Exam 1 Flashcards

(127 cards)

1
Q

Ecology

A

The study of the interactions between organisms and their environment

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2
Q

Organism

A

The unit of natural selection; an individual existing within an ecosystem

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3
Q

Population

A

The unit of evolution; Organisms of the same species living together in a specific area

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4
Q

Community

A

The level above population; an assemblage of populations of different species, interacting with one another

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5
Q

Ecosystem

A

The interacting parts of the biological and physical worlds

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6
Q

Biosphere

A

The planet Earth; the collection of all of our planet’s ecosystems

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7
Q

Levels of Complexity

A

Organism

Population

Community

Ecosystem

Biosphere

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8
Q

How is science a “subjective” process?

A

Our experiences and perspectives influence the “truth” that we approximate through our use of tools and measurements, leading to subjectivity.

Therefore, “good” science can minimize bias by incorporating multiple perspectives and collaborators

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9
Q

Ernst Haeckel

A

German biologist and philosopher who coined the term “oikologie” from the greek word oikos = home

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10
Q

Ellen Swallow Richards

A

An MIT Chemist who was the one to really launch the field of ecology by studying human impact on water chemistry.

Stood up at a conference and told everyone to stand witness to the birth of the field of oikologie.

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11
Q

What is the difference between basic and applied ecology?

A

Basic: Gathering knowledge for knowledge’s sake

Applied: Driven by a human need (Ex: invasive species)

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12
Q

What are the three ways to organize or think about ecology and how are they studied?

A

Taxanomic Organization: Makes it easy for ecologists to compare/study

Organization by place or function: studying organism’s niches

Organization by location: studying the habitats in which organisms live

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13
Q

What are the three different types of studies that ecologists use to conduct science?

A
  1. Observational Studies: More realism/applicability
  2. Models: Conceptual and Mathematical - can illustrate relationships best
  3. Experiments: Field and Microcosm/Mesocosm - most control over variables, micro/meso has most replication
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14
Q

How do you calculate the variance of a sample?

A

Divide the sum of squares by the degrees of freedom.

v = [Σ(xi - µ)2] / (n-1)

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15
Q

Taxonomy

A

The classification of organisms by their unique characteristics into species.

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16
Q

Habitat

A

The place or physical settings in which an organism lives

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17
Q

Niche

A

The range of conditions an organism can tolerate and the way of life it pursues

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18
Q

Scientific Method

A
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19
Q

What properties of water make it beneficial for life?

A

It is dense and viscous

Stays liquid over broad range of temperatures

Unique densities at various temperatures

Good solvent

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20
Q

What aspects of water affect habitat types?

A

Availability

Salinity

Temperature

Flow speed

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21
Q

What three materials make up the different types of soils and how does their composition affect the soil?

A

Soil is made up of differing proportions of:

Sand

Silt

Clay

Their differing proportions change soil’s ability to

Hold water

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22
Q

Describe the seasonal process of mixing in temperate lakes.

A

Summer: Lake stratified, warmest at top, coldest at bottom. 28-8-4

Fall: Mixing, even temperature throughout. 4-4-4

Winter: Ice cover - density curve makes warmer at bottom. 0-3-4

Spring: Mixing again, even temp throughout. 4-4-4

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23
Q

How do freshwater fish deal with osmotic gradients?

A

Freshwater causes freshwater fish to lose salts and gain water.

They counter this by excreting excess water via urine, kidneys retain ions in blood, and absorbing salts/ions in their gills.

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24
Q

How do marine fish deal with osmotic gradients?

A

Saltwater causes marine fish to lose water and have excess solutes.

They counter this by increasing solute excretion through gills and kidneys, while drinking excess water.

