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Coastal Ecosystems

      Dr. Mark A. McGinley
Honors College and Department of
       Biological Sciences
      Texas Tech University
Two Main Coastal Environments
• Estuarine
  – Freshwater and sea water meet
     • Temperate- salt marshes
     • tropics- mangroves
  – Intertidal zone
     • Mudflats
     • Sandy beaches
     • Rocky intertidal
Intertidal Zones
• Dominated by gradients in two physical
  conditions
  – Wave exposure
  – Tidal exposure
Wave Exposure
• Energy in waves can
  influence
  – Particle size
  – Ability of organisms
    to remain attached
    to substrate
Tidal Exposure Gradient
• Vertical gradient
  – Higher areas have longer exposure to air than
    lower areas
• Exposure to air can have two negative effects
  for marine organisms
  – Desiccation
     • water loss
  – Thermal stress
     • Getting two hot
A Bit of Basic Geology
               Particle Size
                                                    Aggregate name
                    Size range      Size range
         scale                                        (Wentworth        Other names
                     (metric)    (approx. inches)
                                                         Class)

−8 <             256 mm <        10.1 in <          Boulder
−6 to −8         64–256 mm       2.5–10.1 in        Cobble
                                                    Very
−5 to −6         32–64 mm        1.26–2.5 in                           Pebble
                                                    coarse grave;l
−4 to −5         16–32 mm        0.63–1.26 in       Coarse gravel      Pebble
−3 to −4         8–16 mm         0.31–0.63 in       Medium gravel      Pebble
−2 to −3         4–8 mm          0.157–0.31 in      Fine gravel        Pebble
−1 to −2         2–4 mm          0.079–0.157 in     Very fine gravel   Granule

0 to −1          1–2 mm          0.039–0.079 in     Very coarse sand

1 to 0           ½–1 mm          0.020–0.039 in     Coarse sand
2 to 1           ¼–½ mm          0.010–0.020 in     Medium sand

3 to 2           125–250 µm      0.0049–0.010 in    Fine sand

                                 0.0025–0.0049
4 to 3           62.5–125 µm                        Very fine sand
                                 in

                 3.90625–        0.00015–0.0025
8 to 4                                              Silt               Mud
                 62.5 µm         in
>8               < 3.90625 µm    < 0.00015 in       Clay               Mud
> 10             < 1 µm          < 0.000039 in      Colloid            Mud
Wave Energy and Shore Particle Size
• Larger particles require more energy to move
  them than smaller particles
• Thus, the size of particles on the shore is
  influenced by the energy in the waves striking
  the shore
• High energy shores contain larger particles
  than low energy shores
Rocky Shore
Boulder Beach
Cobble Beach
Gravel Beach
Sandy Beach
Mud Beach
Rocky Shore
• Rocky intertidal zone dominated by daily rise
  and fall of tides
  – Littoral zone
     • Part of the time covered by water and part of the day
       exposed to air
• Species living in littoral zone must face the
  problems with living in both marine and
  terrestrial habitats
Rocky Shore- Physical Environment
• Two dominant gradients in physical conditions
  – 1) Wave exposure
  – 2) Tidal exposure
     • Vertical gradient
        – Higher areas spend more time exposed to air than lower areas

• Exposure to air can have two negative effects
  – Desiccation
  – Thermal stress
Intertidal Zonation
Zonation in Rocky Intertidal
Intertidal Zone Organisms
What Causes These Zonation Patterns?
• The field of ecology is interested in
  understanding the factors that influence the
  distribution and abundance of organisms
• Determined by abiotic and biotic factors
Rocky Intertidal Zone
• Rocky intertidal zones proved to be ideal
  natural labs for studying ecology
  – Steep vertical gradients
  – Variable physical conditions
  – Mostly sessile or sedentary organisms
  – Small organisms with high density
  – Easily manipulated
Joe Connell’s Experiments With
          Barnacles
Connell’s Experiments With Barnacles
• What causes pattern of zonation?
  – Physical factors or biotic interactions
• Physical Factors
  – Higher regions exposed to air for longer periods
     • Thus greater desiccation
  – Lower regions exposed to air for shorter period of
    times
Question
• Can the barnacles tolerate the environmental
  conditions outside of the zone where they are
  found?
  – Too dry higher up and too wet lower down???
Question
• Is the distribution of the barnacles influenced
  by biotic interactions?
  – Competition, predation


• Could they live higher and lower on the shore
  in the absence of other species?
Manipulative Experiments
• Connell (and others scientists including Bob
  Paine who also worked in rocky intertidal
  ecosystems) recognized the importance of
  manipulative experiments in the field.

• Helped move ecology from a descriptive
  science to an experimental science
Need to Design an Experiment
• What experiments would you suggest to try to
  determine the importance of abiotic and
  biotic factors on the distribution of these
  barnacles?

• What factors can limit distribution?
  – Never got there
  – Can’t live there because of abiotic conditions
  – Can’t live there because of biotic interactions
Questions
• As we talked about in lab, you need to start by
  asking a question.

