Basisc of aquatic bioloogy Flashcards
Ecology
Scientific study of the interactions that determine the dirstributions and abundance of organisms.
Distribution and occurance that we see today are the product of previous.
Fitness
Measure of a genoytpes’s long term success
- Individuals that produce the largest number of offspring over a long period of time have the greatest fitness.
- Fitness is always a relative measure.
- Two components: reproductive potential and survival
Maximum possible fitness never achieved nature Optimization instead.
Abiotic factors
- Temperature
- Oxygen
- pH
- Ions
- Water flow in streams
- Density and surface tension
Temperature
- narrow range of T fluctuations
- Lethal limits of T are less important
- False T dependencies (e. g. warm water contains less O2)
- T very important for regulation of speed of biochemical and physiological processes
Qxygen
- Very important!
- O2 input only at surface
- Productivity and morphometry determine O2 balance and vertical distribution
- Organic poluution can lead to O2 reduction or depletion
- Vertical uneven distribution of O2 in lakes O2 deficiencies and anoxie conditions also in
streams - Groundwater and springwater are often low in O2
Adaptaions to limited or changing O2 concentrations
Adaptations have their limits. O2 deficiencies are very critical for aquatic organisms
- Whole body surface as surface area for gas exchange
- Life in water, but use atmospheric O2
- Supply air bubble attached to body
- Haemoglobin with high O2 affinity
- Diapause
- Anoxibiosis
pH
pH is in turn affected by biological processes
- Direct Effects:
Physiological damage or dysfunction - Indirect effect on water chemistry
o Dissociation of ammonium
o Calcium-carbonic acid equilibrium
o Solubility of metals
Other ions
- Hypertonic regulation is essential to avoid invasion of excess water and loss of ions
- Great energetic cost, because body membranes cannot impermeable, so active uptake and removal against the gradient
- Few species can live at boundary between salt and fresh water
- Calcium is usually the dominant cation and carbonate or bicarbonate the dominant anion in freshwater. Ecologists often relate occurrence of species to calcium concentration
- Freshwater individuals: Have to maintain ion (constantly pump) → Loss of energy
- Brackish water: Very specialised
Water flow in stream
Morphiologcal and behaviourla adapations to cope with all these challenges.
- No vertical gradients, except for light
- Water shear force
- Import and export (Never constant) → Filtering organisms
- Selective transport of sediments, thus different type of bottom depending on stream velocity
- Unidirectional drift, both dangerous and useful
Resources
- Light
- Mineral Nutrients
- Dissolved inorganic carbon
- Inorganic sources of energy
- Anerobic respiration
- Dissolved organic substances
- particulate organic substances
Light
Light is not a boundary condiytion for photosynthesis. It is a consumerable resource
DIC
Dissolved inorganic carbon
- DIC major forms:
o CO2 (aq) (aqueous carbon dioxide – dissolved gas)
o H2CO3 (carbonic acid – trace amount)
o HCO3 - (bicarbonate ion)
o CO3 -2 (carbonate ion)
Plants need CO2 (aq)
Alternative strategies when CO2 in water becomes limiting:
* Aerial leaves in macrphytos
* Use of CO2 in pore water of sediments
* Temporal decoupling of photosynthetic light reaction
* Utilizations of bicarbonate
Mineral nutrients
- Theoretically all elements could be limiting factors, but typically in freshwaters only N, P and some trace elements can become limiting.
- Redfield molar stoichiometric ratio 106C : 16N : 1P
- Approximation, very variable in inland waters
- Only dissolved forms can be uptaken by organisms
Inorganic sources of energy
Chemolithoautotrophic bacteria are extremely important for nutrient cycling in freshwater.
Anearobic respiration
- Heterotrophic bacteria use DOC as source of carbon and energy, but cannot use oxygen as a terminal electron acceptor in respiration
- Instead, oxygen-rich compounds are used to oxidize organic matter:
o nitrate NO3- → denitrification
o sulfate SO42- → desulfurication