Marine Zoology & Ecosystems: Marine properties

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74 Terms

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Physiography definition

shape of sea floor- large & small scales features

spatial arrangement of those features: how they're connected/ laid out

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Physiography is controlled by

broad geological process

geochemical make up of crust & mantle + heat flow= plate tectonics

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Seafloor physiography: First order

underpinning control

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Seafloor physiography: Second order

seawater properties and oceanographic processes & substrate properties

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Seafloor physiography: Third order

biological interactions

effects of competition, predation, bioturbation, reef building

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How does geology control physiography:

Earth crust= geochemically different between continent & ocean

creates different densities

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Continental shelf sea:

much shallower than ocean

continent that happens to be flooded due to high sea levels

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Reasonable approximation of crust & mantle

Crust= solid, brittle

mantle= viscous fluid

Crust floats on mantle

lighter continental crust floats higher than denser ocean crust

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What creates strikingly broad ridges that occur on ocean floor:

results from heat flow from deep in mantel

take form or large-scale convection cells

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Where does new oceanic crust originate?

In areas of high mantle heat flow.

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Why does the seafloor bulge near mid-ocean ridges?

Because the underlying mantle is warm, causing the crust to expand and rise

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What is the rate/type of magma input at mid-ocean ridges?

Relatively slow and steady input of magma.

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Where is the youngest and warmest oceanic crust found?

At the mid-ocean ridge.

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Where is the oldest and coldest oceanic crust found?

Adjacent to the continents.

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How does water depth change with crustal age?

Water depth increases as crust ages because the crust cools, contracts, and becomes denser.

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What major seafloor feature is created by hot, buoyant crust at spreading centres?

Ocean ridges

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What hydrothermal activity is common at ridges?

Episodic hydrothermal vents.

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What covers older seafloor away from the ridge?

Slowly accumulating fine sediment.

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What broad, flat seafloor regions are formed by sediment covering old crust?

Abyssal plains.

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Subduction:

when subduction occurs between two oceanic plates, string of volcanic islands (island arc) form

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Ocean-ocean subduction:

gives rise to deepest ocean trenches

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Shallow water hydrothermal environments:

occur on submarine flanks of volcanoes

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Shelf sea example: North Sea

can be very shallow, considering area

mean water depth 38m

Seafloor slopes are shallow- steepest along line= 0.4% (2m height change over 500m)

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Shelf sea Example: Skagerrak

500m deep channel

Many seafloor habitats in higher temp latitudes are result of global processes

most recent reached peak around 20,000 yrs ago

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Shelf Seas:

Shallow but often spatially highly variable & dynamic:

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Transition from shelf sea to ocean:

Stark & intricate

Main ocean basins- fundamentally different in terms of depth

Nature of transition between shelf sea (Celtic) and deep ocean (abyssal plain)

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Ocean ridges:

Large scale features

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Ocean ridges: Example transect from US-Mauritania

ridge flanks not too dissimilar to continental slops- offer a mix of rocks & sediments on sloping topography

sloping topography affects ocean dynamics (potentially transporting nutrients)

Argued= being very long & linear features, provide potential corridor of habitat

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The tide: What are intertidal zones?

Coastal areas that are alternately exposed and submerged due to tidal cycles.

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The Tide: Why do intertidal zones host diverse communities?

Organisms are specially adapted to repeated wet-dry cycles.

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The tide: What types of habitats occur along intertidal coastlines?

Soft-sediment habitats and rocky shores.

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The Tide: What coastal environments are strongly influenced by tides in temperate regions?

Estuaries, saltmarshes, and tidal flats.

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The tide: Why are flooding and draining important for estuaries and saltmarshes?

They maintain physical structure and ecological balance.

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The Tide: How do tidal currents affect larvae?

Strong currents disperse larvae.

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The tide: What is the "flushing effect" of tides?

Removal of waste products, pollutants, and excess nutrients.

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The tide: When do shorebirds typically feed in tidal environments?

At low tide.

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The tide: How do fish and crabs use the tides?

They move in with the rising tide to feed in newly flooded areas.

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The tide: How are spawning and larval release timed in many marine organisms?

They are synchronized with tidal cycles.

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Spring-Neap Tidal cycle: What causes tides on Earth?

The combined gravitational effects of the Moon and the Sun.

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Spring-Neap Tidal cycle: Which body has the stronger effect on tides, the Moon or the Sun?

The Moon.

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Spring-Neap Tidal cycle: Why does the Moon have a stronger tidal effect than the Sun?

closer to earth than sun

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Spring-Neap Tidal cycle: What is the tidal period associated with the Moon

Approximately 25 hours.

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Spring-Neap Tidal cycle: What is the tidal period associated with the Sun

Approximately 24 hours.

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Spring-Neap Tidal cycle: How strong is the Sun's tidal influence compared to the Moon's

half as strong

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Tide generating force diagrams: black arrow

moon's gravitational attraction

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Tide generating force diagrams: blue arrow

Centrifugal force acting on the Earth.

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Tide generating force diagrams: Red arrow

net tide-generating force.

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How many tides does most of the Earth experience per day

2

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Semi-diurnal tide.

a tide with two highs and two lows per day

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What happens to point P on Earth during one full rotation

it passes through two tidal bulges, producing two high tides

<p>it passes through two tidal bulges, producing two high tides</p>
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What produces tidal waves in the ocean

The tide-generating force

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Why don't shelf seas directly feel the tide-generating force

They are too small relative to the scale of tidal wavelengths

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How does tidal motion appear in shelf seas

Like waves travelling across the shelf, causing the ocean level to rise and fall

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Coriolis effect

The effect of Earth's rotation on the direction of winds and currents.

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Why does water pile up in the eastern Irish Sea

the Coriolis effect deflects moving water to the right in the Northern Hemisphere

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Why is the Coriolis effect important

strongly influences weather systems and ocean circulation

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How fast is Earth's surface moving at the equator

1670 km/h

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Why don't we feel Earth's rotation in everyday life

the land, atmosphere, and oceans move together

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How fast is Earth's surface moving near the North Pole

655 km/h

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In which direction does the Coriolis effect deflect motion in the Northern Hemisphere

To the right

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Which direction do tidal currents flow?

north

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Kelvin Waves

wave like this that is strongly controlled by Coriolis & is bounded by coast

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How does tidal range change in embayments

Increases with embayments

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Funnel-shaped embayments

produces largest tidal ranges

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How does the funnel shape affect tidal range

concentrates tidal energy, increasing tidal height toward the head of the embayment

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What role does side-friction play in embayments

slows tidal flow and contributes to the buildup of water, enhancing tidal range

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What additional effect can increase tidal range in some gulfs

Resonance between the basin shape and the tidal period

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Which well-known location shows strong tidal resonance

The Gulf of Maine

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Why are sea floor sediments important

fundamental control on marine habitats

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How are seafloor sediments typically classified

grain size

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What grain size measures are commonly used to label sediments

Mean or median grain size

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Why does grain size matter for benthic organisms

influences burrowing ability, stability, oxygenation, and food availability

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Wentworth Scale

the classification of sediments by size; a boulder is the largest grain size and clay is the smallest grain size in this classification system

<p>the classification of sediments by size; a boulder is the largest grain size and clay is the smallest grain size in this classification system</p>
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Folk scale

captures little of range of sizes present