• Let’s start by thinking about the cause of the
  boundary between Balanus and Chthamalus
  – Q. 1. Is Balanus missing form the upper zone
    because it has never reached there?
Experiment
• Place Balanus in the Chthamalus zone and see
  if it can survive. Make sure that there are no
  potential competitors or predators affecting
  them
  – Control- move Balanus to the Balanus zone

  – These barnacles are attached to the rocks, so
    Connell was able to move the organisms around
    by chipping off pieces of the rock and attaching
    them elsewhere on the rocks
Results
• Balanus did not survive in the higher zone

• Conclude- Balanus not living in the upper zone
  because they can not deal with the abiotic
  conditions.
  – Hypothesis- too dry in the upper zone
  – What experiment could we do to test this?
Questions

• Q. 2. Is Chthamalus lacking from the lower
  zone because it has never dispersed there?

• Experiment- move Chthamalus to the Balanus
  zone with no potential competitors or
  predators
Results

• Chthamalus was able to grow in the lower
  zone
  – Thus, not limited by lack of dispersal or by abiotic
    conditions

  – Hypothesis- Chthamalus limited by competition
    for space by Balanus
     • Test by moving Chthamalus to the lower level and
       allowing it to interact with Balanus
Results

• Chthamalus could not live in the lower zone
  when Balanus was there
  – Competitively excluded by Balanus
Rocky Intertidal
• Patterns
  – Biomass and species richness increase closer to
    the sea
Tide Pools
• Pools of water may
  become isolated and
  hold water for periods
  ranging from hours to
  several days
• When pools isolated
   – Water evaporates
   – Salinity increases
   – Temperature increases
• Pools can fill during rains
   – Salinity decreases
   – Temperatures decrease
Mangroves
• Mangroves include a number of tropical trees
  and shrubs that are able to live in the
  intertidal zone along tropical coastlines.
• Have adaptations to allow them to live in
  periodically flooded regions with high salt
  content.
• Approximately 70 species of mangrove plants
  come from 20 different plant families
Problems Facing Mangroves
• The soil is very fine and water logged, it is difficult
  for the root system to support the plant.
• Because the roots zone is waterlogged, plant
  roots are unable to pick up the oxygen they need
  through the soil.
• Because they are living in the intertidal zone
  mangrove plants have to be able to live in water
  with high salt concentrations.
• No oxygen in the saturated soil.
Mangroves
Aerial Roots and Pneumatophores
Mangroves- Cool Fish
Importance of Mangrove Ecosystems
• serve as nurseries for a number of marine fish
  and invertebrates.
  – juveniles of many species hide out among the
    mangrove roots until they are large enough to move
    out to the reef.
• Second, the mangrove roots protects the shore
  from the effects of storms and tsunamis.
  – It has been well documented that parts of SE Asia
    that were protected by mangroves were much less
    negatively affected by the big tsunami than those
    regions where the mangroves have been removed.
Mangrove Restoration
     Thailand

