sandy beaches Flashcards

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1
Q

location

A

all over the earth

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2
Q

tide

A

intertidal

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3
Q

substrate

A

sand: Sediment particles have a diameter of 0.02 – 2 mm

Fine sand can retain water, but coarse sand allows water to
drain away

Not much detritus is retained in sand

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4
Q

source of sand

A

depends on the location
rocks on land and/or
calcium carbonate (CaCO3) skeletons of animals and coralline algae, including parrotfish poop

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5
Q

phys char: slope

A

variable over the seasons and varies with location

wave action

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6
Q

phys char: energy

A

moderate to high

Higher energy beaches have a steeper slope and larger sediment particles

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7
Q

DYNAMIC EQUILIBRIUM OF

SANDY SHORES

A

Beach shape & slope fluctuate about an equilibrium (which also
changes with time, but much more slowly)
Forces of erosion and deposition reach a dynamic equilibrium
Waves, tides, currents, and wind erode and transport sand

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8
Q

beach equilibrium profile for storm beaches

A
  • typical of winter and after storms
  • erosional
  • coarser erosion sediment
  • steeper slopes
  • large, high berms
  • narrow back shores
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9
Q

beach equilibrium profile for swell beaches

A
  • typical of fair-weather conditions
  • depositional
  • finer-grained sediment
  • gentler slopes
  • small, lower berms
  • broad back shores
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10
Q

light

A

absorbed or reflected by the surface layer of sand, so no light in sediment below surface but with some transparent particles and spaces between particles light penetrates deeper than in mud

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11
Q

temperature

A

within sand is quite stable
Just like mud, sand is a good buffer against temperature (and
salinity) changes
Below the first few centimeters, the temperature in the sand is the same as the surrounding seawater

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12
Q

salinity

A

within sand is also quite stable

Below the first 10-15 centimeters, the salinity in
the sand is the same as the surrounding seawater

Even with precipitation & run-off, the more dense
saltwater will sink below freshwater

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13
Q

nutrients

A

little to no nutrients in the sand as
nutrients move through with water and are used
quickly

BUT, waves do bring algae to beach

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14
Q

oxygen

A

lots due to high wave action / energy especially at high tide May be reduced in interstitial water at low tide as oxygen is
consumed by organisms
Fine-grained beaches do not allow oxygen to enter as quickly and therefore may become hypoxic at low tide

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15
Q

hydrogen sulphide

A

– little to none

Except at low tide in fine-grained beaches

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16
Q

biodiversity

A

low (except meiofauna)

few organisms are adapted to high energy shifting of sand particles

17
Q

productivity

A

low (there are benthic diatoms in first few

millimeters of sand but producers get shifted around so much and nutrients are low)

18
Q

biomass

A

low to moderate

19
Q

meiofauna

A

Interstitial organisms (spaces between particles)

Size: 62 um to 0.5 mm

Benthic invertebrates (animals from many phyla)

20
Q

importance of meiofauna

A

decomposition

nutrient cycling

food for many consumers at higher trophic levels

very sensitive to anthropogenic pollution, making them excellent
indicators

21
Q

adaptations

A

Living among the shifting sands is the primary challenge here
– particles are always in motion

Burrowing is rapid & powerful (razor clam)

22
Q

bio adaptations

A

camouflage

  • Most organisms depend on waves to bring food & nutrients
    e. g. mole crabs, sand dollars

Wrack line very rich in nutrients
Beach hoppers / amphipods

23
Q

zonation

A

Just like in the rocky intertidal, there is a pattern of zonation
due to tides at sandy beaches

24
Q

ECOSYSTEM SERVICES PROVIDED BY

SANDY BEACHES

A

sediment storage and transport;

wave dissipation and associated buffering against extreme weather events;

dynamic response to sea level rise;

breakdown of organic materials and pollutants;

water filtration;

nutrient mineralization and recycling;

storage of water in dune aquifers and groundwater discharge through
beaches;

maintenance of biodiversity and genetic resources;

providing a nursery area for juvenile fishes (e.g. sand lance, grunion);

nesting sites or rookeries for turtles, shorebirds, and pinnipeds;

prey for birds and other terrestrial wildlife;

scenic vistas and recreational opportunities;

functional links between terrestrial and marine environments

25
Q

human impacts

A

Disturbance of species & sand

Beach grooming

Pollution, especially plastic!

Resource exploitation

Clams, crabs for food

Shrimps, worms for bait

Seaweed as compost

Shells & other treasures

Coastal development

Invasive / alien / introduced species

European green crab, Carcinus maenus

Climate change / sea level rise (erosion)

26
Q

what’s the equilibrium beach profile?

A

Equilibrium beach profile (EBP) explains the balance between destructive and constructive forces acting on a beach.

27
Q

what’s equilibrium?

A

The slope of the floor of a sea, ocean, or lake, taken in a vertical plane, when deposition of sediment is balanced by erosion.