3,000 m3{,}000\,\text{m} and 6,000 m6{,}000\,\text{m}, mantled by thick terrigenous and pelagic sediments.

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Western-Boundary Currents

Deep, fast-flowing, and narrow surface ocean currents situated on the western edges of oceanic gyres that transport warm tropical water poleward (e.g., the Gulf Stream and Kuroshio Current).

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Eastern-Boundary Currents

Shallow, broad, and slow-moving surface ocean currents situated along the eastern edges of ocean basins that carry cool high-latitude waters toward the equator.

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Antarctic Circumpolar Current

The world's largest wind-driven ocean surface current, flowing unobstructed eastward around Antarctica without boundary deflection by continental landmasses.

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Downwelling

The downward vertical transport of well-oxygenated surface water toward the deeper oceanic layers, often triggered by surface water convergence or onshore Ekman transport.

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Equatorial Upwelling

The upward vertical movement of cold, nutrient-laden deep water along the equator, driven by wind-induced surface divergence under opposing hemispheric Coriolis forces.

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Generating Force

A mechanical disturbance—such as wind friction, seismic displacement, or gravitational pull—that disrupts an undisturbed water surface and produces waves.

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Restoring Force

The natural physical force (primarily gravity for ocean waves and surface tension for tiny capillary ripples) that acts to return a disturbed water surface back to equilibrium.

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Wavelength

The horizontal linear distance separating two successive crests or two successive troughs of an ocean wave.

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Wave Period

The total elapsed time required for two consecutive wave crests to transit past a fixed reference position.

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Breaker

A coastal ocean wave that steepens and collapses in the surf zone because bottom friction retards the base while the crest maintains forward velocity.

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Semidiurnal Tide

A tidal regime consisting of two high waters and two low waters of roughly equal tidal height over each lunar cycle of 24 h 50 min24\,\text{h}\,50\,\text{min}.

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Diurnal Tide

A tidal cycle exhibiting only a single high tide and a single low tide within a standard lunar day.

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Mixed Semidiurnal Tide

A tidal pattern consisting of two high tides and two low tides each lunar day that vary significantly in height and duration.

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Great Pacific Garbage Patch

A vast concentration of marine debris and photodegraded microplastics accumulated within the convergence zone of the North Pacific Subtropical Gyre.

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Scavenger

A heterotrophic organism that feeds primarily on dead organisms, discarded tissues, and carrion that it did not hunt or kill itself.

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Decomposer

An organism, such as a heterotrophic bacterium or marine fungus, that biochemically digests decaying organic matter to absorb nutrients and recycle minerals.

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Passive Suspension Feeder

A suspension feeder that lacks active cilia pumps or muscular siphons, relying instead on ambient water flow to carry particulate food onto mucus-lined tentacles or filaments.

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Genetic Diversity

The total inherited variability in alleles, nucleotide sequences, and genotypes present within a single biological species population.

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Ecosystem Diversity

The structural, biological, and ecological variety among distinct habitats, biological communities, and trophic processes across a given region or the planet.