Marine Ecology Flashcards

(137 cards)

1
Q

Describe and explain the seasonal cycle of biological activity (e.g., phytoplankton, zooplankton and fish biomass and production) in the pelagic.

A

Other factors influence phytoplankton growth rates, including water temperature and salinity, water depth, wind, and what kinds of predators are grazing on them. Phytoplankton can grow explosively over a few days or weeks. Basically, the seasonal cycle is driven by sea-surface temperature and the onset of the thermocline leading to phytoplankton blooms during spring, the prevalence of thermal stratification leading to exhaustion of nutrients and subsequent demise of phytoplankton during summer-autumn, and remixing and regeneration of nutrients during winter.

Plankton predominantly comprises short-lived organisms. As a rule, these reproduce so rapidly that several generations may be produced within a single year. The development of planktonic organisms generally follows a regular annual cycle that begins with a spring bloom of the phytoplankton.

Fish biomass:
LOOK AT SLIDES

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2
Q

Explain how environmental factors and the species diversity and biomass of benthic communities vary from the continental shelf to the deep sea.

A

There are a lot of factors that can affect benthic biodiversity along a depth gradient like water temperature, light availability, oxygen (and other elements) concentration and pressure.

Interactions between pelagic and benthic environments are related to a variety of abiotic and biotic processes that have a major influence on the structure and dynamics of marine ecosystems. Transport of particulate and dissolved materials, gases, as well as living organisms, and also sedimentation and erosion are subsumed under these processes that induce a shifting of materials between benthic and pelagic material pools and vice versa. Imbalances in these transactions result in a change of biotic structures and have far-reaching consequences for the development of the communities. Exchange processes are either directed from water to the bottom sediment (termed as pelagic–benthic) or reversed (termed as benthic–pelagic), and impact on abiotic material pools as well as on the biota, such as producers and consumers, or can be related to the exchange between abiotic and biotic material components.

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3
Q

Describe and explain intertidal zonation on rocky shores

A

Intertidal zonation refers to the frequently observed pattern by which species replace one another along a gradient from the low to high tide lines along many of the world’s coastlines.

variation in the distribution of organisms caused by differences in both biotic and abiotic conditions along an environmental gradient. Organisms living on the rocky shore have different adaptations to these factors and therefore will be able to survive at different heights on the shore accordingly.

The intertidal zone or littoral zone is the shoreward fringe of the seabed between the highest and lowest limit of the tides. The upper limit is often controlled by physiological limits on species tolerance of temperature and drying. The lower limit is often determined by the presence of predators or competing species.

The rocky intertidal ecosystem can be divided into four zones: the splash zone, high intertidal, middle intertidal, and low intertidal

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4
Q

What is the Coriolis effect (force)?

A

Apparent deflection of a moving object when viewed from a rotating frame of reference.
Freely moving objects on the surface of the Earth experience the ‘Coriolis force’.
On a non-rotating planet, ocean currents (and winds) would flow directly from areas of high pressure to low pressure.
Because Earth rotates, currents (and winds) flow to the right of this direction north of the equator, and to the left of this direction south of the equator.

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5
Q

What is Ekman Transport?

A

Friction between wind and water surface causes water to move in direction of wind.
The Coriolis effect deflects this current.
The surface layer drags the layer beneath, which is also deflected.
The net movement of the ocean’s surface layer is perpendicular to the right of the wind in the Northern Hemisphere and to the left in the Southern Hemisphere.

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6
Q

Deep Ocean Circulation and Thermohaline Circulation

A

Thermohaline circulation is due to differences in the density that arise from variations of temperature and salinity.
thermo = heat
haline = salt (halide ions)
Solar radiation warms waters in the tropics, causing them to expand (become less dense) and float.
The ocean loses heat to the atmosphere at high latitudes (air colder than water), causing the surface waters to cool and contract (become denser) and sink.

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7
Q

What affects the density of sea water?

A

Density = mass/volume
Units kg m-3
Density increases as temperature decreases
Density increases as salinity increases
Density increases during ice formation because salt is excluded from the ice
Density decreases following rain due to dilution of salt

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8
Q

Mechanisms of Deep Water Formation

A

The mechanisms of deep-water formation are different in North & South Atlantic.
In the North Atlantic, high salinity water (brought north by the Gulf Stream) is cooled in winter leading to deep convective mixing.
On the Antarctic continental shelf, ice formation increases salinity and upon further cooling, the dense water flows off the shelf and down the continental slope.

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9
Q

Thermohaline Conveyor Belt

A

North Atlantic Deep Water flows south along the western side of the N. Atlantic.
Antarctic Bottom Water is the densest water and flows north along the western side of the S Atlantic.
These two deep currents meet in the S. Atlantic and flow eastward into the Indian and S. Pacific Oceans

The deep water flows from the Atlantic to the Pacific, are balanced by a return flow of warm surface waters from the Pacific to the Indian and back to the Atlantic Ocean.
The combination of these slow deep and surface water flows is referred to as a conveyor belt.

The thermohaline circulation is sluggish compared with the wind-driven circulation.
The entire circulation and replacement of the deep waters takes about 1000 years
750 years for the Atlantic
1500 years for the Pacific

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10
Q

What is an ion?

A

an ion is a charged atom or charged molecule
ions form by adding or removing one or more electrons from an atom or molecule
a cation is a positively charged ion
e.g., sodium ion: Na+
an anion is a negatively charged ion
e.g., chloride: Cl-
sulfate: SO42-
ionic bonds hold crystals together
e.g., sodium chloride (= table salt): NaCl

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11
Q

Why is water sometimes described as a universal solvent?

A

Water (H2O) can dissolve more things than any other natural substance.
It is a polar molecule, that can form hydrogen bonds.
Water is good at dissolving salts
which consist of positively (+) and negatively (-) charged ions
NaCl → Na+ + Cl-

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12
Q

What are the sources of the ions in seawater?

A
Runoff from the continents (weathering of rocks)
Na+ , K+, 
Ca2+ , Mg2+
Volcanic activity (hydrothermal vents)
HS- , Cl-
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13
Q

How does the rule of constant proportions make measuring salinity easier?

