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Certain small fish - planktonic stage |
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active swimmers, ex. fish, sea turtle Incapable of sustained, direct horizontal movement |
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about 47% of global primary production only 0.2% of the earth's biomass |
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Eukaryotes: Division Chromophyta Class bacillariophyceae (Diatoms) |
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Important in coastal areas and spring blooms Require silicon; silica frustule |
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Usually marine form Radial symmetry |
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Usually shallow and freshwater form Bilateral symmetry |
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Single-celled 2 flagellae Bioluminuscent Harmful algal blooms 6-8 million/l |
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Red tides Toxic Can cause fish kills
When they are very abundant: 1. Shading (blocking the sunlight) 2. Oxygen depletion (excessive respiration or decomposition) 3. Mechanical irritation (damaging fish kills) |
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SI based Made of silica Round - usually water column Pennate - Usually benthic (on the bottom) |
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Dino=whip
Made of cellulose
Some photosynthesize Some eat other phytoplankton Some live symbiotically with other organisms (Dinoflagellates in corals. Coral bleaching: Dinoflagellates leave) |
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Made of calcium carbonate Plates on them called coccoliths. 10-100 of them Coccolithophores make milky water: Huge blooms. Control their own population with gas clouds White cliffs of Dover made of coccolithophores |
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Too much of a good thing (phytoplankton) |
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1. Shading (blocking the sunlight) 2. Oxygen depletion (excessive respiration of decomposition) 3. Mechanical irritation (damaging fish gills) |
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is naturally-occuring, higher-than-normal concentration of the microscopic algae Karenia brevis (formerly gymnodinium breve) Produces a toxin that affects the central nervous system of fish so that they are paralyzed and cannot breathe. As a result, red tide blooms often result in dead fish washing up on beaches. When red tide algae reproduce in dense concentrations or "blooms," they are visible as discolored patches of ocean water, often reddish in color
Red tide affects human in more than one way. Red tide can cause respiratory problems, rashes, and irritation of the eyes, nose, throat, lips, and mouth. |
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Other classification of plankton |
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Holoplankton - Entire lives as plankton (phytoplankton etc.) Meroplankton - Part of their lives as plankton, juvenile or larval stages Macroplankton - Large floaters such as jellyfish or Sargassum Picoplankton - Very small floaters such as bacterioplankton |
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-On the bottom (epifauna) -Within the bottom sediments (infauna)
Some organisms cross from one lifecycle to another during their life, for example being planktonic early in life and benthic |
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Classification by habitat and mobility |
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Plankton (floaters) Nekton (swimmers) Benthos (Bottom dwellers) |
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1,750,000 world species 86% land species 14% marine species
250,000 marine: 98% benthic 2% Pelagic
The reason in the book: The marine world is more stable - more unstable = more areas to adopt to |
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Organic matter synthesized from inorganic substances |
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Producing organic matter from carbon dioxide and water using light energy
Carbon dioxide + Water + Light --> Organic matter + Oxygen 6CO2 + 6H2O + Light --> C6H12=6 + 6O2
Photosynthesis consumes CO2 and produces O2 |
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What limits primary production in the ocean? |
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Most common limiting factors: Light and Nutrients |
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Euphotic (eu=good) - rarely deeper than 100m; photosynthesis takes place Disphotic = euphotis to 1000m;small but measurable amounts of light Aphotic = dark
Penetration of different wavelengths
PAR: Photosynthetic active radiation (400-700nm)