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Coastal Ecosystems

  • 1. Coastal Ecosystems Dr. Mark A. McGinley Honors College and Department of Biological Sciences Texas Tech University
  • 2. Two Main Coastal Environments • Estuarine – Freshwater and sea water meet • Temperate- salt marshes • tropics- mangroves – Intertidal zone • Mudflats • Sandy beaches • Rocky intertidal
  • 3. Intertidal Zones • Dominated by gradients in two physical conditions – Wave exposure – Tidal exposure
  • 4. Wave Exposure • Energy in waves can influence – Particle size – Ability of organisms to remain attached to substrate
  • 5. Tidal Exposure Gradient • Vertical gradient – Higher areas have longer exposure to air than lower areas • Exposure to air can have two negative effects for marine organisms – Desiccation • water loss – Thermal stress • Getting two hot
  • 6. A Bit of Basic Geology Particle Size Aggregate name Size range Size range scale (Wentworth Other names (metric) (approx. inches) Class) −8 < 256 mm < 10.1 in < Boulder −6 to −8 64–256 mm 2.5–10.1 in Cobble Very −5 to −6 32–64 mm 1.26–2.5 in Pebble coarse grave;l −4 to −5 16–32 mm 0.63–1.26 in Coarse gravel Pebble −3 to −4 8–16 mm 0.31–0.63 in Medium gravel Pebble −2 to −3 4–8 mm 0.157–0.31 in Fine gravel Pebble −1 to −2 2–4 mm 0.079–0.157 in Very fine gravel Granule 0 to −1 1–2 mm 0.039–0.079 in Very coarse sand 1 to 0 ½–1 mm 0.020–0.039 in Coarse sand 2 to 1 ¼–½ mm 0.010–0.020 in Medium sand 3 to 2 125–250 µm 0.0049–0.010 in Fine sand 0.0025–0.0049 4 to 3 62.5–125 µm Very fine sand in 3.90625– 0.00015–0.0025 8 to 4 Silt Mud 62.5 µm in >8 < 3.90625 µm < 0.00015 in Clay Mud > 10 < 1 µm < 0.000039 in Colloid Mud
  • 7. Wave Energy and Shore Particle Size • Larger particles require more energy to move them than smaller particles • Thus, the size of particles on the shore is influenced by the energy in the waves striking the shore • High energy shores contain larger particles than low energy shores
  • 14. Rocky Shore • Rocky intertidal zone dominated by daily rise and fall of tides – Littoral zone • Part of the time covered by water and part of the day exposed to air • Species living in littoral zone must face the problems with living in both marine and terrestrial habitats
  • 15. Rocky Shore- Physical Environment • Two dominant gradients in physical conditions – 1) Wave exposure – 2) Tidal exposure • Vertical gradient – Higher areas spend more time exposed to air than lower areas • Exposure to air can have two negative effects – Desiccation – Thermal stress
  • 17. Zonation in Rocky Intertidal
  • 19. What Causes These Zonation Patterns? • The field of ecology is interested in understanding the factors that influence the distribution and abundance of organisms • Determined by abiotic and biotic factors
  • 20. Rocky Intertidal Zone • Rocky intertidal zones proved to be ideal natural labs for studying ecology – Steep vertical gradients – Variable physical conditions – Mostly sessile or sedentary organisms – Small organisms with high density – Easily manipulated
  • 21. Joe Connell’s Experiments With Barnacles
  • 22. Connell’s Experiments With Barnacles • What causes pattern of zonation? – Physical factors or biotic interactions • Physical Factors – Higher regions exposed to air for longer periods • Thus greater desiccation – Lower regions exposed to air for shorter period of times
  • 23. Question • Can the barnacles tolerate the environmental conditions outside of the zone where they are found? – Too dry higher up and too wet lower down???
  • 24. Question • Is the distribution of the barnacles influenced by biotic interactions? – Competition, predation • Could they live higher and lower on the shore in the absence of other species?
  • 25. Manipulative Experiments • Connell (and others scientists including Bob Paine who also worked in rocky intertidal ecosystems) recognized the importance of manipulative experiments in the field. • Helped move ecology from a descriptive science to an experimental science
  • 26. Need to Design an Experiment • What experiments would you suggest to try to determine the importance of abiotic and biotic factors on the distribution of these barnacles? • What factors can limit distribution? – Never got there – Can’t live there because of abiotic conditions – Can’t live there because of biotic interactions
  • 27. Questions • As we talked about in lab, you need to start by asking a question. • Let’s start by thinking about the cause of the boundary between Balanus and Chthamalus – Q. 1. Is Balanus missing form the upper zone because it has never reached there?
  • 28. Experiment • Place Balanus in the Chthamalus zone and see if it can survive. Make sure that there are no potential competitors or predators affecting them – Control- move Balanus to the Balanus zone – These barnacles are attached to the rocks, so Connell was able to move the organisms around by chipping off pieces of the rock and attaching them elsewhere on the rocks
  • 29. Results • Balanus did not survive in the higher zone • Conclude- Balanus not living in the upper zone because they can not deal with the abiotic conditions. – Hypothesis- too dry in the upper zone – What experiment could we do to test this?
  • 30. Questions • Q. 2. Is Chthamalus lacking from the lower zone because it has never dispersed there? • Experiment- move Chthamalus to the Balanus zone with no potential competitors or predators
  • 31. Results • Chthamalus was able to grow in the lower zone – Thus, not limited by lack of dispersal or by abiotic conditions – Hypothesis- Chthamalus limited by competition for space by Balanus • Test by moving Chthamalus to the lower level and allowing it to interact with Balanus
  • 32. Results • Chthamalus could not live in the lower zone when Balanus was there – Competitively excluded by Balanus
  • 33. Rocky Intertidal • Patterns – Biomass and species richness increase closer to the sea
  • 34. Tide Pools • Pools of water may become isolated and hold water for periods ranging from hours to several days • When pools isolated – Water evaporates – Salinity increases – Temperature increases • Pools can fill during rains – Salinity decreases – Temperatures decrease
  • 35. Mangroves • Mangroves include a number of tropical trees and shrubs that are able to live in the intertidal zone along tropical coastlines. • Have adaptations to allow them to live in periodically flooded regions with high salt content. • Approximately 70 species of mangrove plants come from 20 different plant families
  • 36. Problems Facing Mangroves • The soil is very fine and water logged, it is difficult for the root system to support the plant. • Because the roots zone is waterlogged, plant roots are unable to pick up the oxygen they need through the soil. • Because they are living in the intertidal zone mangrove plants have to be able to live in water with high salt concentrations. • No oxygen in the saturated soil.
  • 38. Aerial Roots and Pneumatophores
  • 40. Importance of Mangrove Ecosystems • serve as nurseries for a number of marine fish and invertebrates. – juveniles of many species hide out among the mangrove roots until they are large enough to move out to the reef. • Second, the mangrove roots protects the shore from the effects of storms and tsunamis. – It has been well documented that parts of SE Asia that were protected by mangroves were much less negatively affected by the big tsunami than those regions where the mangroves have been removed.
  • 41.