Deep Ocean
- Created by: rosieevie
- Created on: 25-05-17 17:55
Technology to Investigate Deep-Sea Ecology
Determine location on Earth surface
Measure envrionmental parameters
Recover biological samples
Observe deep sea and inhabitants directly
Milestones in Deep-Sea Ecology
1818 - John Ross finds Echinodermata phylum member on sounding line ~1400m
1872-1876 - HMS Challenger collects >4000 new species from deep ocean
1929-1934 - Beebe and Barton dive in bathysphere, observe in situ life
1960 - Piccard and Walsh reach ocean's deepest point (~10916m) in bathyscaphe Trieste
Early Notions in Deep-Sea Ecology
1843 - Forbes proposed 'azoic theory' = no life beyone 600m
- Based on dredging observations in Aegean Sea
Theory refuted by 3 expiditions - all dredged to deeper depths and collected specimens
Misconceptions about Ocean Mapping
Often repeated that only 5% Earth's oceans is mapped = NOT TRUE
All been mapped at low resolution (~5km)
Earth is dynamic - hard to create map that applies constantly
Deep Ocean Habitats - Dysphotic Zone
Twilight zone
Mid-water depths - 200-1000m
High productivity
Down-welling sunlight but insufficient for photosynthesis
Bottom of zone ultimate limit of sun's rays
90% animals bioluminescent
Most numerous vertebrates on Earth
Greatest animal migration - diel vertical migrations of deep-water zooplankton
- Move to surface at dusk to feed on phytoplankton
- Move down at sunrise to avoid predators
Largest invertebrate species e.g. Giant squid, colossal squid
Deep Ocean Habitats - Aphotic Zone
Midnight Zone
From ~1000m (to around 4000m)
No down-welling sunlight by 1000m
Bioluminescence used but NOT for counter-illumination
Prey increasingly scarce so adaptations for predation important
Deep Ocean Habitats - Continental Slopes
Drop very slowly (gentle) but sometime very steep
Areas of steeper slope - exposed rock for suspension feeder colonisation
Cut by submarine canyons (old river beds) - important in transferring material
Deep water corals form thickets - support diverse assemblages of polychaetes, ophiuroids, fish
- Corals are scleractinians (stony) = filter feeders (no symbiotic zooxanthellae)
- Growth slow as result (2-25mm per year) = vulnerable to bottom-trawling damage
Chemosynthetic cold seep habitats present here
Deep Ocean Habitats - Abyssal Plains
Flattest part of surface topography (<1:10000)
Abyssal hills occur - most abundant seabed feature
Underlying crustal topography obscured by <3km thick sediment = soft-sediment environments
High species richness of macrofauna living in sedmient
High species richness of sediment meiofauna
Deep Ocean Habitats - Seamounts
Active or extinct undersea volcanoes rising >1000m above seafloor
>39000 worldwide but <300 visually surveyed
Steep slopes = bare rock surfaces for suspension feeder attachment
Enhanced flow around seamounts = increased food for suspension feeders
Taylor column effect (rotating fluids disturbed by solid body form columns) traps larvae
Pressure from deep-sea trawling
Deep Ocean Habitats - Mid-Ocean Ridges
65000km chain of undersea volcanoes
Can be a rift
Rocky-deep sea habitat (similar to seamounts)
Non-chemosynthetic fauna less well-studied than at hydrothermal vents in ridges
Deep Ocean Habitats - Ocean Trenches
Poorly studied
Animal life observed at oceans deepest point (~10916m)
Limited knowledge from scientific trawls and lander deployments
Renewed interest in vehicles may improve knowledge
Ecological questions:
- Do trenches concentrate organic input?
- Do fauna exhibit biogeographic patterns?
- Do taxa have physiological depth limits?