A

The rule of constant proportions states that the relative amounts of the various ions in seawater are always the same (e.g., independent of salinity)
e.g.
Chloride = 55.03% of salinity everywhere in the sea
Sodium = 30.59% of salinity everywhere in the sea
the rule holds for other major ions
This allows chloride, which is easy to measure, to be used to calculate salinity
Chlorinity = mass of chloride in a kg of seawater

Conductivity is now commonly used to measure salinity in practical salinity units (psu)
1 psu = 1 ‰ or 1 ppt

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14
Q

Limiting Nutrients

A

The two main limiting nutrient elements for biological production in sea are nitrogen (N) and phosphorus (P).
These are present as dissolved inorganic ions
phosphate: PO43-
nitrate : NO3-
Concentrations of these ions are often very low in surface waters.
Productivity of the oceans often depends on the regeneration (recycling) of inorganic N and P from organic matter.

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15
Q

Vertical profiles of dissolved O2

A

Feature: oxygen minimum zone
located in thermocline
high respiration rate
limited exchange of water

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16
Q

What are Biogeochemical cycles?

A

Pathways by which a chemical element moves through different compartments (called reservoirs).

Examples
Carbon cycle
Nitrogen cycle
Sulphur cycle
Phosphorus cycle
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17
Q

The Carbon cycle

A

CO2 moves between ocean and atmosphere due to physical-chemical processes (Solubility pump).

C is exchanged between the ocean and the biota via:

Photosynthesis removes CO2 from the atmosphere and ocean.
CO2 + H2O + light → CH2O + O2

Respiration releases CO2 to the atmosphere and ocean:
CH2O + O2 → CO2 + H2O

Carbon enters the foodweb via grazing

Carbon is returned to the ocean as CO2 via respiration

Some primary produces will sink when they die, sequestering (storing) carbon in sediments

Dead stuff becomes detritus/POM (Particulate organic matter) which can be:

Decomposed by bacteria, producing CO2, POM, and DOM (Dissolved organic matter)

Feed on by animals, returning carbon to the foodweb

detritus/POM that is not decomposed sinks, sequestering carbon in sediments

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18
Q

The biological pump

A

Phytoplankton and macro-algae (seaweed) fix carbon

Incorporating C into the food chain (grazing) - or releasing it as DOC/POC

Feacal pellets, marine snow, and dead marine organisms sink to the deeper layers

Where they decay consuming dissolved oxygen and giving off CO2.

Upwelling returns this CO2 to the epipelagic.

The biological pump requires the input of nutrients (N, P) to sustain plankton blooms.

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19
Q

Microbes and the carbon cycle

A

Play a critical role in all nutrient cycles

Fixing carbon
Link to the food chain
Also a source of CO2

Microbial action can make carbon inaccessible recalcitrant – RDOM

This sinks and can be stored for 1000s of years

Microbes decompose POM and DOM, producing dissolved CO2

Microbes degrade the most assessable carbon first.

Carbon that is harder to degrade, called recalcitrant carbon (RDOM), sinks before is can be degraded and is stored in sediments.

The balance between how much carbon sinks and how much is releases is critical in global carbon budgets.

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20
Q

The Nitrogen cycle

A

Nitrogen is fixed by bacteria and cyanobacteria

Key players: Trichodesmium spp.
Atelocyanobacterium spp.
(cyanobacteria)

Bacteria and archaea cycle nitrogen between ammonia, nitrites, and nitrates via nitrification (aerobic)

Fixed nitrogen and nitrates are taken into the biota and cycle through the food web

This nitrogen can be excreted as DON, or sink when taxa die (POM).

Bacteria and archaea recycle POM and DON in decomposition (ammonification)

Nitrogen is returned to the atmosphere via bacterial Denitrification (anaerobic)

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21
Q

The phosphorus cycle

A

Not found as a gas (Contrast to Carbon and Nitrogen)

Normally as part of a phosphate ion: PO43-

Found as salts in ocean sediments or in rocks.

Uplift brings ocean sediments to land.

Phosphate becomes available by chemical weathering.

Input to oceans is via rivers.

Enters the foodweb through uptake by plants, algae and bacteria.

Dissolved phosphate is precipitated and sinks into sediments

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22
Q

More on Limiting nutrients

A

Nutrients, particularly N and P, limit the fertility of many undisturbed ecosystems.

P is typically the main limiting nutrient in freshwaters, followed by N.

N is usually most limiting in marine systems, followed by P.

Although CO2 may limit photosynthesis in terrestrial plants, inorganic C is rarely limiting in aquatic systems.

The micronutrient Fe, has recently been found to be the main limiting nutrient over about 1/3 of the ocean surface – Iron fertilisation hypothesis.

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23
Q

Jawless Fish (Agnatha)

A
 cylindrical, elongated body
 cartilaginous skull
 lack vertebrae
 lack jaws
 lack scales
 feed by suction using a round muscular
mouth and sharp teeth
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24
Q

