EE 144 Exam #4 Review
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Liebig’s Law of the Minimum states that phytoplankton growth is regulated not by the total amount of nutrients available but by the amount of the ______ resource.

scarcest

The ratio of C:N:P in phytoplankton is commonly known as the ______ Ratio.

Redfield

Micronutrients such as ______, Mn, and Zn can sometimes limit productivity in marine ecosystems.

Fe

Respiration is photosynthesis in ______.

<p>reverse</p> Signup and view all the answers

The N:P ratio of seawater is typically close to ______:1.

<p>16</p> Signup and view all the answers

Organic matter that sinks in the ocean is referred to as ______ snow.

<p>marine</p> Signup and view all the answers

Macronutrients that can be limiting to marine productivity include nitrogen, phosphate, and ______.

<p>silica</p> Signup and view all the answers

Redfield’s work showed that the ratio of C:N:P for phytoplankton is ______:16:1.

<p>106</p> Signup and view all the answers

During interglacial periods, atmospheric CO2 levels generally go ______.

<p>up</p> Signup and view all the answers

During glacial periods, more carbon is 'pumped' out of the atmosphere and into the ______.

<p>deep ocean</p> Signup and view all the answers

The 'solubility pump' is related to the chemistry and physics of CO2 dissolving in ______.

<p>seawater</p> Signup and view all the answers

Industrialization has caused atmospheric CO2 to increase well above levels typical of an ______.

<p>interglacial</p> Signup and view all the answers

The 'biological pump' involves the uptake of CO2 by photosynthetic ______.

<p>phytoplankton</p> Signup and view all the answers

HNLC regions are parts of the ocean with high concentrations of nutrients but ______ actually being taken up by phytoplankton.

<p>not</p> Signup and view all the answers

CO2 is more soluble in ______ water, influencing the carbon cycle in polar regions.

<p>cold</p> Signup and view all the answers

Iron (Fe) limitation is the general explanation for ______ regions in the ocean.

<p>HNLC</p> Signup and view all the answers

One approach to conservation of marine biodiversity is establishment of a global network of marine ______.

<p>reserves</p> Signup and view all the answers

A metapopulation refers to a larger population made up of many local ______.

<p>populations</p> Signup and view all the answers

Understanding the connectivity of metapopulations is important to managing biodiverse marine ______.

<p>reserves</p> Signup and view all the answers

The median dispersal of baby fish was found to be only ______ km.

<p>1.7</p> Signup and view all the answers

A possible conservation solution is to establish 'stepping stone' reserves between the major ______.

<p>reserves</p> Signup and view all the answers

The first mid-ocean ridge hydrothermal vents were discovered in ______ at the Galapagos Rift.

<p>1977</p> Signup and view all the answers

Measurements of very hot water in the ______ Sea were among the early indications of hydrothermal vents.

<p>Red</p> Signup and view all the answers

Rocks dredged from the Mid-Atlantic Ridge showed evidence of hydrothermal ______, involving reactions between seawater and basalt rock.

<p>alteration</p> Signup and view all the answers

Coral reefs are sensitive to sediment, nutrient loading, acidification, and ______.

<p>temperature</p> Signup and view all the answers

The colorful symbiotic photosynthetic dinoflagellates that corals eject during bleaching are called ______.

<p>zooxanthellae</p> Signup and view all the answers

Polyps secrete calcium ______, building the hard reef structure over time.

<p>carbonate</p> Signup and view all the answers

The structure that the polyp sits in is called a ______.

<p>corallite</p> Signup and view all the answers

Coral reefs are large platforms built up of calcium carbonate (______ ) over thousands of years.

<p>limestone</p> Signup and view all the answers

Ophiolites are sections of ocean crust emplaced on land by ______ tectonics.

<p>convergent</p> Signup and view all the answers

Seafloor hydrothermal vents are the exit points for seawater that circulates through the hot ocean ______.

<p>crust</p> Signup and view all the answers

Hydrothermal water from the vents is heated to temperatures between ______ and 400°C.

<p>350</p> Signup and view all the answers

The black 'smoke' seen at hydrothermal vents consists of metal-______ minerals.

<p>sulfide</p> Signup and view all the answers

The process of ______ uses energy from chemical reactions to produce organic matter.

<p>chemosynthesis</p> Signup and view all the answers

The tubeworm ______ is a well-known member of the hydrothermal vent community.

<p>Riftia</p> Signup and view all the answers

Vents and vent communities are only active for a few ______ before relocating.

<p>decades</p> Signup and view all the answers

When hydrothermal water mixes with seawater, it creates significant chemical ______.

<p>gradients</p> Signup and view all the answers

Deep sea whale carcasses serve as a temporary home as stepping stones moving towards new active _____

<p>vents</p> Signup and view all the answers

The term _____ refers to the water column in oceanic ecosystems.

<p>pelagic</p> Signup and view all the answers

The _____ province includes the shallow ocean up to the low tide line.

<p>neritic</p> Signup and view all the answers

The intertidal zone, also called the _____ province, is exposed to air at low tide.