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25
How do plants get water from their roots to the tips of their shoots?
Intake at roots via osmosis Transport up xylem via cohesion-tension Exit through stomate via transpiration, which maintains the tension/negative pressure
26
What is the PAR?
Photosynthetically Active Region Refers to visible light, or the wavelengths at which plant molecules absorb light to perform photosynthesis.
27
Albedo
Reflectivity of an ecosystem Higher albedo = more reflection Snow is highest, dense forest low
28
Describe the Algific Talus slopes in "the Driftless Region" and what makes them noteworthy.
The Northern Monkshood flower and the Iowa Pleistocene Snail persist in this area that was not covered in glaciers. Winter air is drawn into vents to turn water into ice and blown out the top. Summer air blows across underground ice/cold water and brought to the slope vents like air conditioning.
29
What is a "life history tradeoff" and what are some examples?
An adaptation that gives an organism some sort of advantage in its habitat, but requires energy and comes at the cost of being able to do something else well. Examples: * C4 Photosynthesis (can close stomates due to CO2 transport to bundle-sheath cells), * CAM Photosynthesis (stomates open during night, closed during day bc of dry climates) * Homeothermy (less dependent on enviro for temp mgmt, but takes energy)
30
Which wavelengths of light are able to travel longer distances in water? What does this mean for adaptations that plants at shallower vs deeper depths might have?
Blue/Short. This means that plants at shallower depths will absorb more red/long wavelength light than plants at deeper depths, which will thrive on blue/short wavelength light.
31
What are the three types of heat transfer?
**Radiation**: emission of electromagentic energy by a warm surface **Conduction**: transfer of heat energy via contact **Convection**: transfer of heat energy by movement of liquids or gases
32
Supratidal Zone
AKA Splash zone; the area above the highest tide that is never submerged, but is often splashed by waves
33
Neritic System
The system of zones that extend to depths out to the beginning of the continental shelf. Supratidal Intertidal Subtidal
34
Oceanic System
The zones that occur beyond the continental shelf. Bathyal Abyssal Hadal/benthic
35
Benthic Zone
The lowest depths of an ocean or lake
36
Pelagic Zone
Open water zones that are not near the bottom, whether in an ocean or lake.
37
Photic Zone
Portion of a body of water that receives sunlight.
38
Aphotic Zone
Portion of a body of water that does not receive sunlight
39
Littoral Zone
The shallows; portion of an ocean that is not past the continental shelf.
40
Limnetic Zone
Portion of a body of water that is **out in the open water** or past the continental shelf
41
Homeotherm
An organism that uses energy to maintain a constant body temperature
42
Poikilotherm
An organism that allows its internal body temperature to change with the environmental temperature
43
C3 Photosynthesis
The most common method of photosynthesis Uses RUBP (Rubisco, low CO2 affinity) to make a 3-C compound in mesophyll cell. Must have its stomates open a lot, risking dessication
44
C4 Photosynthesis
Use PEP Carboxylase to make a 4-C compound that is shuttled into bundle sheath cells and converted to the normal 3-C compound. Allows plant to close stomates more often to protect from dessication.
45
Crassulacean Acid Metabolism (CAM) Photosynthesis
Discovered by Edith Bellamy Shreve Same as C4, but only open stomates during night to protect further from dessication. Best adapted to dry environments.
46
Edith Bellamy Shreve
Discovered CAM Photosynthesis plants in arid conditions.
47
Jim Brown
U. New Mexico, proposed the Metabolic theory of ecology, which states that as temperature increases, maximum growth rate decreases
48
Lauren Buckley
Using bioenergetic modeling, she has applied global climate change maps to effects seen in the energy management of organisms themselves
49
C. Hart Merriam
Developed the idea of "Life Zones" at different elevations that have distinct vegetation and water availability differences
50
What abiotic factors can limit species distributions?
Precipitation Temperature Nutrient Availability Light
51
What is the primary cause of global patterns in climate and vegetation?
Differences in solar radiation across latitudes and Hadley Cells
52
Hadley Cells
Up at the equator, out to 30° lat, down to make deserts
53
What abiotic factors cause **regional** differences in climate and vegetation?
Rain Shadow Effect Slope and Aspect Elevation Soil composition Etc.
54
What abiotic factors influence species distribution in water?
Light Water Flow Salinity Temperature Nutrients
55
What is the River Continuum Concept?