Hagfishes

A
Marine
 Jawless elongate fish
 Lack fins
 No vertebra (sort of)
 Burrow in muddy bottoms at
moderate depths in cold waters
 Feed mainly on dead or dying fish
 Produce slime!
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25
Lampreys
Mainly freshwater or costal - Some migrate to the ocean to mature and bread in freshwater  Have unpaired fins  Redemptory vertebra  Most species are not parasitic! - sea and river lamprey attach to fish, rasp a hole into the victim, and feed on fluids and tissues
26
Cartilaginous Fishes | Class Chondrichthyes
Cartilage skeleton - lighter and more flexible than bone  Placoid scales - tough sandpaper like skin  Moveable hinged jaws  Ventral mouth with well developed teeth  Maintain buoyancy through a oil-rich liver  Can detect weak electric field to locate prey - ampullae of Lorenzini
27
Sharks
Fusiform shape (tapered at both ends) - aids movement through water  Strong caudal (tail) fin for propulsion  Two dorsal fins and paired pectoral fins  5-7 gill slits on each side of body behind the head  Most are carnivorous  Largest sharks are filter feeders (whale shark - Rhincodon typus)
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Ampullae of Lorenzin
Sensing organ that uses electroreceptors to detect the weak electrical currents emitted by living organisms. • For example fish hiding under sand. • Consists of pores connected to gel filled tubes. • Also found in other chondrichthyes (e.g. rays)
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Bony Fishes | Class Osteichtyes
``` Dominant vertebrates in the sea  More taxonomically diverse than rays & sharks  Wide range of shape, size, color, swimming ability, feeding habits, reproduction and behavior ``` Skeleton made of bone  Anterior, midline mouth  Swim bladder to provide buoyancy  Scales made of bone, covered by skin and mucus  Gills protected by a flap of bony plates (operculum)
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Swim bladder
``` Swim bladder (5% of animal’s volume).  Two gas filled sacs – fish achieve neutral buoyancy by changing the volume/pressure of the bladder. ``` Only in bony fish - so what about sharks?  Altered salt content of cellular fluids (low salt) relative to seawater.  High lipid content - liver may occupy up to 25% of volume of a shark  Also “flying” using fins for lift
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Lateral Line System
Gelatin-filled tunnel - runs beneath skin along each side from tail to head - contains clusters of nerve cells for detecting vibration - detects reflections of bow waves off nearby objects, including other fishes Allows rapid movement near solid surfaces and tight schooling
32
Body form in relation to feeding and habitat in bony fishes
Rover predators (tuna, marlin, blue shark) long torpedo shaped = efficient swimmers  Lie-in-wait (ambush) predators (barracuda) – Body does not taper. Acceleration from strong powerful tail, (caudle peduncle is wide).  Flatfish (flounder and plaice - bottom dwelling  Deep-bodied (butterfly fish) – lots of contact with water = manoeuvrable, tight turns  Eel-like (moray eel) fishes are adapted for moving through crevices
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Anadromous and catadromous fish
Anadromous: Feed and grow at sea - Reproduce in freshwaters • Salmon Catadromous: Feed and grow in freshwaters  Reproduce at sea  European and American Eels
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The Epipelagic
``` Topmost zone, light is abundant ▪ This is where photosynthesis takes place = lots of food ▪ You need to see your lunch before it sees you – or you become lunch! ▪ Speed is king – escape or catch Adaptations: - Large eyes - Strong muscles, fast swimming - Counter shading - Streamlined ```
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Mesopelagic environment
``` Sufficient sunlight for vision, but not photosynthesis ▪ Energy comes from sinking organic material - ≈20% of primary production sinks out of the epipelagic - <5% of primary production reaches 1000 m Depends on the surface layers for O2 Natural thermocline ``` Short on food: Most adaptations are concerned with finding food, or conserving energy They also have to stay afloat, within these constraints Vision is still a key sense: Seeing in the dark, and not being seen is key. Despite the lack of food, as much as 95% of fish biomass may be in the mesopelagic!
36
Mesopelagic Fishes | Adaptions to lack of food
Common adaptations: ``` ▪ Small size – don’t waste energy Make the most of every meal ▪ Large mouths ▪ Hinged extendible jaws ▪ Needle-like teeth ▪ Unspecialised diets ```
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Mesopelagic Fishes | Adaptions to lack of food
Common adaptations: ``` ▪ Small size – don’t waste energy Make the most of every meal ▪ Large mouths ▪ Hinged extendible jaws ▪ Needle-like teeth ▪ Unspecialised diets ``` Carnivores have: ▪ large mouth ▪ extendible jaws & needle-like teeth (e.g. viperfish & rattrap fish) Zooplanktivores have: ▪ smaller mouths to rapidly ingest small prey ▪ upward facing eyes to spot zooplankton in the downwelling light (e.g. lanten fish)
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The two strategies of | mesopelagic fish
Stay put, sit and wait 2. Go find food Many mesopelagic fish undergo a diel vertical migration, moving up to the surface at night (when they are safer from predators) to find food. This is the biggest migration on earth.
39
Vertical migration
Following food source (e.g. zooplankton) ‘Safer’ from predators at night Vertical migrators possess - well developed muscles - swim bladder (often filled with lipid rather than gas) Migrators contribute to the deep-scattering layer Migrators bring surface production down with them - enriching food in the mesopelagic - non-migratory predators feed on them
40
Characteristics of non migrators
``` non-migrators cope with the reduced food supply (relative to migrators) by reducing energy demand ▪ near neutral buoyancy ▪ lack swim bladders ▪ less muscle ▪ watery flesh ▪ soft weak bones Sit and wait predators - lurk in the dark and wait for a meal (use of lures) ```
41
Mesopelagic Fishes | Adaptions to low light
``` Look up ▪ Large, often tubular, eyes ▪ Upward orientation ▪ Main retina for upward field ▪ Secondary retina for lateral vision ``` Vision is still important in the mesopelagic, but counter shading is less effective with less light. Most fish are looking up at you so common adaptations are: • Transparency • Lateral compression of body to reduce silhouette Counter illumination Counter illumination - - photophores (light emitting organs) on underside (ventral) - bioluminescence - blue light to match spectrum of downwelling light Countershading - using coloration (silver sides and black backs) to blend in.
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Bathy & abyssopelagic | Adaptations to Very Low food Supply
We see many adaptations that we saw in the mesopelagic to deal with lack of food: ▪ Week flabby muscles (don’t waste energy) ▪ Large mouth/teeth ▪ Generally slow metabolisms ▪ Reduced or no swim bladder ▪ Bioluminescence ``` Adaptations seen in mesopelagic fish to low food are generally exaggerated. Don’t miss a meal: ▪ large mouth ▪ hinged extendible jaws ▪ long sharp teeth ▪ bioluminescent lure Don’t waste energy: ▪ sluggish ▪ flabby watery muscles ▪ weak skeletons ▪ poorly developed respiratory and circulatory systems ▪ poorly developed nervous system ▪ lack swim bladders ```
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Sex in the deep sea