<p>littoral</p> Signup and view all the answers

Benthic communities can be divided based on substrate, often categorized as hard-bottom vs _____-bottom.

<p>soft</p> Signup and view all the answers

Estuaries are coastal zones typically located at the mouths of rivers where _____ and seawater mix.

<p>freshwater</p> Signup and view all the answers

Barrier islands protect the mainland by acting as storm _____ barriers.

<p>energy</p> Signup and view all the answers

Muddy soft-bottom communities tend to have more _____ feeders.

<p>deposit</p> Signup and view all the answers

Flashcards

Limiting Factors for Marine Productivity

Nutrients, like nitrogen, phosphate, and silica, that restrict the growth of phytoplankton, even if other nutrients are plentiful.

Redfield Ratio

The typical ratio of carbon, nitrogen, and phosphorus in phytoplankton (106:16:1).

Liebig's Law of the Minimum

Phytoplankton growth is controlled by the scarcest nutrient, not the total amount available.

Limiting Nutrient (e.g.Nitrogen)

The nutrient that's in shortest supply relative to a plant's needs, thereby limiting its growth.

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Micronutrients

Essential nutrients required in tiny amounts, but can still limit marine productivity in certain circumstances (ex: iron).

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Nutrient Sources in Marine Ecosystems

Nutrients come from diverse sources, including river runoff and the regeneration of organic matter from respiration.

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Respiration

The process where decomposers consume organic matter, releasing CO2 and regenerating nutrients in seawater. It's essentially photosynthesis in reverse.

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Marine Snow

Sinking organic matter, sampled using sediment traps in the water column.

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Atmospheric CO2 during glacial periods

During glacial periods, more carbon is removed from the atmosphere and stored in the deep ocean.

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Atmospheric CO2 during interglacial periods

During interglacial periods, carbon stored in the deep ocean is released back into the atmosphere.

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Solubility pump

The process of carbon dioxide dissolving in seawater, moving to the deep ocean and then returning to the surface.

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Biological pump

Phytoplankton absorb CO2, and the carbon is transported to the deep ocean as marine snow (e.g., fecal pellets).

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HNLC regions

High nutrient, low chlorophyll regions of the ocean.

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Iron limitation in HNLC regions

A lack of iron prevents phytoplankton from using available nutrients to grow.

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Mauna Loa CO2 record

A continuous record of atmospheric CO2 concentration since 1958.

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Ocean's carbon uptake

The ocean absorbs significant amounts of CO2 released by human activities.

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Marine Reserve Connectivity

The degree to which marine populations among protected areas are interconnected, allowing for movement and gene flow.

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Metapopulation

A large population composed of many smaller, interconnected local populations.

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Dispersal Kernel

The pattern of dispersal of individuals (like fish larvae) from a central location, showing how far they travel.

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Reef Fish Dispersal

The movement of reef fish, primarily through larval stages influenced by ocean currents, showing a limited dispersal range.

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Stepping Stone Reserves

Smaller reserves strategically placed between larger protected areas to improve connectivity and facilitate gene flow.

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Hydrothermal Vent

A fissure in the Earth's crust from which hot mineral-rich water erupts.

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Mid-Ocean Ridge

An underwater mountain range where new oceanic crust is formed.

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Hydrothermal Vent Communities

Unique ecosystems thriving near hydrothermal vents, adapted to extreme conditions with chemosynthesis at their base.

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Coral Bleaching

A process where corals, stressed by high water temperatures, expel their symbiotic algae (zooxanthellae), causing them to turn white and become vulnerable.

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Coral Reefs: Hard Bottom Communities

Coral reefs are vibrant, high-energy ecosystems built by coral polyps, featuring diverse seaweeds, filter feeders, grazers, and predators.

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Coral Polyp

The individual, animal building block of a coral reef. A coral polyp secretes calcium carbonate to build its protective skeleton, called a corallite.

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Zooxanthellae

Symbiotic, photosynthetic dinoflagellates living inside coral polyps. They provide food for the coral and give it its color.

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Coral Reef Threats

Coral reefs face various threats, including sedimentation, nutrient pollution, ocean acidification, and rising temperatures.

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Pelagic vs. Benthic

Pelagic refers to organisms and processes in the water column, while benthic refers to those in or on the sediment at the seafloor.

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Oceanic vs. Neritic

Oceanic province is the deep ocean, while neritic province is the shallow ocean including the continental shelf.

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Littoral Province

The intertidal zone, the area between high and low tide lines that is periodically underwater or exposed to air.

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Why is the open ocean sparse?

The open ocean (oceanic province) has low biological productivity because nutrient concentrations are low.

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Epipelagic Zone

The top 200 meters of the oceanic province, where sunlight penetrates and supports most life.

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Coastal Ocean - A Feast of Life

The coastal ocean is teeming with life, featuring high biodiversity and productivity due to diverse environmental gradients.

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Estuaries as Mixing Zones

Coastal zones where freshwater and saltwater mix, like the Chesapeake Bay and Delaware Bay.

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Barrier Islands and Lagoons

Barrier islands are sandbars protecting lagoons (quiet water behind islands), offering storm protection for the mainland.

