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Chapter 16 The Ocean Depths
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“Inner Space” Dark, cold, inhabited by bizarre fearsome looking creatures Humans can only venture into this mysterious realm only with the aid of elaborate, specially designed craft – element of risk as well
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Least known of all our planet’s environments
Ocean depths include a number of distinct habitats
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Mesopelagic lies below the epipelagic “middle pelagic”
Still has some dim light – not enough for photosynthesis
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Deep Sea Below the mesopelagic No sunlight at all
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Several Different Habitats are found in the ocean depths
Each has a distinct community of organisms All of them lack primary production of food by photosynthesis Depend on organic matter produced in the surface layers of the ocean for food
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Characteristics of the Habitat
Life is much less abundant below the photic zone Most food particles get eaten before they sink into deeper water Deep-water organisms depend on the surface for food and oxygen
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There is a gradual thermohaline circulation to even the deepest parts of the sea, bringing life-giving oxygen To sink all of this way the oxygen-rich surface water must become very dense (cold and salty)
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Great Ocean Conveyor Surface overturn reaches the bottom in the Atlantic south of Greenland and just north of Antarctica After the water sinks, it spreads through the Atlantic and into the other ocean basins The water eventually rises to the surface and flows back to the Atlantic Thought to play a role in regulating earth’s climate
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The Twilight World
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The Twilight World The mesopelagic is a world of twilight
Dim light during the day is enough to see by As the depth increases the sea gets darker 1000m (3,300 ft) there is no light at all The absence of light marks the end of the mesopelagic zone
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Temperature at a given depth in the mesopelagic varies much less than in the epipelagic
Main thermocline is in the mesopelgaic Organism that move up and down in the water column encounter larger changes in temperature
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The Animals of the Mesopelagic
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Mesopelagic supports a rich and varied community of animals, which are often called midwater animals
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Zooplankton Major group of animals in the mesopelagic zooplankton are much the same as those in the epipelagic Krill and copepods dominate Krill and most mesopelagic shrimps have a common adaptation of midwater animals – photophores or light organs – specialized structures that produce light
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Figure 16.02
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The light produced is known as bioluminescence
Ostracods can be very abundant – group of crustaceans Arrow worms or chaetognaths – important midwater predators
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Jellyfish, siphonophores, comb jellies, larvaceans and pteropods are also common
Squids have photophores which are typically arranged in different patterns for each species
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Figure 16.04
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Midwater Fishes Most are quite small (2 to 10 cm) (1 to 4 in long)
Bristlemouths and lanternfishes are the most abundant Most abundant fish on earth (Cyclothone signata)
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Viperfish Dragon-fishes Barracudinas Sabertooth fishes Lancetfishes Snake mackerels Cutlass fishes
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Adaptations of Midwater Animals
They are well adapted to their unique environment
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Feeding and Food Webs Most of the food produced in the epipelagic is used there About 20% of the surface primary production sinks to the mesopelagic Mesopelagic is chronically short on food Abundance of midwater organisms reflects the productivity of the waters above
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Many of the characteristics of midwater animals are related to the lack of food
Large mouth Hinged, extendable jaws Fearsome teeth Very broad diets and eat just about anything Large jaws allow them to eat just about anything
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Two groups of Midwater Animals
One group stays in the mesopelagic (non-migrators) One group migrates to the surface each night (Migrators)
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Figure 16.09
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Nonmigrators A few species of small zooplankton, mainly copepods and krill These organisms filter out detritus and small amounts of zooplankton that sink Fecal pellets are an important part of the detritus eaten by mesopelagic filter feeders
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Most non-migrating midwater animals are fishes, shrimps and squids
Sit and wait predators Have a number of adaptations that reduce their energy requirements Flabby, watery flesh No swim bladder – too much energy required to fill and deflate it