Hard to find a mate in a sparsely populated sea. Especially when you don’t move much. ▪ Some species are simultaneous hermaphrodites ▪ Some use pheromones to find each other ▪ Angler fish have dwarf males that attach to females (can't waste an opportunity to mate)
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Deep sea benthic fish
No natural light here and very little food. Very little food reaches the bottom - Food falls (whale carcasses etc) - Marine snow and fecal pellets (POM) Covered in a fine muddy sediment. - bacteria and meiofaunna degrade POM/DOM and make it available to the food chain - Fish also scavenge larger food fall directly
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Characteristics of deep sea benthic fish
Scavengers with strong muscles to move to food falls ▪ Relatively large and slow growing ▪ Often elongated (eel-like) ▪ Strong muscles (will swim a long way to find food). ▪ Small or no eyes (few are bioluminescent) ▪ Black/brown in color
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phytoplankton: Diatoms
unicellular protist about 40-50% of marine primary productivity silica cell wall called a frustule single cells or long chains ``` capable of rapid growth tolerant of low light temperate and polar regions bloom forming (spring bloom, upwelling) adequate light high nutrient concentrations subject to intense grazing pressure from zooplankton cysts (dormant stage) survive for years (e.g. in sediments) seed for new population growth ```
47
Coccolithophores
Coccosphere Cell wall composed of calcium carbonate (CaCO3) plates Complex, and still poorly understood, life cycle Often important in tropical waters Capable of forming large blooms, usually following the diatom bloom Major source of CaCO3 to the sea floor. Responsible for extensive CaCO3 rock formations (e.g. White Cliffs of Dover). Upon dying, coccolithophores produce large amounts of dimethyl sulfide (DMS), a gas that escapes to the atmosphere. DMS may aid cloud formation and allows sulfur to be transported from the ocean to the land.
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Dinoflagellates
``` Dinoflagellates motile using two flagella longitudinal (trailing behind the cell) transverse (around the cell's middle) cell wall (theca) consists of cellulose ``` Capable of vertical migration in stratified waters Slow growing, requiring high light Form cysts that can persist in sediments for years seed for new population growth when environmental conditions are favourable Red tides, not due to rapid growth, but rather due to persistence and accumulation of toxins associated with defences against grazers Small contribution to marine primary productivity None-the-less, ecologically and economically important Includes about 100 toxic species, producing a variety of effects in man and fish.
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Cyanobacteria
prokaryotic blue-green to pink in colour phycobiliproteins (phycocyanin, phycoerythrin) are major light-harvesting pigments includes the smallest and some of the largest phytoplankton Trichodesmium is capable nitrogen fixation - transforming N2 gas into ammonium Synechococcus accounts for about 20-30% of total ocean primary productivity Prochlorococcus is the smallest photosynthetic cell (<1 µm diameter)
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What are the characteristics of the zooplankton?
heterotrophic protists and animals rely directly, or indirectly, on phytoplankton for food largest biomass in surface waters (epipelagic) ``` metazoan zooplankton Crustacean zooplankton Chaetognaths (arrow worms) Pteropods (molluscs) Gelantinuos zooplankton (coelenterates, ctenophores, salps) ``` protozooplankton ciliates, flagellates, amoeboids ``` Single-celled animals that are grouped based on motility into flagellates ciliates amoeboids: foraminifera radiolaria ``` consume bacteria, phytoplankton and other protozooplankton fed upon by larger zooplankton mixotrophic protists are both photosynthetic and phagotrophic
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Protozooplankton
Radiolaria silicate test feed using long, thin, retractable pseudopodia planktonic species may contain symbiotic algae (zooxanthellae) many benthic species
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BACTERIO- and VirioPlankton
The term bacterioplankton refers only to heterotrophic prokaryotic organisms in the plankton. excludes cyanobacteria, which are autotrophic. includes archaea, which are not bacteria. Bacterioplankton consume organic matter consuming O2 and releasing CO2. Bacterioplankton also play important roles in the nitrogen cycle. Virioplankton are viruses that infect bacteria, phytoplankton, protozoa and other organisms.
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Plankton DEFINITIONS
``` Meroplankton = zooplankton that spend part of their life in the plankton and the remainder in the benthos Holoplankton = planktonic organisms that spend their entire life in the plankton Ichtyoplankton = planktonic developmental stages of fish Neuston = organisms associated with the sea surface Pleuston = organisms that protrude into the air (Portuguese man-of-war) ```
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Primary production
Autotroph = an organism that manufactures its own organic carbon using energy from the sun or other sources. photosynthesis uses light energy (photoautotrophy) chemosynthesis uses chemical energy (chemoautotrophy) Primary production = the conversion of inorganic carbon into organic compounds by autotrophs.
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What affects Primary production?
availability and uptake of nutrients temperature affects the rate of metabolic reactions specific temperature optima and tolerance ranges intensity and quality of light net primary production is confined to relatively shallow water depths due to the high attenuation of light in water the relationship between photosynthesis and light intensity Limiting Factors: Nutrients Nitrogen is the principal limiting nutrient for many pelagic marine ecosystems. Iron is a limiting factor in the Southern Ocean and other ‘high nitrate/low chlorophyll’ (HNLC) regions. Diatoms require silicate. Phosphorus can limit growth of N2-fixing cyanobacteria.
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What are the requirements for a phytoplankton bloom to take place?
nutrients in high concentrations near the sea surface sufficient light throughout the surface wind-mixed layer to allow net phytoplankton growth, and the growing phytoplankton population must also escape from the high mortality imposed by zooplankton grazers
57
What are the adaptations and conditions that allow diatoms to persist through winter?
diatoms tolerate low light, mixing keeps these non-motile cells in suspension, silica cell wall and large cell size provides protection from many protozoan grazers
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Start of Spring Phytoplankton Bloom
phytoplankton growth rate increases due to the increased availability of solar radiation, and shallower mixed layer depth diatoms are poised to take advantage of these favourable conditions because of their ability to grow rapidly, and to avoid being eaten by protozoa
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End of Spring Phytoplankton Bloom: Grazing
diatoms provide an excellent food source for crustacean zooplankton calanoid copepods are the principal grazers of diatoms adult female copepods may lay up to 50 eggs a day comb jellies, tunicates and arrow worms become abundant, grazing on the copepods zooplanktivorous fish become abundant in the declining phase of the spring bloom
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protozoan zooplankton in summer