45% 1m down 16% 10m down 1% 100m down - Called the one percent light level |
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Carbon: important but abundant in seawater Nitrate (NO3-), Nitrite (NO2-), Ammonium (NH4+) Phosphate (PO4 3-) Silicate (SiO4)
106CO2 + 16NO3- + PO4 3- + 122H20 + 19H+ + Light --> (CH20)106(NH2)16(H3PO4) + 138O2
Redfield ratio: C:N:P = 106:16:1 (in phytoplankton) |
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Justus von Liebig "Father of pertilizer industry" |
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1803-1873
Leibig's law of the minimum (for oceans):
Phytoplankton growth is determined by the response of the phytoplankton to the single factor that is most limiting
These factors include N, P, Fe, Si and other trace materials |
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Euphotic zone: Photosynthesis > Respiration
Compensation depth
Export: Marine snow Aggregates Fecal pellets
Photosynthesis < Respiration |
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Organic matter + O2 --> CO2 + NO3 + PO4 + H2O
Respiration (remineralization, regeneration, degradiation) -Consume oxygen Produces carbon dioxide -Regenerate nutrients |
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Oxygen minimization layer - depleted by photosynthesis
Nutrient maximum - remineralization
Down in ocean: Nutrient remain high, O2 high - decause its replenished with hight oxygen cold water from polar regions |
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Vertical distribution of nutrients |
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Depleted in surface water, abundant in deep water |
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Primary production by phytoplankton |
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CO2 enter the ocean Nutrients adds Goes to phytoplankton
50 times more inorganic carbon in the global ocean than in the atmosphere |
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Cold water hold more gas, CO2 enter the ocean at the pole Water sinks into the deep ocean layer Rises to the surface at the equator and outgasses |
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Gas exchange allows CO2 to enter ocean |
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-Flux depends upon air-sea CO2 difference -Solubility increases in cold water (polar region are sinks, equatorial sources) |
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Combined biological processes which transfer organic matter and associated elements to depth - pathway for rapid C sequestration
Quickly remove C from surface ocean &atm |
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What controls carbon export? |
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Biological pump and the ocean C sink- an inverted pyramid
Carbon uptake Carbon flux - 100m Farbon flux 1000m Carbon burial |
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What controls algal primary productivity? |
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Temperature Light (via solar angle and or mixing Major nutrients (N, P, Silica) Grazing Micro-nutrients (Iron) |
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What are minor nutrients? |
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Iron (Fe), Zinc (Zn)..... |
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Vertical profiles of elements in the north pacific ocean |
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Fe and Zn profiles are similar to those of the major nutrients (depleted in the surface, abundant in the deep), unlike Na & Cl |
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Since algal growth is limited by the resource that is in smallest supply relative to its needs, it was hypothesized by John Martin that iron was limiting phytoplankton growth in open-ocean environments
"give me a half a tanker of iron, and I will give you an ice age" |
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Enrich a small area of the ocean by adding iron along with an inert and sensitive tracer
Follow what happens through time by ship-board measurements and satellite observations
Experiments have been to date conducted in the equatorial pacific (2), north atlantic (1) and southern ocean (4)
Varying responses have been seen... Sometimes plankton bloom, sometimes they don't However, little or no increase in carbon expert was observed
IronEx-1: No phytoplankton biomass increase, rapid increase in photosynthetic capacity IronEx-2: Increase in biomass, productivity EisenEx: Small increase, but then a storm came SOIREE: Clear increase, long-lived effects, unusual iron chemistry SEEDS: massive bloom SOFeX: Small bloom |
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So what does it all mean?
