Quiz 9 Flashcards
(58 cards)
What is a nutrient loading model? (3)
A model that shows the max amount of nutrients that can be added to a lake without it becoming eutrophic given certain parameters (eg. Mean depth, residence time)
Lakes and reservoirs have a critical nutrient loading rate beyond which they become eutrophic
The objective is to stay in the “meso-oligotrophic” range
What are the main components that determine a lake’s productivity? (4)
Edaphic influence
Geographic influence
Morphometric influence
Human influence
history of fisheries biologists and predicting fish yield (5)
1927 - thienemann proposed that oligotrophic lakes were > 18m and eutrophic lakes were < 18m
1939 - Rawson produced chart showing inter-related factors affecting lake productivity
During WWII, the Canadian government asked Rawson to develop a method to predict sustainable fisheries production
He used mean depth to develop hyperbolic curves for variation in zooplankton, zoobenthos, and fish for various lakes in North America
Then after 1950, it was found that TDS actually have a larger effect than depth and models were created to take both into account, as well as residence time
What was discovered in the 1950s pertaining to plankton and fish production? (5)
Significant increases in plankton, bottom fauna, and fish quantities occurred with increases in total dissolved solids content (nutrients)
There was a significant difference demonstrated between summer epilimnion temperature and plankton
It was found that total dissolved solids were even more of a determinant of production than depth
However, depth and total dissolved solids could not be used alone or together to predict productivity within a region
Therefore, Dick Ryder came up with the Morphoedaphic Index to distinguish between regions
What is the generalization for the relationship between mean depth and production of plankton, bottom fauna, and fish?
Amount of fauna from lakes of great mean depth are never as high as those found in SOME lakes of low mean depth
Morphoedaphic Index (4)
Dick Ryder thought about using both parameters, TDS and mean depth, and combined them into an index expressed in log 10 units to compare regions
A very simple equation to predict fish yield:
MEI = total dissolved solids/mean depth
Yield increases from polar to tropical regions
Assumptions of the Morphometric Index (3)
Relationship between mean depth of lakes and various hydrologic characteristics (flushing rate and stratification regime)
water transparency characteristics (water colour and turbidity)
and the stoichiometric relationship among ions (expressed as a proportion between TDS and the concentration of primary nutrients, total phosphorus, and total nitrogen)
What happened to the predictive power of the MEI with increasing tropic levels? (2)
It became progressively weakened, even though these basic assumptions could be supported empirically
MEI could account for 85% of the variation in TP and TN, 50% of the variation in chlorophyll a, but none of the variation in biomass of herbivorous zooplankton (higher on the food chain)
Vollenweider’s first loading model (4)
Richard Vollenweider developed the critical loading rate theory and equations for lakes, based on the analysis of numerous lakes in Europe and North America
First model only used mean depth to determine critical P and N loading
Determined lake tolerance to P loading depending on size and depth
Was imperfect but useful for establishing permissible and dangerous loading levels of P and N
What is the general tolerance of lakes to P loading according to Vollenweider’s first model (2)
In general lakes can tolerate higher P loading rates as they increase with size and depth due to dilution
This is described as a higher flushing rate, so nutrients are diluted or flushed out = less effect of nutrient loading
Vollenweider’s second model (3)
Included water residence time, putting the flushing rate into the equation
This is a better model to use
Lp=P*z(1+sqrt(Tw))/Tw
Where: Lp=critical annual P load (mg P/m2/yr) P=spring overturn phosphorus concentration (mg P/m3) Tw=water residence time (yr) z=mean depth (m)
What are the 9 major phytoplankton groups?
Cyanobacteria Green algae Yellow-green algae Golden-brown algae Diatoms Cryptomonads Dinoflagellates Euglenoids Brown and red algae
What are phytoplankton? (4)
Complex mix of algae and Cyanobacteria that are floating in standing water and slow moving rivers
Almost all phytoplankton species are obligate photoautotrophs
Some are mixotrophic
Some are heterotrophic
What is Cyanobacteria? (4)
True bacteria with simple prokaryotic cell structure
Reproduce by binary fission
Have chlorophyll a so can photosynthesize
Are structured like bacteria but function like an aquatic plant (no chloroplast or mitochondria)
Green algae (3)
Large and morphologically diverse group
Many members are flagellated
Can reproduce asexually and sexually
Yellow-green algae (2)
Unicellular, colonial, or filamentous
Characterized by carotenoids instead of chlorophylls which is why they’re yellow-green
Golden-brown algae (2)
Most are unicellular, some are colonial, but they are rarely filamentous
B carotene is dominant in addition to chlorophyll so they show a golden brown colour
Diatoms (4)
Very important group - the Bacillariophyceae
Primary characteristic is their silicified cell walls
Two types: Centric Diatoms which have radial symmetry
And Pennate Diatoms which have bilateral symmetry
Cryptomonads (2)
Unicellular and motile (single celled and capable of motion)
Have a variety of pigments, hence they can appear green, blue, red, or brown
Dinoflagellates (3)
Unicellular flagellates algae which are motile (single celled and mobile)
Reproduce sexually and asexually
Large body size (400um) which makes them relatively inedible to most grazing zooplankton
Eulenoids (4)
Large and diverse group
Few species are planktonic
Almost all are unicellular
They lack a distinct cell wall and have 2-3 flagella
Brown and red algae (4)
Brown algae are filamentous or thalloid
Most are marine, can be planktonic but not in freshwater
All attach to substrate
Red algae is rare in freshwater, none are planktonic, and if in freshwater are restricted to fast flowing streams of well-oxygenated cool water
Algae as nutrition (5)
Algae are a variety of sizes
Some are too small or too large to be eaten or are undesirable
The very middle size category (nanoplankton) are preferred for optimizing carbon flow to higher trophic levels (2.0-20.0um)
Cyanobacteria are inedible, non-nutritious, and or toxic
They also have a mucilaginous coating that protects them from being digested during passage through Daphnia
Algae that are too small (2)
Picoplankton are undesirable as they are too small for larger zooplankton to consume (0.2 to 2.0um)
They expend much of their energy in metabolism and less carbon is available to transfer up to food web