protozoan zooplankton become increasingly important as the water column remains stratified protozoa regenerate nutrients in summer most of the primary productivity depends on recycling of nutrients between protozooplankton, bacterioplankton and phytoplankton with little export in sinking particles
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Dissolved nutrient concentrations are typically very low in summer. What adaptations contribute to success during summer?
picophytoplankton have high surface area-to-volume ratios and high nutrient affinities N2-fixing cyanobacteria can tap the atmospheric N2 source vertically migrating dinoflagellates, because they can migrate to nutrient rich deep waters.
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Latitudinal variability in primary production
Regulated by the same environmental factors and ecological interactions as the seasonal cycle. Typically nutrient-limited in tropical seas. Little seasonal variability. Typically light-limited in polar seas. Summer bloom.
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Predation Pressure in the Pelagic
One of the major differences between the pelagic and most other environments is that there is virtually no place to hide in the open water. Exceptional, are clumps of the floating plant Sargassum and other floating debris. These ‘islands’ often attract animals.
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How do organisms protect themselves from high predation pressure
``` Body armour (Chitin, CaCO3, SiO2, Cellulose) Chemical warfare (toxic dinoflagellates) Camouflage transparency colour/shading counter illumination Diel vertical migration ```
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Vertical Migration
There are two broad classes of vertical migration. Ontogenetic - associated with different developmental stages in an organism’s life history (seasonal). Diel - a behavioural response that involves a trade-off between: maximising feeding and avoiding being eaten. Diel Vertical Migrations (DVM) often involve upward migration at or after dusk (following isolumes) and downward migration prior to dawn (endogenous biorhythm)
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Langmuir Circulation
Accumulation of buoyant cells in sinking regions of Langmuir circulation, or accumulation of sinking cells in rising regions of Langmuir circulation.
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Cetacea
Order Cetacea Odontoceti: Toothed whales: dolphins & porpoises Mysticeti: Baleen whales: the great whales streamlined, elongate body to reduce drag forelimbs reduced to stabilising paddles hind limbs completely reduced (vestigial bones) highly muscular posterior ending in a horizontal tail for propulsion - fluke nearly hairless body thick subdermal fat layer (blubber) insulation streamlining energy reserve ``` blow-hole (nostrils) located on back of head expel CO2 upon reaching the surface Mysteceti – two Odontoceti – one storage of O2 haemoglobin in blood myoglobin in muscle hearing is the most important sense sound travels faster and further in water than in air light is attenuated rapidly some river dolphins are blind ```
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Toothed whales and porpoisesOdontoceti
``` sperm & killer whales, dolphins & porpoises active hunters of large prey sonic and subsonic clicking signals echolocation communication social animals ``` killer whales travel in small pods dominant female, several females and subordinate males subordinate males remain with mother’s pod but mate with females from other pods
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Echolocation
Clicks are generated by moving air between internal cavities (air sacs) and are focused using a fatty structure (melon) Incoming sound is perceived by lower jaw, and transmitted to the inner ear
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Baleen whales
filter feeders having baleen plates instead of teeth right whales swim slowly = current = zooplankton (<3 mm length) strained on baleen plates rorqual whales intermittent suspension feeders -expandable pleats of elastic tissue in throat and thorax -enclose swarms of zooplankton in mouths and use tongue to force water through baleen plates to strain prey
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Migrations
most toothed whales do not migrate, but do travel to search for food many baleen whales - feed in polar regions on abundant plankton in summer - migrate to warmer regions to breed in winter still uncertain how whales navigate - visual clues when close to shore - earth's magnetic field
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Pinnipeds (seals)
large eyes for vision in low light hearing most important sense whiskers are tactile organs used in detecting prey moult annually feed on fish, cephalopods, krill, other seals some bottom feeders (crabs and shellfish) prey to sharks, killer whales migrate between feeding ground and haul out sites mate and rear young on rocky shore areas suitable beaches are limited in extent, hence large colonies and competition for space large males arrive first and establish territories, and maintain them by display and combat dominant males maintain harems subordinate males at the fringes of the territories of the dominant males
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Adaptations for diving in animals
Adaptations to prevent the bends -formation of N2 bubbles in blood and joints during rising from depth collapse lungs before diving -limits the amount of N2 that can dissolve in blood under high pressure experienced at depth Adaptations to reduce O2 demand Heart rate slows (in northern elephant seal, for example, from 85 to 12 beats per minute) Blood supply to vital organs (brain, heart) is maintained Blood supply to extremities and intestine is reduced
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Flow of Energy in Marine Systems
``` Trophic interactions (i.e. predation) lead to flow of energy Not all consumers eat all prey Not all consumers eat producers Energy flow through steps – “Food-Chain” Each step = Trophic level Many chains in every web! ```
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Tides are one of the dominant forces affecting near-shore life
tides alternatively submerge and expose intertidal plants and animals affecting - physical stress (heat and water stress) - food supply - susceptibility to predation tides drive water circulation in bays tides trigger spawning in some species
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What causes the tides?
Two forces cause the tides - gravitational forces exerted by moon and sun, and - centrifugal force due to rotating earth. Result is the equilibrium tide -two bulges on opposite sides of the earth.
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Spring & Neap Tides
Spring tides = greatest tidal range (highest high and lowest low) occur during new and full moon Neap tides have the lowest tidal range (lower high and higher low) occur when sun and moon are at 90o.
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Micro and Macro tidal
The tidal range in the ocean varies from 0 (Caribbean) to 15 m (Bay of Fundy, Canada) Macrotidal = large tidal range > 4 m range British Isles tidal currents are important in sediment transport Microtidal = small tidal range <2 m Mediterranean sea waves are important to sedimentary processes
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Wave formation
Waves begin to form as soon as the wind starts to blow Size of wave depends on speed and duration of wind fetch = span of water over which the wind blows Waves break when their orbital motion feels the friction of the sea bed
