I. Zones and distributions
A. Physical factors
1. Changes in water levels
– seasonal; some unpredictable
2. Changes in temperature
– changes oxygen capacity
a. Small streams; unshaded streams
b. Stratification rare except in pools.
3. Oxygen
4. Chemistry – determined
by catchment:
“In every respect, the valley rules the stream” (Hynes 1975)
5. Light – if stream has
canopy or is turbid, low light may limit primary production in the
stream
itself
6. Flow
a. Advantages
1. respiration
2. filter feeding
3. transportation (if organisms can control it)
4. chemical communication – water flow increases chemical movements –
prey
can detect upstream predators
b.
Disadvantages –
1. can dislodge organisms
2. shearing action of flowing water transports and deposits material,
continually
changing the physical environment
B. Riparian zone – normally above water
line;
may be inundated during floods
1. Allochthonous inputs
– inputs to the system from outside – DOM, leaves, etc.
2. Water and nutrient inputs
Chemical transformation -- e.g.,
NH4+ to NO3-
adsorption of nutrients
C. Shore zone – often bare; colonization
difficult
– water level often fluctuates
D. Water column
1. Potamoplankton
– river plankton; usually algae
2. ‘tychoplankton’
– don’t belong there but are washed in
3. drift – mostly aquatic
insects – organisms being carried downstream; may include zooplankton
in
large rivers
4. fish
E. Benthos - – attached or free-living on bottom
1. Aufwuchs –
fungi,
algae, bacteria, protozoans and some organisms feeding on them
a. Epipelic
b. Epilithic
c. Epiphytic
2. rooted plants
3. animals: aquatic insects,
mollusks, fish
F. Hyporheic – “below current”
II. Adaptations
A. Algae
1. firmly attached to hard
substrates
2. motile
3. body form
a. flattened – trying to remain in boundary layer where there is little
current
b. trailing filaments – increase exposure to nutrients
B. Higher plants (angiosperms, liverworts, mosses)
1. attached to rocks
2. rooted in substrate –
tough yet flexible stems
C. Potamoplankton
1. River size – there are
more potamoplankton as go downstream, with increased size of stream and
often get decreased velocity spots
(pools)
2. No special adaptations
3. Seasonal changes due
to export from nearby quieter waters
D. Benthic Invertebrates – most adaptations, wide phylogenetic
diversity
1. Diversity
a. Mollusca (Gastropoda,
Bivalvia);
b. Turbellaria
(flatworms)
c. Crustacea (crayfish, amphipods, isopods),
d. Oligochaetes, Hirudinea
(leeches)
e. Acari (water mites), Porifera
(sponges)
f. Cnidaria
(hydra)
g. Nematoda (roundworms)
h. Major orders of stream insects
a. Plecoptera
-
stone
flies; mostly in temperate regions; rare in tropics; cool, clean
streams
of low orders;
sensitive to low oxygen; tolerant of low pH; adults are poor fliers
b. Trichoptera
-
caddis flies; worldwide distribution; both free-living case-building
species
c. Ephemeroptera
– mayflies; world-wide distribution; gills for respiration; sensitive
to
low pH; adult lifespan short and do not feed
as
adults.
d. Odonata
-
dragonflies
and damselflies; occur worldwide predators; stalk their prey; can eat
vertebrates
as well
e. Diptera
(true
flies)- midges(Chironomidae - nonbiting midges); black flies
(Simuliidae)
f. Coleoptera
(beetles)
aquatic beetles tend to live in water both as larvae and as adults
2. Morphology
a. Flattened and streamlined - decrease resistance to flow; but is also
an adaptation for living under rocks
b. Suckers and hooks - allows to grasp rocks; hooks (tarsal claws)
c. Tubes -- Chironomid larvae, sticky silk, attached to rock
d. Ballast - help them to remain on bottom
3. Behavioral responses
to
stream flow
a. Current avoidance
b. Drift (both a noun and a verb)
mostly at night
c. There is also some movement upstream, but this is relatively slow
d. Why drift?
1) Proximate cause (cues) - light
2) Ultimate or adaptive cause
a) None - Accidental -
e.