Possible side effects
Why does this matter? |
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Twelve small-scale experiments over the past decate in several ocean locations consistently showed that intentional iron additions do result in phytoplankton blooms
Previous studies of artificial and natural blooms have shown wholesale changes in the species that make up the two lowest links of the marine food chain - phytoplankton and the bacteria that feed on them
Phytoplankton are the base of the food chain - change them and you could see repercussions all the way up the food chain..so is this good or bad? |
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Other possible side effect |
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When a plankton bloom runs its course and the organic material that is produced sinks to deeper waters, the resulting bonanza and decomposition uses up oxygen in the water
Dead zone formation: 1. Fresh water runoff create barrier, cutting off saltier water below from contact with the air 2. Nitrogen and phosphorous from fertilizer in the freshwater layer ignite huge algae bloom. they die and sink to the saltier water below. 3. Starved of oxygen and cut off from resupply, the deeper water becomes a dead zone. Fish avoid the area or die in massive number |
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SeaStar satellite/SeaWiFS view of ocean chlorophyll and land vegetation |
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Most along equator and in north/south, less right next to equator
Upwelling areas: California, Peru, south Africa, canary islands, west coast of Australia Therefore, very productive areas Cooler, deeper seawater |
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regional primary productivity |
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Varies from very low to very high depending on: Distribution of nutrients and seasonal changes in solar radiation About 90% of surface biomass decomposed in surface ocean About 10% sinks to deeper ocean Only 1% of organic matter not decomposed in deep ocean Biological pump (CO2 and nutrients to sea floor sediments) |
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Primary productivity Polar oceans |
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Nutrients are abundant due to vertical mixing Limited by sunlight: darkness for winter months Partly covered by sea ice
Most diatom biomass in April/May, slowly decreasing until jan, then faster increasing Most zooplankton biomass in aug, faster decreasing until Dec, then slow increasing |
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Availability of sunlight High nutrients due to upwelling of north atlantic deep water -no thermocline -no barrier to vertical mixing |
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tropical ocean productivity |
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Permanent and strong thermocline is barrier to vertical mixing Low rate primary productivity (lack of nutrients) High primary productivity in areas of Equatorial upwelling Coastal upwelling Coral reefs (Symbiotic algae and recycle nutrients within the ecosystem) |
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Short essay question
Primary productivity Polar oceans: |
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Nutrients are abundant due to vertical mixing Limited by sunlight: darkness for winter months Partyly covered by sea ice
Diatom biomass peaks in spring, slowly decreases, then rapidly increasing Zooplankton peaks in early summer, then rapidly goes down Know how to draw the diagram |
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Strong and permanent thermocline Production is limited by lack of nutrients Exceptions: Equatorial upwelling, coastal upwelling, coral reefs (organisms are adapted to low-nutrient conditions and recycle nutrients) |
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Seasonal Thermocline development |
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Stratification: Feb-Aug De-stratification: Sept-Dec |
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Primary productivity in temperate oceans |
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Winter: Lowest sunlight, highest nutrients Spring: Increasing sunlight, decreasing nutrients Summer: Highest sunlight, lowest nutrients Fall: Decreasing sunlight, increasing nutrients
Spring bloom: Abundant nutrients due to vertical mixing in water Higher solar energy available Stratification traps algae in the euphotic zone Spring bloom dies as nutrients become depleted and phytoplankton is consumed by zooplankton
Fall bloom: Nutrients come back due to break down of thermocline Short Not as dramatic as spring bloom |
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Primary productivity in temperate oceans |
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Winter: Lowest sunlight, highest nutrients Spring: Increasing sunlight, decreasing nutrients Summer: Highest sunlight, lowest nutrients Fall: Decreasing sunlight, increasing nutrients
Spring bloom: Abundant nutrients due to vertical mixing in water Higher solar energy available Stratification traps algae in the euphotic zone Spring bloom dies as nutrients become depleted and phytoplankton is consumed by zooplankton
Fall bloom: Nutrients come back due to break down of thermocline Short Not as dramatic as spring bloom |