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Vertical zonation in Rocky Intertidal Zone
Vertical zonation - dominant species occur in distinct horizontal bands - along a gradient from fully terrestrial to fully marine. Zones are compressed in protected areas with low tidal range. On open coasts, the zones are extended by wave splash.
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Upper Intertidal Zone
Lichens (Verrucaria) -black blotches cyanobacteria (Calothrix) -dark green mats Tufts of algae - algae (Ulothrix) - brown (Pelvetia) - red (Porphyra) Periwinkles (Littorina) and Limpets (Patella) graze on algae Top predators include terrestrial animals (e.g., birds, rats) and marine predatory snails
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Middle Intertidal Zone
Acorn barnacles form bands at upper end (Chthamalus, Balanus & Semibalanus) Lower in the mid-intertidal are - mussels (Mytilus) - gooseneck barnacles (Pollicipes) - rockweed (Fucus & Pelvetia)
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Lower Intertidal Zone
Mussels & barnacles are rare due to high predation pressure Zone is dominated by seaweeds Sea urchins are common grazers
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Rocky Intertidal Zone: Causes of Zonation
Four major factors involved in zonation are larval settlement (dispersal & colonisation) physiological tolerance of stress Predation (e.g. by seastars, birds etc) competition for space
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Physical Stress - Wave Action
``` Epifauna = live on the surface Some animals avoid being dislodged by seeking shelter in cervices behavioural response Adaptations to hold on holdfasts in seaweeds mussels glue themselves on using byssal threads limpets and chitons (right) cling on using a muscular foot ```
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Physical Stress - Temperature
extremes of temperature during periods of emergence sea has more stable temperature than air due to high heat capacity of water adaptations include: ability to tolerate high temperature range use of light colours to reflect sunlight sheltering in moist places to allow evaporative cooling (under rocks… like the below)
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4 classifications of estuaries
Drowned river valley (= coastal plain estaury) formed when sea level rose at end of last ice age Examples include Thames Estuary Delaware Bay Chesapeake Bay Fjords are estuaries in deep valleys cut by glaciers formed when sea level rose at end of last ice age high latitudes including Norway, Southwestern Chile Bar built estuaries: sediments build up to form barrier sand bars & islands North Carolina Bays behind protection given by Cape Hatteras North Sea coast of the Netherlands & Germany Tectonic estuaries are formed by subsidence
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Estuarine circulation
Freshwater flows out near the surface Saline water flows in near the bottom Salt wedge = a layer of denser, saltier seawater that flows along the bottom of the estuary There is mixing at the interface between salt and fresh waters due to wind, tides and river flow Tidal prism = the volume of water that is moved in and out of an estuary with the change in the tides
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Salinity and biodiversity
Mid-salinity zones of estuaries are often regions of low taxonomic diversity Estuarine species must be able to tolerate salinity fluctuations Stenohaline species tolerate low salinity range Euryhaline species tolerate a high salinity range Osmoconformers allow the salinity of their body fluids to change with external salinity Osmoregulators keep the salt content of their body fluids constant
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Primary producers of muddy shores
Diatoms (Bacillariophyceace) Cyanobacteria (Cyanophyceace) 3. Euglenoids e.g. Euglena 4. Macroalgae e.g. Ulva, Enteromorpha 5. Angiophyceace e.g. Zostera (eel grass) 6. Chemoautotrophs e.g. Sulphur oxidising bacteria
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Salt marshes
Salt marshes are intertidal habitats dominated by cord grasses (Spartina spp.) Spartina typically spreads by vegetative growth of rhizomes (root networks within sediments) Often a marsh consists of one or a few clones Roots and rhizomes trap & stabilise sediment, leading to build-up of the marsh and infilling of estuaries Spartina blades contain siliceous deposits that deter grazing Typically, <10% of blade growth is consumed by grazers; the remainder fuels detritus food chains Salt marsh creeks are often productive nurseries for marine fish species.
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Spartina anglica
Spartina anglica originated in southern England in about 1870 when the European cordgrass S. maritima hybridized with the introduced American S. alterniflora more vigorous than either native species -rapid rate of growth, high fecundity and aggressive colonisation planted for coastal erosion control - rhizome systems bind coastal mud - stems increase silt deposition, thereby assisting in land reclamation from the sea
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Mangroves
mangroves are salt tolerant tropical and subtropical trees salt is secreted from leaves by salt glands mangrove forests (mangal) support detritus-based food webs root systems are adapted to anoxic, waterlogged conditions oxygen is transported to below ground tissue by upward facing pneumatophores allowing aerobic metabolism in an anoxic sediment fine roots take up nutrients prop roots support the body of the tree
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Seagrass Meadows
Like cord grass (Spartina), these grasses have extensive rhizome systems Reduced turbulence traps fine sediments Roots extract nutrients from sediments Shoots obtain CO2 from the water column Beds expand largely by vegetative growth of shoots from the rhizomes
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Kelp
Kelp are macroalgae (brown seaweeds) a holdfast attaches the kelp to hard bottoms the stipe provides support allowing the blades to reach the sea surface buoyancy is provided by pneumatocysts
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Macrocystis Life Cycle
Alternation between large sporophyte (diploid, spore-producing) and microscopic gametophyte (haploid, gamete producing) stages Spores settle on bottom, develop into male or female gametophytes Sperm produced by male gametophyte fertilize eggs produced by female gametophytes to produce diploid sporophytes
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Climate Variability and Kelp Ecology
Kelp growth off California depends on upwelling of cold nutrient rich waters Upwelling, in turn, varies with large scale patterns in the winds and ocean circulation Coastal upwelling is associated with along shore winds that blow towards the equator on the west coast of continents
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Coastal Upwelling
occurs as a result of Ekman transport of surface waters the Coriolis force causes surface water movement to be deflected to the right of the direction of the wind in the N. hemisphere (to the left in the S. hemisphere) thus, when winds blow from the N to S off California (or S to N off Peru), the surface layer flows off shore
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What is El Ni~no ?