It describes the differences between streams of different widths (order 1 is narrow - order 12 is very wide) Higher order streams have higher numbers of trophic levels Lower order have allochthonous inputs Higher orders have autochthonous inputs
56
Upwelling Zones
Water zones where the Coriolis Effect and prevailing winds act on the ocean to bring cool, nutrient-rich water up on the western coasts of continents during spring and summer. They lead to very productive communities
57
Rain Shadow Effect
Moisture builds up as the prevailing winds blow towards a mountain, ending in precipitation on one side of the mountain, with dry wind dessicating the other side into a desert.
58
Adiabatic Cooling
Air cools as it rises in elevation and volume and decreases in pressure.
59
ENSO event
El Niño Southern Oscillation Event 4 yrs from El -\> La -\> El Occur every 2-10 years El Niño causes warm winter for USA
60
Charles Elton
An ENGLISH ecologist who linked organisms with physical factors Also coined the term **food web**
61
Food Web
Feeding relationships among interconnected organisms
62
A.G. Tansley
An ENGLISH scientist who coined the term **ecosystem**
63
Alfred J. Lotka
An AMERICAN scientist who linked energy transfer in an ecosystem to the 2nd Law of Thermodynamics
64
Raymond Lindeman
An AMERICAN scientist who studied uner G.E. Hutchinson and used equations to define/quantify energy in trophic levels as well as how much passes between them.
65
Eleanor Hall Lindeman
Wife of Raymond Lineman, who died at age 27. She helped him complete his graduate studies, often hauling samples into their boat while he was vomiting over the side. Raymond's PhD dissertation was rejected by journals, but resubmitted by G.E. Hutchinson and accepted.
66
Eugene P. Odum
Furthered work on quantifying ecosystem ecology. Created the "Universal Model": Boxes at any trophic level can show inputs, assimilation, and outputs to other trophic levels, etc.
67
What are three ways by which production can be quantified?
Measuring Biomass Measuring Carbon isotopes Measuring Photosynthetic rates
68
What abiotic factors limit production?
Precipitation Light Temperature Nutrients
69
How do the flux pyramids differ for energy and biomass?
Energy flux pyramids always taper UP Biomass pyramids can taper in EITHER direction
70
Production
Energy within an ecosystem
71
Ecological Efficiency Equation
NPPn/(n-1) \* 100% The % of energy transferred from one level to the next
72
Food Web
Feeding relationships among interconnected organisms
73
Gross Primary Production (GPP)
The energy that is assimilated and respired
74
Net Primary Production (NPP)
Only the energy that is assimilated
75
Trophic structure
the organization of energy levels and the way producers/consumers
76
What are the two ways which organisms can disperse?
Spatially and temporally (dormancy, hibernation)
77
How does chili peppers' hotness help them disperse?
Since birds are immune to capsacin, they become perfect high-quality dispersers for chili seeds. Mammals and walkers are not immune to the hotness of capsacin, so they are selected against.
78
What are the differences between movement, dispersal, and migration?
Movement: Org changes physical position/location Dispersal: Movement away from place of birth Migration: Seasonal movement of a complete population
79
What are some COSTS and BENEFITS of movement, dispersal, and migration?
Costs: takes lots of energy to move Less chance to mate susceptible to predation in new environment BENEFITS: can escape poor conditions, find new resources
80
Long-Distance Dispersal (LDD)
Unusually long movements when dispersing from one place to another
81
Walter Diagrams
Describe biomes using temperature, precipitation, and months of the year when the min Temp is above 0
82
Whittaker Diagrams
describe biomes by ascribing environmental variables to vegetation patterns including Temperature, precipitation, and disturbance by fire
83
**Tropical Rain Forest** Location, Climate Zone, Vetetation
Loc: Equatorial CZ: Always moist and year-round mild temps Veg: Evergreen tropical rain forest
84
**Tropical Seasonal Forest/Savanna** Location, Climate Zone, Vetetation
Loc: Tropical CZ: Summer rainy and winter dry season Veg: Seasonal forest, scrub, or savanna
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**Subtropical Desert** Location, Climate Zone, Vetetation
Loc: Subtropical (hot deserts) CZ: Highly seasonal, arid climate Veg: Desert vegetation with considerable exposed surface
86
**Woodland/Shrubland** Location, Climate Zone, Vetetation
Loc: Mediterranean CZ: Winter rainy season and summer drought Veg: Sclerophyllous (drought-adapted), frost-sensitive shrublands and woodlands
87
**Temperate Rain Forest** Location, Climate Zone, Vetetation
Loc: Warm temperate CZ: Occasional Frost, often with summer rainfall maximum Veg: Temperate evergreen forest, somewhat frost-sensitive
88