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Have soft weak bones Have lost the defensive structures like spines and scales – reduce weight and make them more neutrally buoyant Are not streamlined – do not swim much
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Vertical Migration and the Deep Scattering Layer
Do not have to sit and wait for food to come to them Swim up at night to feed in the rich surface layers and during the day they descend several hundred meters or more Spend the day in a lethargic stupor
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Vertical Migration Adaptations
Well developed muscles and bones Retain the swim bladder for buoyancy Swim bladder can be filled with fat which does not expand when the pressure changes Can tolerate temperature changes
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Importance of Vertical Migration
Transports food into the deep water Vertical migrators carry products of surface production down with them Greatly increases the food in the mesopelagic Many non-migrating species feed heavily on the migrators Have more muscle so they are a more nutritious meal
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Sense Organs Have eyes that are large and unusually sensitive – fish, squid, shrimps Tubular eyes – some mid-water fishes have – complex visual system that is almost like having two pairs of eyes – very acute vision in the direction the eyes point
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Coloration and Body Shape
Mesopelagic predators rely heavily on vision Camouflage is perhaps even more important than in the epipelagic – basic strategies remain the same Countershading, transparency, reduction of the silhouette
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Transparency Common in the shallower and better-lit parts of the mesopelagic Copepods, jellyfish, shrimps, bristlemouth fish Deeper – tend to be more silvery Deepest darkest part – black or red – no red light appear black
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Countershading Black backs and silvery sides
To reduce the silhouette they have laterally compressed bodies which reduces the size of the body outline
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Bioluminescence Allows organisms to mask their silhouette
Bioluminescent photophores produce light that breaks up the silhouette and helps the animal blend in Counter illumination – the emission of light by midwater animals to match the background light
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Many mesopelagic animals can control the brightness of the light they produce and match it to the brightness of the light coming down from above
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The ways to produce light
Photophores Animal’s own specialized tissue Symbiotic bacteria that live inside the light organ
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Important Functions of Bioluminescence
Counter illumination The pattern of photophores is different among species and even between sexes – communicate and attract mates Bioluminescent secretions may serve as a defense mechanism Light to lure prey Light around eyes to help them see
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The Oxygen Minimum Layer
Midwater organisms have to deal with a shortage of oxygen in the water Oxygen enters the water in two ways: gas exchange with the atmosphere and as a by product of photosynthesis Once a water mass leaves the surface and descends into mesopelagic depths there is no way for it to gain oxygen
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Water becomes depleted in oxygen often in fairly defined layers around 50 m (1,600 ft)
Known as the oxygen minimum layer Oxygen concentration can drop to practically nothing
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The water below the oxygen minimum layer retains most of the oxygen it had when it left the surface since there is little decomposition and respiration
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Adaptations to Little Oxygen
Large, well developed gills Relatively inactive Complex biochemical adaptations like hemoglobin that functions well at low oxygen concentrations
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The World of Perpetual Darkness
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Lies below the mesopelagic
Sunlight never penetrates here Largest habitat on earth and contains about 75% of the planets liquid water
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The Pelagic Depth Zones of the Deep Sea
Bathypelagic zone (1,000-4,000 m 3,300-13,000 ft) Abyssopelagic zone (4,000-6,000 m 13,000 to 20,000 ft) Hadopelagic or Hadal pelagic zone – waters of the trenches (6,000 m and below)
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Each of the depth zones supports a distinct community of animals
They have many things in common
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Conditions of the Deep Pelagic Environment
The environment is very stable Always dark Always cold (1 to 2 C or 35 F) Salinity and other chemical properties are uniform No countershading Most zooplankton are drab gray or off-white, fish are black, shrimps are bright red
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Bioluminescence is very common – not used for counterillumination and these organisms have fewer photophores Used for attracting prey, communication and courtship Becomes less common the deeper you go Functional small eyes in the upper deep sea
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Fishes of the deep parts of the deep sea are blind or have very small eyes
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The Lack of Food
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Organisms face a continual shortage of food
