15.2.2 Biota
Aquatic organisms are classified according to their habitats. The plankton are small free-
floating organisms. Planktonic plants, called phytoplankton, include cyanobacter, green
algae, and diatoms. Planktonic animals are zoopl ankton and include protozoans, small
crustaceans such as Daphnia species and larval forms of other animals. Organisms
such as duckweed that float on the surface are called neuston. Active swimmers that
live in the pelagic zone, such as fish, are called nekton. The community of microscopic
bacteria, fungi, and small plants and animals that live attached to submerged surfaces such
as rocks are referred to as aufwuchs. A subset of these are the periphyton, which are
algae that grow attached to surfaces. (Aufwuchs and periphyton are what makes sub-
merged rocks so slippery to step on.) All organisms that live on the bottom or within
the sediments, whether in the littoral or profundal zones, are called benthic organisms,
or simply the benthos.
Lotic ecosystems have planktonic organisms only in the slowest of rivers. Periphyton
dominate over phytoplankton, and benthos over zooplankton.
Prokaryotes Three types of autotrophic bacteria are typically found in lakes: cyanobac-
ter, chlorobacter, and chemoautotrophs. Cyanobacter (blue-green bacteria) are found in
the epilimnion. Chlorobacteria peaks just below the thermocline, their numbers decreasing
with depth. If the hypolimnion becomes anoxic, sulfate-reducing bacteria will appear to
produce hydrogen sulfide. However, most of the bacteria are heterotrophs. Heterotrophic
concentrations peak in the thermocline and near the sediment. In highly polluted streams
the filamentous bacteria Sphaerotilus can form lush gray mats waving in the current .
One of the notable roles of cyanobacter, espec ially Aphanizomenon, is in the fixation of
atmospheric nitrogen. This allows it to grow whe n nitrogen limitations apply to other
algae. Some cyanobacter, such as Oscillatoria or Microcystis, cannot fix N
2
. The latter
depends on ammonia recycled by animal or bacterial excretion or by solubilization
from the sediments. In rivers, Nostoc or Rivularia may fix considerable amounts of
nitrogen.
Gas vacuoles enable cyanobacter to float to the surface during the calm night, where
they can be found forming a scum at dawn. As the sun rises higher, the cyanobacter can be
damaged by ultraviolet radiation, so they tend to sink by midmorning. Anabaena does this
by collapsing gas vesicles by osmotic pressure which has increased as a result of glucose
formed by photosynthesis. Colonies of Microcystis and Aphanizomenon, as well as fila-
ments of Anabaena, also regulate their buoyancy by manufacturing glycogen, which is
about 1.5 times as dense as normal cell material. At night they use up the glycogen
and start to rise again. By moving up and down, the algae not only control their light
exposure but take advantage of nutrients farther below the surface.
Cyanobacter (Figure 15.5) make chemicals that inhibi t feeding by zooplankton. They
make compounds that have been known to poison cows and pigs that drank from
eutrophic sources of water. Cyanobacter and some actinomycetes also produce geosmin
and methyl isoborneol, the most common causes of taste and odor problems in drinkin g
water. These compounds are contained in the cells, but released when the cells break
down.
Green Plants Algae are plantlike protists (Figure 15.6). They are distinguished from
plants in that they do not have stems, roots, or leaves. They can be unicellular, colonial
508 ECOSYSTEMS AND APPLICATIONS