Compensation for drift -- why aren't all the insects in the
ocean?
Why are there any left in the streams?
(1) Colonization cycle – upstream flight
Adults fly upstream; not tested until recently
-Arctic stream insects were labeled with 15NH4+
by introducing it into the stream
-Collected adults upstream later in season when emerging
-Any insects above the 15NH4+
emergence
point with 15N had to have come from downstream
Average distance of flight upstream ~2 km
Average distance of downstream drift ~2 km
Therefore upstream flight of adults can
compensate for drift
(2) Excess production hypothesis
Even if many drift, there are still a lot left
Better success of eggs deposited upstream – less competition
Difficult to assess because it is difficult to measure upstream
production
and combine these
measurements with downstream movement
III. Stream ecosystem ecology
A. Feeding – functional group concept
– ‘guilds’
1. shredders -
biters
and chewers; take large food and produce small foods;
herbivorous or detritivorous (leaves and microfauna)
2. scrapers - feed
on aufwuchs (on substrates); specialized mouth parts to scrape material
on substrates
3. collectors - spin
nets or use setae to collect organic matter; feed on fine particulate
organic
matter;
filter with nets, hairs; cephalic fans (black flies)
4. predators -
carnivorous;
swallow prey whole or bite pieces or suck out contents
B. detrital material - much of the food web in a
stream is detrital; this detritus is broken up into categories by size
1. CPOM - coarse particulate
organic matter; >1 mm; leaves, wood, litter
2. FPOM - fine particulate
organic matter; 50 mm-1mm
3. DOM - <~0.45 mm
C. How do the guilds fit together?

D. River continuum concept (Vannote et al.
1980)
- Streams change as you
go from the headwaters to the high order rivers
1. predictable physical features and gradients

-Why P<R at 1st order? --
4. criticisms -
i. oversimplified;
ii. mostly holds for pristine rivers
iii. relates only to macroinvertebrates
iv. if low order streams are devoid of forest then they aren't shaded
and
don't have high CPOM loads
E. Resource spiraling concept (Newbold et
al. 1982)
1. closed system (no inputs
or outputs; have rate and pathways)
2. open system (inputs,
outputs; rates, pathways, residence time)
3. open system with
spiraling
(downstream transport)
a. rate
b. pathway
c. residence time
d. downhill transport 'spiral length' :
Important for looking at distubances and the responses to disturbances because they propagate downstream
F. Controls on lotic community structure -- What
controls the biosystem?
1. density dependent
= 'biotic interactions'; function of how many organisms are around
a. competition - for space
b. predation
c. parasitism
2. density independent
= 'abiotic factors'
a. floods
b. changes in substrate
c. changes in temperature (e.g. freezing)
3. Which mechanism
dominates?
Evidence for both
a. Abiotic factors have clear influences
b. Correlational evidence -- density dependent correlations of 1
species
with another.
c. Experiments
1) Have shown clear effects of grazers feeding on periphyton
2) Manipulation of insect predators in cages have demonstrated
biotic
density dependent control
3) Manipulations of fish predators in cages -- small biotic
effects
(when you change fish abundance,
the abundance of insects doesn't change much), although big
behavioral
effects
d.
Conclusions
1) Evidence favors strong abiotic controls
2) Importance of time scale, large abiotic factors (flood/freeze) reset
the system frequently so that you don't get
enough time/high enough densities for important biotic effects in many
streams
3) In more stable conditions you get lots of biotic interactions
3) Really not settled yet
a) continuum of regulation -- Peckarsky
b) long-term records -- to see how often resetting occurs
c) density dependent effects -- often subtle; behavioral
GOOD GENERAL STREAM ECOLOGY TEXT BOOKS
(also see Riparia book reference in last handout)
Allan, J.D. 1995. Stream ecology: structure and function of running
waters. Chapman & Hall.
Cushing, C. and J.D. Allan. 2001. Streams: Their Ecology and Life.
Academic Press.
Giller and Malmqvist. 1998. The biology of streams and rivers. Oxford
University Press.