Only about 5% of the food from above makes it down to the waters of the deep sea The animals do not make vertical migrations Deep sea animals are few and far between
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Most common, bristlemouths are small 50 cm (20 in) but they are larger than mesopelagic fishes
It is believed that deep sea fishes put their energy into growth and therefore reproduce slowly and late in life Adaptations to food shortages are similar to the mesopelagic but they are accentuated
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Adaptations to lack of food in the deep sea
Fish are sluggish and sedentary Flabby, watery muscles, weak skeletons, no scales and poorly developed respiratory, nervous and circulatory systems No swim bladders Have huge mouths and can consume prey much larger than they are
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Many have stomachs that can expand to accommodate large prey
Swallowers (Saccopharynx) Gulpers (Euryphyarynx) Anglerfishes – dorsal fin is a modified pole with a fleshy bit of tissue on the end
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Sex in the Deep Sea
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Finding a mate can be difficult
Most are hermaphrodites so that any two fish of a species can breed Bioluminescence, pheromones (special chemicals that a male can detect and follow), male parasitism (male bites on to the female and stays)
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The Deep Sea Floor
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Shares many characteristics of the pelagic waters above it
Absence of light Constant low temperature Great hydrostatic pressure Communities are different than the pelagic waters because there is a bottom
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Scientist know more about the deep sea benthos than the deep sea pelagic organisms
However only 500 m2 (5,400 ft2) of the 270 million km2 (105 million mi2) of deep sea floor have been studied
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Feeding in the Deep Sea Food shortage is critical however, once the food lands on the bottom it remains until it is found and eaten unlike the pelagic waters above Rain of organic matter from above is more like a drizzle
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Meiofauna, tiny organisms that live among the sediment particles are the most numerous organisms of the deep sea Suspension feeders are rare Deposit feeders are common – many are infauna burrowing through the sediment, some are epifauna resting on the sediment Polychaete worms are the most abundant macrofauna
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Crustaceans Bivalve mollusks Sea cucumbers
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Predators of the Deep Sea
Fairly rare Sea stars, brittle stars, crabs Fishes, squids Sea spiders (pycnogonids) Inverts of the deep sea are often much larger than their shallow water counterparts – deep sea gigantism
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Tripod fishes If a large piece of food makes it to the bottom amiphods are usually the first to find it Fish that come quick are: grenadiers or rattails, brotulas, cusk eels, deep sea spiny eels, hagfishes – tend to be larger, more active and more muscular than bathypelagic fishes
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The Nature of Life in the Deep-Sea Benthos
Life proceeds at a very different pace Animals grow very slowly, probably because of lack of food Live for a long time Low temperature and high pressure may slow down the processes of life Or they may need to live a long time to store up enough energy to reproduce
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Eggs are usually large with a good supply of food of the larva to make it through its early stages without eating Deep sea animals only produce a few eggs
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Figure 16.27
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Hot Springs, Cold Seeps and Dead Bodies
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1977 rich flourishing communities are found around the deep sea hydrothermal vents – Alvin
Around the vents there were gigantic worms, clams, dense clusters of mussels, shrimps, crabs and fishes Vent communities vary considerablely from place to place Over 400 species have been found around different vents
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Primary producers are chemosynthetic archaea and bacteria
Hot water rising from the vents is rich in hydrogen sulfide which is toxic to most organisms but is also an energy rich molecule Chemosynthetic prokaryotes use the energy in hydrogen sulfide to make inorganic matter – they are the base of the food chain
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Many vent organisms have symbiotic bacteria that live within them and provide them with organic matter
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Cold Seeps Places mostly along continental margins or in sediment rich basins where hydrogen sulfide and methane seep out from the sea floor Chemosynthetic prokaryotes use these molecules to support a community
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Dead Bodies After scavengers eat a whale the decomposing remains produce hydrogen sulfide and methane and can support a community similar to the vents and seeps
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Spring, Seep and Body Communities
Organisms enjoy an energy rich environment and grow fast and large Specialized habitats that are tiny oases separated by vast distances Unreliable energy sources
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The End
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