Bioluminescence
Created by oxidation of luciferin substrate via luciferase enzyme (exact chemicals involve vary)
Animals obtain chemicals from food or bioluminescent bacteria in photophore organs
Most blue wavelength - attenuates less rapidly and matches down-welling light
Uses:
- Counter-illumination (only dysphotic)
- Signalling to conspecifics
- Catching prey
- Evading predators
Counter-Illumination
Dysphotic zone only - downwelling irradiance casts 'shadow'
Many predators have sensitive upward-looking eyes to detect shadows e.g. tube-eye, barrel-eye fish
Bioluminescence breaks up or mashs silhouettes
Matches downwelling irradiance = camouflage
Alternative to counter-illumination = transparent bodies to cast no shadows
Signalling to Conspecifics
Attract mates or social purposes
Examples in cephalopod molluscs - firefly squid
Catching Prey
Bioluminsecent lures e.g. angler fishes
Iluminating prey during hunting e.g dragonfish
Dragonfish:
- Emit red light from suborbital photophores
- Invisible to most animals
- Eyes contain chlorophyll that boosts colour range
- = Illuminate prey without prey realising
Evading Predators
Confuse predators - expel bioluminescent fluid
May also discourage predators - burglar alarm hypothesis = display or expelling sticky fluid attracts predators' predator and threatens them
Example - bloodybelly comb jellies
- Expel red light from transparent stomachs when eating
- Masks bioluminescent prey
- = Avoids detection by predators
Living Under Pressure
Pressure increases ~1atm per 10m = 5000m = >50,600kPa
Internal and external pressure equalised as solids and liquids incompressible = no structural adaptations to pressure and do not 'explode' at surface
Pressure can trap water on unfolded protein surface - prevents folding into enzymes
- Prevention using chaperone molecules = remove water and promote correct folding
Example - TMAO
- Fish and decapod crustaceans
- TMAO concentrations increase with depth
- Elasmobranch fish (sharks, rays etc) - high TMAO concentratios at surface = adaptation to osmotic stress
- Inability to accumulate sufficient TMAO limits elasmobranch fish to <3000m
- Hypothesis that teleost fish may not live at bottom of ocean
- Other taxa use different chaperones = live in hadal zones
Predation
Prevalent in aphotic and dysphotic
Ambush predation - lower energetic cost than active hunting
Adaptations for predation and to evade predation - evolutionary arms race
Predators tackle large prey = flexible jaws and expandable stomachs
- Dragonfishes - additional neck joint = wide jaw opening
Suspension Feeding
Need to escape boundary - seabed friction reduces flow
- Long stalks
- Climbing and colonise upstanding features
Anchor if stalked = limit distribution if no hard substrata available
Deposit-Feeding
Extract organic matter from sediment
3 types of gut:
- 'Batch-reactor'
- Ophiuroids
- One entrance and exit
- Episodic input and output times
- 'Continous-flow stirred-tank reactor'
- Decapods
- Seperate entrance and exit
- Episodic input and output times
- 'Plug-flow reactor'
- Holothurians
- Seperate entrance and exit
- Continous input and output
Scavenging
Olfactory and other sensory adaptations to detect food falls e.g. dead fish
Exploiting Larger Organic Falls
Some organic input much larger than particulates in size e.g. animal carcasses and wood falls
Taxa specialists in exploiting resources, using partnerships with symbiotic bacteria
- Xylophagidae wood-eating bivalves
- Osedax spp. bone eating polychaetes (zombie worms) - digest any bone
- Burrows in plesiosaur fossils
Finding a Mate
Pairing behaviour
- Finds member of opposite sex and sticks with it until mating
- Holothurian double excretion tracks on seabed
Accessory Dwarf Males
- Male parasitic on larger female = ensures mating
- Angler fish suborder Ceratioidei
- Osedax spp. polychaetes and xylophagidae molluscs
Opportunistic Mating Behaviour
- Squid and cephalopod moluscs shoot spermatophores at female for sperm transfer
- Deep-sea males found with spermatophores attached to them = shooting them at anything
Possible Aggregation of Broadcast Spawners
- External fertilisation method where unfertilised gametes released in water at same time
- Aggregations e.g. echinoids - adaptation to improve fertilisation success
Deep Ocean Evolutionary History
Most species smaller than shallow water relatives - lack of food?
Few exhibit gigantism e.g. isopods, chephalopods, amphipods
Example of Island Rule - colonists tend to evolve contrasting body sizes to ancestors
- Deep ocean recolonised repeatedly follow Ocean Anoxic Events in geological past
- Ocean Anoxic Events - mass extinction where oceans less oxygenated due to changing ocean currents/global climate change
- After recolonisation, colonists have few predators = larger than normal
Anthropogenic Impacts
Fisheries - increase has impacted slope and seamount habitats
- Bottom trawling damages seabed habitats
- Stony corals take long time to recover, as do many species due to slow growth/maturity times
Litter - modern litter and clinker
- Clinker - damage seafloors and create new exposed areas for suspension feeder attachment
Microplastics -accumulate in high concentration which explains missing plastic/garbage patches
- Dilutes marine snow - affects deposit feeders
Pollution - accidents from gas and oil may look cleared up but found in high concentration in deep
Potential - Seabed Mining at hydrothermal vents and seamounts
- Impacts poorly understood so studies to reduce effects necessary
Declines in Biomass in Deep Ocean
Two main patterns:
- Decline in biomass with depth
- Decline in biomass with distance from land
Related discussions on The Student Room
- Why are we looking for life on Mars?? »
- English Language Paper 1 Q5 »
- EPQ ideas, help! »
- marine biology / conservation / oceanography? »
- Enviromental Science or Conservation and Ecology »
- Are my A levels good for neuroscience? »
- can someone give me a mark out of 24 and a grade. »
- Marine biology at Plymouth »
- Advanced Higher Biology Project Ideas »
- best way to complete A level outside college? »
Comments
No comments have yet been made