Deep Sea Ecosystems Flashcards

1
Q

Oceanic Depth Zones

A

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

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2
Q

Components of deep-sea topography (4)

A

Abyssal plain: largest ecosystem on earth, deep basins between continental margins and mid-ocean ridges

Seamounts

Mid-ocean ridge

Trenches

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3
Q

Factors affecting deep-sea life (6)

A

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

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4
Q

Food sources in the deep sea (3)

A

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)

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5
Q

What does the amount of POM reaching deep-sea depend on? (3)

A

The density of organisms (spring bloom vs summer)
Level of primary production
Bacterial activity in the water column

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6
Q

Adaptions to low food availability

A

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

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7
Q

Feeding Modes in the deep-sea(5)

A

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

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8
Q

Larvacean Mucous Nets

A

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)

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9
Q

Sinkers

A
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
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10
Q

Effects of limited food on abyssal ecology (

A

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

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11
Q

Goals of ceDAMar (4)

A

Describe biodiversity in the abyss on a global scale
Describe new species
Investigate what regulates diversity
Collect baseline data for climate change

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12
Q

CeDAMar major findings ()

A

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

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13
Q

Threats to deep-sea

A

Polymetallic nodule mining and other forms of resource extraction
Climate change

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14
Q

Effects of mining (3)

A

Chemical effects: toxicity and plume effects

Physical effects: habitat destruction

Major regulation challenges

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15
Q

Climate change and the deep sea

A

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

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