Environmental Engineering Reference
In-Depth Information
Table 2.7 Diatom Succession in Algal Biofilms.
Species
Growth Form
Growth Dynamics
Light Adaptation
Early colonisers (phase I)
Attached diatoms
High irradiance species
High G max and I s values
Gomphonema angustatum
Short chains of cells
Settlement from high
population level in water
column
Meridion circulare
Attached rosettes
Fast immigration due to rapid
reproduction after
attachment
Surirella ovata
Single cells or pairs
Fast immigration due to rapid
attachment
Mid-successional species
(phase II)
Attached diatoms
Low irradiance species
Low G max and I s values
Cymbella sp. Gomphonema
olivaceum
Vertical growth via long
mucilaginous stalks
High growth rate maintained
in dense algal conditions
Late-successional species
(phase III)
Unattached, tangled
diatoms
Low irradiance species
Moderate G max and very
low I s values
Fragilaria vaucheriae
Unicellular
High growth rate
Aulacoseira varians
Chain forming
maintained in dense algal
Cocconeis placentula
Prostrate
conditions
The transition from early colonising diatoms to mid- and late successional species is related to growth form, growth dynamics and light
adaptation (see text). Light adaptation parameters: G max - estimated maximum growth rate; I s - estimated light intensity at half G max .
of grazing by invertebrates) are also a key deter-
minant. The sequence shown in Fig. 2.24 gives an
indication of general trend (from pioneer commu-
nity to mature periphyton) and may terminate as a
mature community at any point in the succession,
depending on conditions. The intermediate biofilm
community varies considerably, ranging from a
mucilaginous biofilm (typically rich in bacteria, but
containing algae) to a non-mucilaginous community
composed largely of attached algae - particularly
diatoms. In conditions which promote active algal
growth, the sequence may thus progress from pioneer
to periphyton community, with little development of
a mucilaginous biofilm.
Factors affecting community development can be
studied under controlled laboratory conditions. Gain-
swain et al . (2006), for example, looked at the influ-
ence of substrate particle size - fine material (
biofilm development and phosphorus release in a lab-
oratory fluvarium. Progression to periphyton (sub-
stantial filamentous mass) only occurred with gravel
and stone substrate - the fine material was not suffi-
ciently stable to support attached filamentous algae.
2.9 Algal biofilms
Biofilms are monolayer communities of microorgan-
isms occurring at a physical interface, which in fresh-
water systems includes water/air boundaries (neuston
biofilm at the water surface) and substratum/water
boundaries - such as the surfaces of fine sediments,
rocks and plants. Microalgae are important con-
stituents of biofilms, both in the developing biofilm
and in the mature community. This may remain at
an early stage of development, such as the diatom
biofilm on estuarine sediments (Sutherland et al. ,
<
2
mm), gravel (2-20 mm) and stones (
>
20 mm) - on
 
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