Week 11: Classifying organisms, productivity and rocky intertidal communities Flashcards
Plankton
DRIFTERS
- surface
-most of earth’s biomass
Nekton
SWIMMERS
-can move around all throughout water
Benthos
BOTTOM DWELLERS
-touching bottom
Phytoplankton
Autotrophic- produce own food via photosynthesis (primary producers)
Zooplankton
Heterotrophic- cant produce own food
Plankton- classification
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
Benthos- Classification
- Epifaunal- on sediment
- Infaunal- in sediment
- Nekobenthos- swimming just above ocean bottom
Benthos- Life strategies
- Burrowers (infaunal): wiggle into sediment
- Epifaunal: attatch to sediment via byssal threads
- Borers: bore into hard rock
Divisions of the marine environment- based on sunlight
Photic zone
Aphotic zone (no sunlight)*below 600m
Photic zone
- Euphotic zone: bulk of biological productivity in the ocean; sunlight for photosynthesis (70m)
- Disphotic: not enough sunlight for photosynthesis (600 m)
Divisions of the marine environment - pelagic zones
- Epipelagic (200m)
- Mesopelagic (1000m)
- Bathypelagic (4000m)
- Abyssopelagic (6000m)
- Hadopelagic
Epipelagic
Light present
High O2
Mesopelagic
Twilight zone - little light
Low O2 levels
Bathylpelagic and abyssopelagic
Dark, create own light via bioluminescence
High pressure
Live on detritus (remains of organisms)
Divisions of the marine environment- Benthic environment
Intertidal
Sublittoral
Bathyal
Primary productivity
Rate at which organisms store energy through the formation of organic matter (carbon-based compounds) from inorganic carbon
*Biomass formation
Measuring primary productivity
gC/m2/yr
What effects primary productivity?
- Solar radiation
- Nutrient availability
- Water temp
Solar radiation and productivity
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
Limiting factor
A biotic or abiotic factor that restricts number or production of an organism
Red light and phytoplanktons
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
Gross and net primary productivity
Gross primary productivity= total amount of organic material created by producers
Net production ( gross productivity -respiration)
Compensation depth for photosynthesis
Gross photosynthesis is balanced by respiration
Water depth at which light is limited so that net photosynthesis =zero
- amount used= amount produced
Nutrient availability- phosphorus
Phytoplankton cant reproduce without it
Nutrient availability- nitrogen
Needed for nitrogen fixation
Supports photosynthesis, aquatic plant growth and protein synthesis
Nutrient availability -nitrate
Increased abundance w depth bc of upwelling
Brings deep water nutrients to surface
Nutrients- Redfield ratio
Nutrient concentrations in tissue of phytoplankton
106 carbon: 16 nitrogen: 1 phosphorus
Why are conditions optimal with 16:1 ration of N:P
Organic processes tend to control proportions of these elements in the water
ex. denitrification and nitrogen fixation by diazotrophs
Nutrient availability- Limiting factor
Can be too much or too little of nutrients (ex. N, P, Fe)
Eutrophication
Excessive loading of water w nutrients
ex. N and P