Midterm 3 Flashcards
Aquatic Communities - 2 types
7 and 1
Marine: intertidal, sub-tidal kelp beds, continental shelf, open ocean, deep ocean, coral reefs and arctic/antartic
Freshwater lakes
Vertical Zonation
This is the phenomenon associated with the different strata.
Generally, narrow bands that species live within strata
Sub-tidal Kelp Bed Communities
Highest primary productivity of all communities on the planet
Provides physical protection to shoreline communities
Foraging and shelter for a large number of species
These are stratified habitats
Zonation of Pelagic Zone (5)
Epipelagic (0-200m) Mesopelagic (200-1000m) Bathypelagic (1000-4000m) Hadal (4000-6000m) Benthic - seafloor
Coral Reefs
Tropical waters have very little phytoplankton so coral reefs with zooxanthellae symbionts provide the basis of the trophic pyramid
Greatest species diversity on the planet
Highly efficient recycling of nutrients
Arctic (6)
mainly frozen ocean surrounded by land
4000m water depth, 3m ice cover
upper 15m reduced salinity from large rivers
A complex layering of Atlantic and Pacific waters
High abundance of plankton in summer, arctic cod, seals, beluga, narwhal, bowhead whale
The polar bear is a terrestrial predator
Antarctic (6)
Large frozen continent surrounded by the ocean 98% ice cover up to 2 km in thickness
Mountainous 4500m elevation
Low species diversity - bacteria, lichen penguins
Surrounding very cold oceans with high primary productivity and species diversity
Weddell seal, leopard seal, elephant seal, penguins, Orca, humpback
No terrestrial predator
Lake Classification (4)
Oligotrophic - clear water lakes (low productivity)
Dystrophic - stained (tea-coloured) lakes (low productivity), very acidic
Mesotrophic - intermediate productivity
Eutrophic - high productivity lakes
Lake Stratification Summer
Wind causes mixing within Epilimnion
Separating layer (thermocline)
With cold water below (hypolimnion)
Lake Stratification Fall and Spring
Constant mixing of the whole water column
Due to max density of water at night in fall causes it to fall and mix
In spring ice melt sinks and mixes
Lake Stratification WInter
Frozen top with an upper oxygen environment
And an oxygen sparse dead zone at the bottom
Due to decomposition occurring down there
Tundra
3-6 months of darkness with ice/snow Permafrost Cold hardy plants Surface soil thaws in summer 3 Strata -- Soil, ground, low shrubs Many aquatic/terrestrial insects Shorebirds, waterfowl (seasonal migrants) Hare, fox, wolves, caribou, grizzly bear, polar bear High productivity during spring/summer
Temperate Coniferous Forests (Taiga/boreal forest)
Conifers Few shrubs The ground layer of ferns and mosses Trees with monopodial growth 4 strata -- trees, shrubs, ground, soil Short summers and long cold winters (slow decomposition) Seasonal migrants Occasional hibernation/torpor for residents
Temperate Rainforest
Ancient trees
4 Strata with high 3D structural complexity
Multiple species of fungi, mosses, angiosperms
High insect diversity
Species-rich riparian zones
1000 yr for seral stage recovery, after clear cut
Greatest biomass/ha for all terrestrial ecosystems on the planet
Tropical forests
6 Strata
A - emergent trees over 60m (discontinuous)
B - up to 20m (discontinuous)
C - lowest trees (continuous canopy)
D - Shrub layer, tall ferns and herbs
E - Ground layer, herbaceous plants and seedlings
F - Root/soil layer (shallow and poorly developed)
High species diversity of most taxonomic groups
High biological turnover, high recycling of nutrients
A and F are connected by vines (many epiphytes)
Relative nitrogen levels in strata of different ecosystems
Arctic – Tundra has most (90%) in soil and Taiga has about 50% in soil
Temperate – Grassland has about 30% in soil and Deciduous forests have 40% in the soil
Tropical – Savannah and Equatorial forest have similar proportion with very little in soil (<10%)
Polar Cell
Between the arctic tundra and temperate forests
Cold dry air falls
Ferrell Cell
Between the temperate forests and the deserts
Subsidence zones, cold dry air sinks
Hadley Cell
Between equatorial forests and deserts
Hot moist air rises from the equator and forms cumulus clouds
High cool dry air moves north and south and cools more
Latitudinal Diversity Gradient
This shows that generally, species diversity increases as you move towards the equator
Diversity can also differ along with the same latitude
Ocean depth in terms of diversity
Unique in that increasing depth doesn’t seem to affect the species diversity
Very consistent across the different depths
Marine Productivity Trends
Highest productivity at the poles where the cold water is nutrient-rich
This is because water sinks at 4 degrees displacing colder water up mixing in nutrients
Desert across most of the open ocean
Decent productivity at the equator due to polar currents bringing in nutrients from the rotation of the earth
Terrestrial Productivity Trends
Most of the primary productivity on land occurs at the equator
During our summer the northern hemisphere has higher productivity and during our winter the southern hemisphere has higher productivity
Productivity is mostly controlled by a combination of temperature and rainfall
Sunlight variation from poles to the equator
They generally receive the same amount of sunlight (~ 1:1)
The difference is that the equator receives more solar energy from the direct impact of photons
Competition theory
At temperate latitude, the lower productivity causes broader niches and r-selection which don’t allow for as many species
At tropical latitudes, the higher productivity causes narrower niches and k-selected allowing for more species
Spatial heterogeneity theory
Increased spatial heterogeneity causes an increase in structural complexity and this allows for more niche segregation
This means more species
Environmental Age Theory
This predicts that the older the environment is following some kind of succession, the more species richness you expect to find
Increase species richness with environmental age
Major explanations for differences in species richness (4)
Primary productivity
Competition
Spatial heterogeneity
Environmental Age
Hypotheses on biodiversity, complexity and stability (3)
Diversity-stability hypothesis (Charles Elton)
The linear increase in stability as # of species increases (tropics)
Rivet Hypothesis (Paul and Anne Erhlich) The exponential increase in stability as species increase slows down as # of species gets large
Redundancy Hypothesis (Brian Walker)
Flatline of stability increases at large species numbers, a sharp decrease in stability if keystone species is lost
(Intertidal communities)
Island species numbers compared to mainland
There are disproportional fewer species numbers on islands for their area size
The slope of species numbers from the area is much lower on islands (this slope is independent of distance from the mainland)
What causes the cyclicity and high turnover of islands?
The lack of predators (predation) allows species to go above carrying capacity and then crash
This causes the cyclicity that allows for a high turnover rate
A small population of a species are prone to extinction
Essential features of Equilibrium Theory (3)
The number of species moves towards an equilibrium between extinction and colonization as a function of island area and distance
At equilibrium, actual species composition is in a continuous state of change as some species go extinct and new species colonize (high turnover as species equilibrium is reached)
Can predict numbers of species but not the species composition
What occurs after the defaunation of small islands
The small islands that were closest to the mainland has the best and fastest recovery
They also noticed that the species that persist on the islands after tend to be the species that originally occupied that island
Becuase those species had specific attributes for that niche space
Where does speciation occur on a 3D biogeographical process map?
The highest levels of speciation occur on isolated islands of a large area.
This helps to increase species richness on very isolated islands