El Ni~no Southern Oscillation (ENSO) The term El Ni~no was coined in 1891 to describe an event that devastated the Peruvian fishery - warm surface current flowed over the coastal waters off South America near Christmas 1891 - thus associated with Christmas (hence El Ni~no, the (Christ) child) It is a short-term weather disturbance that influences wind patterns, sea surface height and precipitation, and affects marine and terrestrial plant and animal populations
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What is the Southern Oscillation?
a change in atmospheric pressure distributions that accompany El Ni~no normally, atmospheric pressure is - high over the eastern Pacific and - low over the Indian Ocean - prevailing winds blow from east to west
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What happens during a La Ni~na Event?
central Pacific trade winds increase in intensity the South Equatorial current speeds up upwelling of cold, nutrient rich water increases surface waters off Peru & California cool down
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Soft Bottom benthic communities
Soft bottoms are those into which organisms can burrow sand, silt, and/or clay depending on how much water motion there is and the source material for the sediment Exposed places with strong waves have course sand or gravel bottoms Calm, sheltered areas with little wave action often have muddy bottoms Soft bottoms are unstable and shift in response to waves tides currents Sediments may be vegetated (e.g., sea grass beds) or unvegetated (e.g., sands, muds)
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Sediment Characteristics
Sediment is a mixture of inorganic particles decomposing organic mater labile = readily degradable carbohydrates, lipids and proteins, with high extractable energy content (freshly produced) refractory = what is left over after labile material has been extracted - decomposition products including cellulose, chitin microorganisms bacteria, algae, protozoa
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Sediment type affects physical properties
course sediments are well drained and can dry out fine sediments retain water poorly sorted sediments can become water logged O2 (oxygen) content is determined by -the microbial activity (respiration) in the sediment -which consumes O2 and by the extent of mixing which introduces O2 Anoxia develops where -the rate of O2 consumption by respiration exceeds the supply of O2 by percolation of water through the sediment mixing of the sediment by waves or currents Anaerobic bacteria break down organic matter using - sulphate (SO4) instead of O2, - produce hydrogen sulphide (H2S)
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Classification of soft bottom fauna
``` Meiofauna live in the interstitial spaces between sediment grains Macrofauna Where they live: Epifauna live on the sediment surface. Infauna burrow within the sediment How they feed: Predators & scavengers Deposit feeders: Surface feeders Head-down (in sediment) feeders Filter feeders ```
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The main source of organic matter to the bottom is via a Rain of Detritus
faecal pellets, chitinous exoskeletons, and marine snow are produced by plankton in the epipelagic much is remineralized (broken down) along the way by bacteria and meso- and bathypelagic organisms sediment traps (cylinders placed at different depths in the water column) are used to sample this material there is a pulse following the spring bloom in temperate waters it can take months for this material to reach the bottom
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Food Supply to the Deep Sea
Food falls of dead fish and sea mammals provide "hot spots" of activity on the deep-sea bed. Deep-sea fishes and invertebrates can home in on these food falls.
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Hot Vent Communities
high biomass of clams, crabs, mussels, limpets and tube worms most feed on mats and suspensions of free-living sulphide oxidising bacteria dissolved H2S from the vents provides energy that supports these communities chemosynthesis uses the energy from oxidation of H2S to fix CO2 into organic matter
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Zooxanthellae
(zooxanthellae) are essential for reef-building by hermatypic corals corals that lack zooxanthellae are ahermatypic and generally do not form reefs zooxanthellae contribute to success of hermatypic corals by removing CO2 which promotes CaCO3 precipitation providing organic matter to the host zooxanthellae benefit from stable environment freedom from predators nutrients supplied by host
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Factors Affecting Reef Growth
high calcification only occurs in warm water zooxanthellae require light rapid growth is limited to depths <50 m tidal exchange and coastal currents bring nutrients and zooplankton to the reef suspended solids (turbidity) reduce light and smother coral polyps strong waves can damage corals role of tropical storms parrot fish and burrowing/boring invertebrates attack living corals creating rubble
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Types of Coral Reefs
Fringing reefs develop near shore, throughout the tropics, where there is a hard surface for larval settlement. Barrier reefs are separated from the shore by a lagoon. The lagoon is protected from the waves, and has a soft bottom. An atoll is a ring of reef, sand bars and islands surrounding a central lagoon.
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Fringing Reef
``` susceptible to damage by sedimentation, pollution and freshwater runoff. reef flat is sand, mud and coral rubble. living hard corals seaweeds, seagrasses and soft corals. ``` reef crest is subject to intense wave action reef slope is steep with dense coral cover
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Barrier Reef
``` Example: Great Barrier Reef (Australia) consists of back-reef slope, reef flat, reef crest and fore reef slope separated from shore by a lagoon ``` fore reef slope is steep with dense coral cover
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Competition for Space amongst Corals
Fast-growing corals grow up and branch out to collect sunlight also shade their neighbours. Other species attack their neighbours with mesenterial filaments (used for digeston and absorption of prey) or sweeper tentacles that are loaded with nematocysts. The most aggressive species are slow-growing massive corals.
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Food chain
the steps of energy transfer from primary producers through consumers. Energy is lost at each step in a food chain. The longer the food chain, the lower the biomass and productivity of the top carnivores.
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Open Ocean (Pelagic) Fisheries
low primary productivity long food chains to the commercially important top carnivores (sharks, tuna, salmon) Temperate and Equatorial open ocean regions Southern Ocean
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Managing the impact of fishing
Managing effort limiting catch per boat limiting total catch (close fishery once limit is reached) Restrictions on access number of boats length of season size of fish that are allowed to be caught Restrictions on gear power of boats mesh size prohibition of some types of gear
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What is pollution?
The introduction by human activity of substances that decrease the quality of the marine environment An oil spill is pollution, a natural oil seep is not. Humans have affected the entire marine environment from beaches to the deepest oceans.
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Atmospheric deposition