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Yearly fluctuations in different types of fish is due to if they match the blooms or not |
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Primary productivity
Aquatic vs Terrestrial |
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60% of global production is in oceanic water Picoplankton can contribute |
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Algae-supported biotic community |
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Sun Radiant energy (sun)---> Producers (sea grass) Chemical energy --> Fish Fish (consumer)---> Heat energy ..... |
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Nutrients cycled form one chemical form to another Biogeochemical cycling Example, nutrients fixed by producers Passed onto consumers Some nutrients released to seawater through decomposers Nutrients can be recycled through upwelling |
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Producers - Herbivores - Carnivores Chemical energy transferred from producers to consumers Also lose energy Feeding stage is trophic level About 10% of energy transferred to next trophic level |
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Transfer of energy is very inefficient One exception: Sunlight to phytoplankton: 2%
500,000 units of radiant energy-->10,000 unites of plankton --> 1000 units of lever 2 --> 100 units of small fish --> 10 units of fish --> 1 unit of radiant energy equivalent converted to human mass |
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Three orders: 1. Carnivora 1a Pinniped 2. Sirenia 3. Cetacea 3a Odontoceti 3b Mysticeti
Definition of mammal 1. Warm blooded 2. Breathe air 3. Have hair or fur at some stage of development Bear live young 5. Females have mammary glands that produce milk
Approximately 116 species of marine mammals |
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Prominent canine teeth Skin covered flippers Examples: Sea otters (no blubber, dense fur, eat various shellfish and crustaceans, kelp beds) Polar bears - Webbed paws, thick and hollow hair, eats mainly seals |
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Short fur Vibrissae For flippers All of them are very social, although to varying degrees Examples: Seals Sea lions Fur seals |
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Sea lion and fur seal Small slim head External ear flaps Long and wing-like front flippers, usually hairless, no noticable nails Hind flippers: Large and paddlelike, ahirless, webbed
Seal Tiny ear holes, no ear flaps Short and blunt front flippers, covered with hair, clawlike nails on digits Hind flippers: Short and paddlelike, covered with hair, nails on all digits
Walruses m/f have tusks (1m) Eat benthic organisms Sensitive hearing
Sea lions (and fur seals) vs. seals Have external ear flaps Longer flippers (they can awkwardly walk) Almost non-existent claws/nails
California sea lion Opportunistic feeders Found in the western pacific (California and south to the Galapagos) Incredibly common (found in groups of hundereds)
Harbor seals Shy and quiet Only social during mating and resting Likes to haul out on sandy beaches or on small rocks Haul out in large groups Found all over the world Eat mostly fish
Seals on the cape Harbor seal Grey seal
Elephant seals There are two species: Northern and southern Bulls - 16ft (5m) and 6,000lb Cows - Measure about 10ft (3m) and 2,000lb The largest known bull elephant seal weighted 5000 kg (11,000lb) and measured 6.9m (22.5ft) in length This makes elephant seal the largest member of the order Carnivora
Southern elephant seal Males up to 3000-4500kg Very aggressive Dive to 1900m
Leopard seal Second largest species of seal in the Antarctic (after the southern elephant seal), and is near the top of the antarctic food chain Highly evolved for its role as keystone predator Shallow water hunter They do not dive deep
Northern fur seal Found throughout the northern pacific Solitary, except when mating or nursing their young Remain in the water except for mating Eats most types of fish Have extremely long hind flippers Only 15 in captivity
Walruses Neither seal nor sea lion, they have their own group Found in the arctic, on shallow-water ice floes Have tusks up to 1m long Males can grow about 3m long Usually reddish to a pale grey Feed mostly on echinoderms |
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Manatees - Coastal areas of tropical atlantic ocean Dugongs - Tropical indian and western pacific ocean The only vegetarian marine mammal; shallow water grasses Florida/Antillean/west african/amazonian manatee |
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Elongated (telescope skull) Blowholes on top of their skull Very few hairs Horizontal tail fin Swim fast because the elongated body and their skin Deep diving |
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Prominent teeth Complex and long lived social groups One blowhole Best sound developments Good vision - but uses echolocation |
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Suborder: Odontoceti - teeth (spade shaped), single blow hole Family delphinidae Risso dolphin - no beak Bottlenose dolphin Common dolphin: Slender, not robust, distinct side markings, defined break, often travel in huge herds (1000+), Beak, Pronounced, curved fin |
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Suborder: Odontoceti - teeth (spade shaped), single blow hole Family Phocoenidae No beak, small and rounded head, well... |