**Temperate Seasonal Forest** Location, Climate Zone, Vetetation
Loc: Nemoral CZ: Moderate climate with winter freezing Veg: Frost-resistant, deciduous, temperate forest
89
**Temperate Grassland/Desert** Location, Climate Zone, Vetetation
Loc: Continental (Cold deserts) CZ: Arid, with warm or hot summers and cold winters Veg: Grasslands and temperate deserts
90
**Boreal Forest** Location, Climate Zone, Vetetation
Loc: Boreal CZ: cold temperate with cool summers and long winters Veg: Evergreen, frost-hardy needle-leaved forest (taiga)
91
**Tundra** Location, Climate Zone, Vetetation
Loc: Polar CZ: Very short, cool summers and long, very cold winters Veg: Low, evergreen vegetation, without trees, growing over permanently frozen soils
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Large River Deltas
Nutrient rich, biodiverse, 12 on continuum Low flow Many trophic levels
93
Temperate Upland rivers
5-6 trophic levels (intermediate) Endemism Moderate Flow
94
Large Lakes
Biodiverse Both Temperate and tropical regions Endemism
95
Polar Seas
Low temps and salinity Lots of plankton when whales absent bc of high DO Upwelling brings nutrients
96
Temperate Shelfs and Seas
Some stratification Tide influence bc near coasts Relatively shallow -\> warm
97
Tropical Coral
HYPER diverse shallower water -\> warm, lots of light
98
Temperate Upwelling Zones
High nutrients, biodiversity, and endemism Lower than expected temps W Coasts only! Structurally complex and fragile
99
Tropical Upwelling Zones
Similar to Temperate (high nuts, biodiversity, and endemism) VERY diverse bc warmer by default structurally complex and fragile
100
How long are Earth's natural heating and cooling cycles?
100,000 yr long cycles 10,000 yrs of cooling 90,000 yrs of warming
101
The Carbon Cycle
102
Water Cycle
103
What are the 3 major greenhouse gases?
CO2, CH4, and N20
104
Milankovitch Cycles
Changes in Earth's heating and cooling based on changes in the Earth's tilt
105
Free Air Carbon Dioxide Enrichment (FACE)
An experiment where scientists enrich the air around plants with CO2 and see how growth changes.
106
The Nitrogen Cycle (Simplified)
107
What are the Inputs and Losses of Phosphorus in an ecosystem?
INPUTS: Weathering, Wind deposition, and Humans Losses: Organism Uptake and Particulate Erosion
108
What is a dead zone and what causes them?
It is a portion of habitat that has changed so much over a short period of time that the organisms that live there cannot survive. Especially caused by excesses of nutrients.
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Nitrification
NH3/NH4+ -\> NO3-
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Denitrification
NO3- -\> N2
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Ammonification
N2 -\> NH3/NH4+
112
What are some examples of non-symbiotic nitrogen fixation?
Lightning Cyanobacteria
113
What are the effects of eutrophication on an ecosystem?
Lower diversity Higher production Shifts in spp composition Higher consumer abundance (but lower diversity)
114
Lincoln-Peterson Index AKA mark-recapture equation
#Marked in 2nd sample / #caught in 2nd sample = caught in 1st sample / total pop size
115
What does the Lincoln-Peterson Index assume?
All indivs =ly likely to be captured N doesnt change betw sampling No marked indivs are lost
116
What is the simplest form of population growth?
EXPONENTIAL (can be continuous or discrete)
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Assumptions of Exponential Growth Model
All individuals are same age and genetics B and D are constant No E or I Habitat is perfectly uniform
118
What is the difference between exponential and geometric growth?
None really; one is continuous and one is discrete.
119
What does the Logistic Growth Model represent? Who was it "created" by?
Density-Dependent Growth Lowell Reed and Raymond Pearl
120
Fecundity
bx The # of FEMALE offspring produced per reproductive season or age interval
121
Survival
Sx Probability of surviving to the next age class S = nx+1/nx
122
Survivorship
lx Probability of a newborn surviving to age x Divide population at age x by initial population size lx = nx/no
123
Net Reproductive Rate (Ro)
Mean # of offspring that a female produces in her lifetime =Σbxlx
124
Generation Time (T)
Avg age of parents of all offspring produced by a single cohort AKA how long it takes to breed a new generation T = Σxbxlx/Σbxlx =Σbxlx/Ro
125
What is the difference between positive and negative density dependence?
Positive: growth increases with density (more mates, yay!) Negative: Crowding
126
Allee Effect
Population growth is positively density-dependent until resources start becoming scarce This is when the INFLECTION point happens
127
Ideal Free Distribution
Organisms in a habitat will distribute to various patches of resources. The patch with the highest number of resources will have the highest number of individuals.