Sources: - Nitrogen oxide from burning fossil fuel - Volatilisation of nitrogen from fertilizer and animal waste - Biomass burning Input via wet (rain) and dry (dust) deposition. This is the primary source of anthropogenic nitrogen into the open ocean
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Land runoff
Fertilizers washed off from agricultural land into rivers High in nitrogen and phosphorus Also toxicants such as pesticides and pesticides Increase in extreme weather events means this is likely to get worse. (Christensen & Christensen, 2003) The primary input into costal systems
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Sewage
Sewage is the wastewater generated by domestic and industrial activity. ``` Contains high amounts of organic nutrients (N and P) and chemical toxicants: Drugs (pharmaceutical & illicit) Cleaning products Heavy metals Pathogens ``` During heavy rain untreated sewage is directly discharged into rivers, and untimely into the marine environment.
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Ecological impacts of eutrophication?
Shift in the balance of an ecosystem from slow growing corals or seagrass to fast growing macro- or microalgae. ``` Algal blooms Increased phytoplankton Increased benthic and epiphytic algae Oxygen depletion Turbid water Decreased biodiversity ```
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Impacts of cultural eutrophication
Harmful algal blooms Toxic algae Shellfish poisoning Anoxic (no O2) or hypoxic conditions (low O2) Fish kills (suffocation) Loss of harvestable shellfish/fish Odour & loss of cultural value H2S is produced when SO42- replaces O2 in the decomposition of organic matter
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Hypoxic zones
In extreme cases eutrophication can lead to permanent or seasonal hypoxic zones. This occurs when large amount of phytoplankton sink and are decomposed by bacteria, depleting oxygen Animals either leave the area or die, undermining ecosystems and fisheries Hypoxic zones are a natural phenomenon but are increasing in size and number
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Effects of microplastics on marine animals
Plastics break down (e.g. exposure to UV) and enter the food chain when consumed by filter feeders such as jellyfish and mussels. Negatively impact fitness due to lack of energy pay off. Toxic additives used in the manufacture of plastics can affect endocrine, reproductive and/or immune systems. They also for agglomerations with other organic pollutants (Pesticides, PCBs) facilitating bioaccumulation in fatty tissues. Plastic pollution has potential to impact biogeochemical cycles such as the biological pump
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Biomagnification
Organic pollutants such as: chlorinated hydrocarbons (many pesticides) polychlorinated biphenyls (PCBs) manufacture of plastics dioxins and furans As they can dissolve in fat they are very persistent once ingested, and are then accumulate up the food web. Due to biomagnification can reach high concentrations in top predators.
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Biomagnification and bioaccumulation def
bioaccumulation is a build up of a given toxin over time due to PROLONGED exposure Biomagnification increases in concentration UP the food web BOTH are dangers to Human Health and Marine Life
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Effects of heavy metals
Direct mortality/toxicity (e.g. copper) Effect sense organs in fish (smell), impacting: -predator avoidance -foraging -schooling -navigation (delayed migration in salmon) -Breeding (finding mates/delayed spawning salmon) Slow growth Increased disease Antibiotic resistance via co-selection
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Noise pollution
Propeller driven ships Oil, & gas uses seismic surveys that create pulses of intense noise. Anti-submarine measures and sonar generate very loud short pulses of sound that may damage the brain and other organs. Offshore construction (e.g. wind farms) requires prolonged pile-driving and underwater use of explosives.
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Thermal pollution
Seawater is used as a coolant in power plants, oil refineries etc. – leading to elevated temperature around discharges. Fish may be attracted to these areas In tropics, most organisms live in waters that are close to their upper temperature tolerance limit. Fish that should migrate don’t, but are venerable to cold shock if the hot water is disrupted Reduces dissolved oxygen levels Localized change in plant communities as macroalgae/seagrass are replaced with phytoplankton
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Radioactive waste
Low level radioactive wastes are discharged to environment, and high levels of radioactivity may be released during accidents. Low-level radioactive waste has been discharged into the Irish Sea from Sellafield since 1952. Greenpeace described the Irish Sea as the most radioactively contaminated sea in the world.
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Impacts of oil pollution: toxicity
Inhibit growth of phytoplankton/primary producers kill invertebrates and fish Increase susceptibility of fish to disease Cause hypoxia and anoxia as oil is degraded (what is this similar too?) Destruction of habitats Bioaccumulation of toxic components from water, sediments, or food. lose their insulating ability, leading to death of mammal and birds due to exposure.
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Microbes matter!
Marine phytoplankton perform 50% of global photosynthetic CO2 fixation They also release CO2! Nutrient re-cycling, underpinning food webs. They are venerable to change: Microorganisms have fast turnover rate, for example compared with trees (days versus decades). how microbial communities have/will respond to change is uncertain
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Sink or Source
The balance between marine microbial autotrophy and heterotrophy will be of key importance with a changing climate - (Sarmento, Philos Trans R Soc B Biol Sci . 2010). There is evidence that the balance may shift towards heterotrophic processes as the climate warms - (Vaqué, Environ Res Lett 2015; 10) This could result in a feedback loop between CO2 production and microbial heterotrophic activity!
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Effects of ocean acidification on Fish
Lower pH of fish blood (acidosis). This costs energy to correct and reduces fitness. Changes in behavior e.g. reduced predator avoidance and have trouble navigating. (See Moodle for the debate) corrosion of placoid scales in sharks
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Changes in habitat due to acidification
Tropical seeps dead reef substratum (yellow) is eroded structural complexity of living corals declines algae proliferate sub-tropics loss of hard coral/coralline algal cover diverse macroalgal communities replaced by turf algae. temperate coasts loss of brown algal canopy cover. coralline algae decline as turf algae proliferate In each case, calcified invertebrates (sea urchins) become fewer and smaller
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Problems with the data used for fishery management
Difficult to assess stock size because of patchiness in distribution differences in efficiency of capture methods intermixing of stocks on feeding grounds Usually assessed by landings divided by effort (Catch per Unit Effort = CPUE) which reflects population size spatial distribution of the population intensity of fishing effort number of fishing boats, their size and fishing hours However, fishing is not random Effort and catch are self-reported by fishers verified (sometimes) by inspectors