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The Intertidal,Part 2 and Meiofauna

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Swash and ... Swash is gentle. Wave energy consumed by the surf. Reflective - wave ... Backwash and swash collide to deposit sediments. Dissipative and ... – PowerPoint PPT presentation

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Title: The Intertidal,Part 2 and Meiofauna


1
The Intertidal,Part 2and Meiofauna
  • Lecture 12
  • Marine Biology

2
Intertidal Sandy Shores
The most important factor is wave action Beaches
are defined by swash and backwash Swash - water
running up the beach (builds beaches) Backwash -
water running down the beaches (removes
beaches
3
Swash and Backwash
4
Beaches, cont.
  • High wave action/strong waves leads to steep
    beaches with coarse particulate size.
  • Low wave action leads to gentle sloping,
    fine-grained beaches
  • Wave induced substrate movement - particles are
    picked up and redeposited. They are moved and
    sorted.
  • Heavy wave action results in smaller particles
    which remain in suspension and are carried from
    the beach.
  • Light wave action results in smaller depth of
    sediment being disturbed.

5
Beach Types
Beach types Dissipative - strong wave action
and surf with fine sediments. Beach is flat and
maximally eroded. Swash is gentle. Wave energy
consumed by the surf. Reflective - wave action
is minimal. Sediment is coarse. No surf zone.
Large swash. Steep slope. Backwash and swash
collide to deposit sediments.
6
Dissipative and Reflective Beaches
7
Beaches, cont.
Abundance and diversity of macrofaunal organisms
are strongly correlated with particulate size and
slope. High abundance occurs in very exposed,
coarse-grained sediments with steep slopes versus
fine sand beaches, flatter slopes where wave
action is dissipated in surf rather than on the
beach. Thus, very exposed beaches can support
rich megafauna if it is a dissipative beach and
not reflective. Higher biomass of filter-feeders
correlated with dissipative conditions.
8
Beaches, cont.
Seasonal changes are often dramatic. Few
organisms can permanently occupy surfaces on sand
or gravel beaches. This leads to a barren
appearance. Oxygen content can become limiting
in substrate. The finer the substrate, the higher
the potential for anoxic conditions to occur with
fewer organisms able to persist in these low
oxygen zones.
9
Adaptations
Deep rapid burrowing (avoids dislodgement) Smooth
shells reduce surface resistance to facilitate
burrowing.Heavy shells anchor in the
substrate. No plants or sessile organisms in this
habitat.Annelids, crustaceans, and mollusks
dominate the infaunal diversity either as
suspension or filter feeders. Differences in
temperate and tropical communities exist with
respect to faunal composition
10
Adaptations
Tube-building by worms and other invertebrates
combat sediment instability. Saturation of oxygen
in blood pigments occurs at very low oxygen
tensions (hemoglobin, hemerythrin occur as blood
pigments in many species) Glycogen stores -
function to provide energy under anaerobic
conditions (enable aerobic metabolism)
11
Tide Pool Organisms
12
Tidepool
13
Fine and Coarse Grained Organisms
14
Beach Types
15
Intertidal Sand Organisms - Clams
16
Organism Distribution in Sand
17
New England Sand Community
18
Sand Community Zonation
19
Muddy Shores (mudflats)
Think of a muddy shore as a very protected
shore. - very fine sediments, rich in organics
(characteristic of
estuaries, salt marshes,
and mangroves) Habitat is completely
protected from wave action and found in proximity
to sources of very fine sediments such as
rivers.Anaerobic conditions prevail - The
transition between aerobic and anaerobic layers
referred to as redox potential discontinuity
layer (rpd).
20
Muddy Shores, cont.
A rapid change in redox potential occurs within
the first few mms of the sediment surface, going
from ---gt - Below the rpd, a decomposition of
organic matter is by anerobic bacteria
(chemolithotrophic bacteria) This zone is
identified by transition from brown to grey to
black
21
Muddy Shores, cont.
Why is this important? Reduced compounds
diffuse upwards where oxygen occurs and bacteria
oxidize compounds such as CO2, NO3, and SO4 -
these are important chemicals for starting the
base of the food chain. In the anaerobic zone,
bacteria reduce compounds and release phosphate.
This is crucial for new plant growth. In fact,
plant growth usually begins directly above the
hypoxic zone.
22
New England Mudflat Community
23
Intertidal Fish
24
Intertidal Fish
25
Intertidal Birds
26
Intertidal Interactions
27
Meiofauna
28
Meiofauna, cont.
29
Meiofauna, cont.
30
Benthic Meiofaunal Food Web
31
Meiofaunal Types
32
Meiofauna Images
33
Distribution of Meiofauna in Sediments
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