Deep Sea Ecosystems Flashcards
Oceanic Depth Zones
Euphotic (day-light zone): up too 200m
Twilight/Disphotic Zone: Mesopelagic zone (200-1000m), detectable light to 1000m but no photosynthesis
Midnight/Aphotic Zone: Devoid of light
Seafloor: Average depth of 3800m
Components of deep-sea topography (4)
Abyssal plain: largest ecosystem on earth, deep basins between continental margins and mid-ocean ridges
Seamounts
Mid-ocean ridge
Trenches
Factors affecting deep-sea life (6)
Light: no light below 1000m, animals of the deep sea exist in total darkness
Temperature is uniformly low and salinity is high
Oxygen is non-limiting except in specific areas
Predominantly soft-sediment habitat
Pressure is extremely high: increases by 1 atm per meter (average deep-sea pressure is 380 atm)
Food supply is low and unpredictable
Food sources in the deep sea (3)
Particulate Organic Matter (POM) is generated by primary production at the surface
Chemosynthesis: sulphur based (hydrothermal vents) and hydrocarbons (methane creeps)
Food falls (carcasses): short term or long term (whale fall communities)
What does the amount of POM reaching deep-sea depend on? (3)
The density of organisms (spring bloom vs summer)
Level of primary production
Bacterial activity in the water column
Adaptions to low food availability
Conserve Energy: Watery muscles, fatty tissues, weak skeletons, no scales, poorly developed respiratory, circulatory and nervous systems, no vertical migration behaviour
Enormous/expandable mouths to swallow a variety of large prey
Expandable stomachs to hold large prey items
Feeding Modes in the deep-sea(5)
Deposit Feeding: dominant method due to soft sediments
Suspension Feeding: less common due to food paucity
Sporadic but found in areas with abundant suspended particles
Mucous Nets: larvaceans
Predation: fish, tunicates
Scavenging
Larvacean Mucous Nets
Giant Larvacean: feeds with large mucous nets, harness food in the deep sea, absorbs a wide range of organic matter down to colloidal material, clog in 1-2 days and discarded (sinkers)
Sinkers
Important input of carbon to deep-sea High in carbon Contribute to the organic content of seafloor Sink quickly (800m a day) Con occur in substantial numbers
Effects of limited food on abyssal ecology (
Reduced faunal densities
Deep-sea food supply cannot sustain large numbers
Compared to the epipelagic zone: 5-10 times fewer organisms in the mesopelagic zone and 50-100 times fewer organisms in the deep-sea
Size of deep fauna
Mesopelagic and deep-sea organisms are generally smaller compared to organisms of the epipelagic zone
Gigantism can occur
Goals of ceDAMar (4)
Describe biodiversity in the abyss on a global scale
Describe new species
Investigate what regulates diversity
Collect baseline data for climate change
CeDAMar major findings ()
Extreme is normal: wide range of organisms thrive, business as usual
Rare is common: nearly all abyssal species are rare, no one species dominates, density is low but biodiversity is higher than expected, lots of unique species found in the deep sea
Threats to deep-sea
Polymetallic nodule mining and other forms of resource extraction
Climate change
Effects of mining (3)
Chemical effects: toxicity and plume effects
Physical effects: habitat destruction
Major regulation challenges
Climate change and the deep sea
As primary production decreases at the surface the productive layer decreases and there is weaker upwelling.
The supply of carbon to the deep-sea will decrease