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Ocean Crust Heat Flow

The ocean crust is surprisingly cool, given its proximity to magma. This is due to heat loss through seawater circulation, which carries away heat efficiently.

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Chemosynthesis

A process where organisms use energy from chemical reactions, like the interaction of hydrogen sulfide and oxygen, to create food.

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Black Smokers

These are hydrothermal vents that release dark, metal-rich fluids, creating a striking visual contrast with the surrounding water.

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Riftia Tubeworms

These iconic vent animals rely on symbiotic bacteria to obtain energy through chemosynthesis.

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Vent Communities

These unique ecosystems thrive near hydrothermal vents, relying on energy from chemosynthesis, not sunlight.

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Vent Community Transience

Hydrothermal vents are ephemeral, only active for a few decades before shifting location or ceasing activity.

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Population Connectivity

The question of how vent communities move to new locations after their old vent stops emitting hydrothermal water.

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Study Notes

EE 144 Exam #4 Review

  • Exam format includes multiple choice, matching, fill-in-the-blank, diagram interpretation, and sketching.
  • Calculations will use round numbers, calculator not needed.
  • No equations need memorizing.
  • Exam covers lectures 26-34 (Wednesday, Dec 4).
  • Exam excludes reading material not covered in class.

Lecture 26

  • Understand limiting factors for new productivity (light or nutrients).
  • Macronutrients limiting marine productivity include nitrogen (nitrate, nitrite, ammonia), phosphate, and silica for diatoms.
  • Redfield Ratio (C:N:P) for phytoplankton is 106:16:1. (C:N:P:Si in diatoms is 106:16:1:16).
  • Liebig's Law of the Minimum: phytoplankton growth is limited by the scarcest resource, not the total amount available.
  • Micronutrients (metals like Fe, Mn, Cu, Zn, B, Mo) can also limit productivity, though requirements are small.
  • Sources of nutrients to marine ecosystems include nitrogen and phosphorus.
  • Respiration consumes oxygen, produces CO2, and regenerates nutrients, thus, N:P ratio of seawater is often close to 16:1.
  • "Marine snow" is sinking organic matter, sampled with sediment traps.

Lecture 27

  • Carbon cycle relationship with climate, carbon, and marine productivity.
  • Data from polar ice cores shows atmospheric CO2 rises during interglacials and falls during glacial periods.
  • Carbon is pumped into the deep ocean during glacial periods, returning to the atmosphere during interglacials.
  • Solubility pump and biological pump account for carbon removal.
  • Industrialization and fossil fuels have caused CO2 to increase beyond interglacial levels, seen in Mauna Loa CO2 record since 1958.
  • Oceans absorb half of anthropogenic CO2, much taken up by deep North Atlantic.
  • Annual CO2 cycle related to photosynthesis and respiration balance.

Lecture 28

  • Stellwagen Bank, a US National Marine Sanctuary, is a summer feeding ground for humpback whales.
  • Stellwagen Bank's geology: shallow areas (banks) formed from glacial deposits.
  • Physical aspects: cold, nutrient-rich water from the Labrador Current, tidal currents, upwelling.
  • Biological aspects: sand lance are a food source for whales, and other organisms in the region
  • Iron fertilization hypothesis: increasing atmospheric CO2 during glacial periods is a result of iron limitation in HNLC (high-nutrient, low-chlorophyll) areas overcome by atmospheric dust.

Lecture 29

  • Prof. Buston's lecture covered coral reef biodiversity
  • Importance of biodiversity for ecosystem services
  • Metapopulation ecology: a population made up of many local populations
  • Connectivity of metapopulations and management of marine reserves
  • Dispersal kernels of fish vary between species; dispersal drops off rapidly over distance scales, which suggests that widely separated marine reserves may not be interconnected.

Lecture 30

  • Mid-ocean ridge hydrothermal vents and their associated communities.
  • Vents are exits from hydrothermal circulation.
  • Hot, chemical-rich water (H2S, metals) mixes with cold ocean water supporting chemosynthesis-based ecosystems.
  • Chemosynthesis: energy from chemical reactions (H2S and O2) to create organic matter
  • Vent communities are transient, and whale carcasses might serve as temporary habitats for moving to new locations.

Lecture 31

  • Coastal ocean and coral reefs
  • Pelagic (water column) vs. benthic (seafloor) organisms and processes.
  • Oceanic, neritic, and littoral provinces.
  • Coastlines have high levels of life.
  • Coastal diversity depends on light, nutrients, temperature, tides, salinity, etc., like coral reefs, seagrass meadows, kelp forests, beaches, tidal flats, mangroves, marshes, etc.

Lecture 32

  • Coastal Biogeochemistry
  • [Data regarding coastal processes/variables]

Lecture 33

  • Sea level

Lecture 34

  • Climate change and mitigation.

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Prepare for EE 144 Exam #4 with a comprehensive review covering lectures 26-34. This quiz will help you solidify your understanding of marine productivity factors, nutrient limitations, and the Redfield Ratio. Get ready for multiple-choice and diagram interpretation questions!

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