Week 11: Classifying organisms, productivity and rocky intertidal communities Flashcards

1
Q

Plankton

A

DRIFTERS
- surface
-most of earth’s biomass

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2
Q

Nekton

A

SWIMMERS
-can move around all throughout water

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3
Q

Benthos

A

BOTTOM DWELLERS
-touching bottom

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4
Q

Phytoplankton

A

Autotrophic- produce own food via photosynthesis (primary producers)

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5
Q

Zooplankton

A

Heterotrophic- cant produce own food

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6
Q

Plankton- classification

A

Life cycle
1. Holoplankton: organisms that spend entire life as plankton
2. Meroplankton: organisms that spend their juvenile or larval stages as plankton, then mature (ex squid)

Size
1. Picoplankton
2. Macroplankton

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7
Q

Benthos- Classification

A
  • Epifaunal- on sediment
  • Infaunal- in sediment
  • Nekobenthos- swimming just above ocean bottom
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8
Q

Benthos- Life strategies

A
  • Burrowers (infaunal): wiggle into sediment
  • Epifaunal: attatch to sediment via byssal threads
  • Borers: bore into hard rock
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9
Q

Divisions of the marine environment- based on sunlight

A

Photic zone
Aphotic zone (no sunlight)*below 600m

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10
Q

Photic zone

A
  1. Euphotic zone: bulk of biological productivity in the ocean; sunlight for photosynthesis (70m)
  2. Disphotic: not enough sunlight for photosynthesis (600 m)
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11
Q

Divisions of the marine environment - pelagic zones

A
  1. Epipelagic (200m)
  2. Mesopelagic (1000m)
  3. Bathypelagic (4000m)
  4. Abyssopelagic (6000m)
  5. Hadopelagic
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12
Q

Epipelagic

A

Light present
High O2

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13
Q

Mesopelagic

A

Twilight zone - little light
Low O2 levels

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14
Q

Bathylpelagic and abyssopelagic

A

Dark, create own light via bioluminescence
High pressure
Live on detritus (remains of organisms)

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15
Q

Divisions of the marine environment- Benthic environment

A

Intertidal
Sublittoral
Bathyal

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16
Q

Primary productivity

A

Rate at which organisms store energy through the formation of organic matter (carbon-based compounds) from inorganic carbon
*Biomass formation

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17
Q

Measuring primary productivity

A

gC/m2/yr

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18
Q

What effects primary productivity?

A
  1. Solar radiation
  2. Nutrient availability
  3. Water temp
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19
Q

Solar radiation and productivity

A

Light reaches 1000m deep but not enough for photosynthesis, has to be euphotic zone
- more nutrients, light doesn’t travel as deep
- less nutrients, light travels deep

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20
Q

Limiting factor

A

A biotic or abiotic factor that restricts number or production of an organism

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21
Q

Red light and phytoplanktons

A

Phytoplankton absorb red light wavelengths which doesn’t extend far into the ocean so they stay at surface
Limiting factors bc it keeps primary productivity at surface

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22
Q

Gross and net primary productivity

A

Gross primary productivity= total amount of organic material created by producers
Net production ( gross productivity -respiration)

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23
Q

Compensation depth for photosynthesis

A

Gross photosynthesis is balanced by respiration
Water depth at which light is limited so that net photosynthesis =zero
- amount used= amount produced

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24
Q

Nutrient availability- phosphorus

A

Phytoplankton cant reproduce without it

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25
Q

Nutrient availability- nitrogen

A

Needed for nitrogen fixation
Supports photosynthesis, aquatic plant growth and protein synthesis

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26
Q

Nutrient availability -nitrate

A

Increased abundance w depth bc of upwelling
Brings deep water nutrients to surface

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27
Q

Nutrients- Redfield ratio

A

Nutrient concentrations in tissue of phytoplankton
106 carbon: 16 nitrogen: 1 phosphorus

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28
Q

Why are conditions optimal with 16:1 ration of N:P

A

Organic processes tend to control proportions of these elements in the water
ex. denitrification and nitrogen fixation by diazotrophs

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29
Q

Nutrient availability- Limiting factor

A

Can be too much or too little of nutrients (ex. N, P, Fe)

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30
Q

Eutrophication

A

Excessive loading of water w nutrients
ex. N and P

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31
Q

Effects of eutrophication

A

Increased biomass production
Increased O2 consumption and O2depletion
Algal blooms lead to hypoxic conditions and creates dead zones

32
Q

Impacts of eutrophication

A

Food security
Ecosystem health
Disruptions in tourism
Fisheries and health industries

33
Q

Iron (Fe)

A

Essential micronutrient; controls phytoplankton productivity

34
Q

Iron limitation

A

HNLC
High nutrient, low chlorophyll areas but bioavailable Fe is scarce

35
Q

Why is iron low in seawater?

A

Limiting nutrient
High reactivity of Fe2+ w O, so less Fe2+
Low solubility of Fe3+

36
Q

Sources of Fe

A

Hydrothermal activity releases Fe to be upwelled
Dust

37
Q

Carbon dioxide removal (CDR) technique

A

Artificially add Fe to the ocean’s surface to stimulate growth of phytoplankton which capture CO2

38
Q

Will CDR work?

