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general categories of aquatic habitats
lentic- systems in which water doesn’t move or moves slowly, lakes & ponds
wetlands- habitats where soil is saturated with water (at least temporarily)
lotic- systems in which water flows, creeks, streams & rivers
characterizations of streams
watershed size
stream order
discharge
flow regime
vegetation
lotic systems: rivers & streams
dynamic systems:
the shape of a river is constantly changing
rivers respond to the land it traverses
i.e. catchment area
catchment/ watershed/ basin
defined as a region that drains into lake, pond, or river
catchments vary by:
size
soil type/ bedrock
vegetation present
differences impact:
nutrients
pH
water color
large catchments= larger impact on chemistry
classification of streams
based on order
1st, no streams flowing into it
2nd, two 1st order streams joining
3rd, two 2nd order streams joining
3rd order stream cannot be formed by 2nd + 1st
headwater streams are orders 1-3
mid-sized rivers are 4-6
large rivers are orders 7-12
~85% of streams in the US are 1-3
low order streams
headwater streams
shaded
coarse particulate organic matter provides resource base for consumer comunity
allochthionous inputs
originating or formed somewhere other than the place where it is currently found
functional feeding groups
shredder= coarse particulate organic material, e.g. leaf litter or wood
grazer/ scraper= algae and associated material
collectors= fine particulate organic material from stream bottom or water column
predators= feed on other consumers
mid-order streams
energy inputs change as stream broadens
light
CMOP
fine POM (FPOM)
sunlight supports significant periphyton production
shredders are replaced by grazers
collectors are still abundant
predator abundance about the same
high order streams
energy sources continue to change
light
FPOM dominated
primarily autochthonous inputs
as streams widen the flow decreases
turbid
bottom substrate becomes finer
phytoplankton & zooplankton become prevalent
primarily collectors and predators
river continuum concept
headwater streams (1-3)
most organic material allochthonous
respiration > production
lots of shredders & collectors
midreach streams (4-6)
increasing autochthonous organic material
respiration < production
lots of collectors & grazers
lower reach streams (>6)
large flux of organic material- water becomes more turbid
respiration > production
lots of collectors
water discharge & velocity
discharge is volume per unit time
velocity is how fast water is going (distance per unit time)
discharge is not velocity
flow can mean discharge or velocity
hydrographs are a plot of discharge over time
human influences
damming, channelization and excessive water use
reservoirs allow sediments to settle ad make rivers downstream ‘sediment starved’
dams fragment riparian habitat
alteration of temperature regimes
restoration of rivers
goal: restoration of natural hydrology and ecosystem functions
reintroduction of natural riparian vegetation
creation of macrohabitats (logs, pools, etc)
improvement of water quality
monitoring to assess restoration success
dam removal
benefit: restore river connectivity
issues: release of large amounts of sediment and accumulated toxins, permitting, training
transport of material by rivers and streams
rivers carry materials dissolved from land to the sea
important part of the carbon cycle
N, P, S, & C
erosion
under base flow, riffles are erosional habitats and pools are depositional habitats (opposite during floods)
factors like presence of macrophytes can affect sediment trapping and transportation
mobile material
suspended load (fine material suspended in the water column, turbidity or total suspended solids)
bed load slides or rolls along the bottom
importance of transport of solid materials
habitat alteration
movement of rocks
movement of contaminated sediments
transport of organisms
drift: at any given time a small number of macroinverts may be suspended
catastrophic drift can accidentally be triggered by floods or pollutants