A

Wont be able to make enough phytoplankton
Over oxygenation creating dead zones

39
Q

Direction of energy flow in marine ecosystems

A

Unidirectional

40
Q

Producers

A

Autotrophic

41
Q

Consumers

A

Heterotrophic; herbivores, carnivores, omnivores

42
Q

Decomposers

A

Break down organic compounds

43
Q

Energy flow in marine ecosystems

A

Energy transferred up to higher trophic levels
Primary producer- primary consumer- secondary consumer- tertiary consumer

44
Q

Microscopic algae- Phytoplankton

A

Autotrophic- create glucose through photosynthesis
Occupy the euphotic zone
90-96% of surface ocean’s carbohydrate

45
Q

What are the types of Phytoplankton- microscopic algae

A

Coccolithophores
Diatoms
Dinoflagellates

46
Q

Coccolithophores

A

Moderate to low nutrient conditions
Tend to live in waters that are brightly lit, warm

47
Q

Phytoplankton blooms

A

Exponential growth, reproduce asexually
Seasonal (bloom in spring and fall) and depend on latitude (higher)
Factors:
- Favourable winds and currents
- Overfeeding
- High water conditions

48
Q

Dinoflagellates

A

Flagella: allow organism to adjust its orientation and vertical position in the water to obtain best light and nutrients
-Bioluminescent
- explosive growth causes red tides and harmful algal blooms

49
Q

Where are phytoplankton?

A

Phytoplankton distribution corresponds to nutrient distribution in the water (upwelling areas)

50
Q

Phytoplankton- Marine cyanobacteria

A

Smallest known photosynthesizers (Prochlorococcus)
Nutrient poor water (oligotrophic)

51
Q

Macroscopic algae (seaweed)

A

Unicellular/ multicellular algae (not plants)
- photosynthesize
- diverse shape and size
- non-vascular
-dont grow below euphotic zone, can thrive in shallow water

52
Q

Limiting factors of algae

A

Temp
Nutrient supply
Substrate
Light

53
Q

Green seaweed- Chlorophyta

A

Intertidal, shallow water

54
Q

Red seaweed- Rhodophyta

A

Most abundant
Widely distributed
Attached to substrate or encrusting

55
Q

Brown seaweed- Phaeophyta

A

ex. rock weed and kelp

56
Q

Marine angiosperms

A

Plants that reproduce w flowers and seeds
Sea grasses and mangroves
Autotrophic, vascular plants (hydrophytes, macrophytes)

57
Q

Mangroves

A

Trees that grow in water
Grow in intertidal zone
Lower latitudes (dont like cold)
Can expel salt
**kelp and mangroves never in same place

58
Q

Chemosynthesis

A

Conversion of one or more C-containing molecules into organic matter
Oxidation of inorganic compounds as a source of energy
No light -aphotic zone

59
Q

Who performs chemosynthesis?

A

Deep ocean or hydrothermal vent communities
ex. gutless giant tube worms have symbiotic relationship w bacteria
ex. yeti crabs

60
Q

Intertidal community

A

Area above water at low tide and underwater at high tide

61
Q

Who lives in the intertidal community?

A

Invertebrates (benthic)- The molluscs
Gastropods, bivalves, cephalopods

62
Q

Molluscs- gastropods (snails)

A

Periwinkles
Limpets
Dog whelks

63
Q

Arthropods

A

Lobster, crabs, shrimp, barnacles

64
Q

Arthropods - Barnacles

A

Cementers
Sessile suspension feeders (use cirri)
Stalkless- acorn barnacles
Stalked- goose barnacles

65
Q

Types of barnacles

A

Semibalanus (light colour)- lower intertidal, long life, high mortality
Chthamalus (dark colour)- upper intertidal, fast growing, short life)

66
Q

Competition of barnacles

A

“Competitive dominance”
Semibalanus outcompetes chthamalus by crowding or smothering
Chthamalus occupy higher tide levels resistant to dessication

67
Q

Echinoderms

A

Sea stars and urchins

68
Q

Cniadaria

A

Sea anemones

69
Q

Difficulties of rocky intertidal communities

A
  • Rapid temp changes
  • Dessication
  • Salinity changes
  • Moving substrate
  • Wave shock
  • Exposure to marine and terrestrial predators
70
Q

Ways to combat dessication

A

Hide in low lying area
Clam up to preserve moisture
Protect body by covering w shells
Lose an arm (starfish)

71
Q

Ways to combat wave shock

A

Well anchored
Find shelter
Wedge in cracks

72
Q

How do sea anemones combat wave shock?

A

Can adjust height based on wave action
ex. shorter in high wave activity

73
Q

Why live in rocky intertidal communities?

A

Abundant food
Many nutrients
Abundant dissolved gases
Numerous places to live

74
Q

Biotic community

A

Assemblage of organisms that live together within some definable area or habitat

75
Q

Ecosystem

A

Biotic plus abiotic community- organisms exchange energy