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There are two types of chemical weathering, name one: |
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Congruent and incongruent |
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Photosynthesis Respiration |
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Photosynthesis: CO2 + Light + nutrients --> O2 + Organic matter
Respiration: O2 + Organic matter (C:N:P, 106:16:1, Redfieldz) --> CO2 + Nutrients |
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Macro nutrient: N, P -needed in higher amount Micro nutrient: Fe, Zn -needed in lower amount |
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Where O2 is lowest and nutrients highest |
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No dominant process in the deep ocean, so the nutrient concentration stays high. O2 increases because warm water from the equator goes up to the poles, gets cold, holds a lot of O2 and sinks down and back to the equator. (Also lower respiration rates) |
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: Congruent weathering results in |
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A) Rib tides B) Dissolved ions C) Erosion D) All of the above |
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Congruent vs Incongruent Weathering |
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Congruent weathering Dissolved ions
Incongruent weathering Dissolved iond + particles |
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Wind, water, pressure, temperature, precipitation, animals Surface area increases |
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Plankton Holoplankton Meroplankton |
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Plankton "Aimless wanderer" (Opposite: Nektons "active swimmers")
Holoplankton Entire life as plankton
Meroplankton Part of life as plankton |
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QUESTION: The Redfieldz ratio is |
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1) 106 carbon:15N:12 2) 601:61:1 3)106 carbon:16N:1P: 4) Who cares |
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Fe increase phytoplankton growth, and eventually increase CO2 drawdown in the ocean |
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There are different ones, which is dominent, what forces causes them. Know the bigger picture: Neap, spring, lunar day |
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Animals of the pelagic environment |
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Phytoplankton live in the sunlit surface waters; therefore...many marine animals live there too!
Pelagic organisms live suspended in seawater and comprise a VAST majority of the ocean's biomass
Biomass - The mass of living organisms
Pelagic organisms tend to be more dense and have less surface area to volume per unit of body mass, so they tend to sink more rapidly than phytoplankton. |
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How do pelagic marina animals remain in the water column? |
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-Containers of gas -Soft bodies, void of high density hard parts -Swim |
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Range in size - microscopic (ex. copepod) to large (ex. jellyfish) Copepod has a hard shell or test Larger (ex. jellyfish) has soft gelatinous bodies
Collectively called zooplankton Comprise second largest biomass in the ocean Most are herbivores, some are omnivores |
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Radiolaria illustration from the Challenger expedition 1873-1876
Amoeboid protozoa Productive intricate skeletons (made of silica) Found throughout the ocean Skeletal remains cover large portions of the ocean floor (known as radiolarian ooze) Rapid turn-over of species |
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Most abundant - Planktic Most diverse - Benthic Shells made of calcium carbonate |
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Group of small crustaceans Every sea and almost all freshwater habitats Constitute the biggest source of protein in the oceans Many species are planktonic, but more are benthic Some continental species may live in limno-terrestial habitats and other wet ....
Extremely numerous... In fact, they are one of the most numerically dominant types of multicelled organisms on the planet |
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Air is about 1000x less dense than water at sea level Rigid gas container and swim bladder --> neutral buoyancy Amount of air in their bodies regulates density, so they can remain at a particular depth |
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Chambered shell Internal chambered structured Pressure in shell - air at atmosphere Therefore, must stay above 500m or its shell will collapse |
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Osteichthyes - Bony fishes |
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Has bones Has a swim bladder Has gill covers Has scales
Is the largest class of vertebrates in existence today 1. Ray-finned fish (Actinopterygii) - 95% of all fish 2. Lobe-finned fish (Sacropterygii) |
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Condricthyes - Cartilaginous fishes |
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No bones No swim bladder 5-7 gill open gill slits No scales Three main types: Sharks Rays Chimaeras Sharks and rays called elasmobran.... |
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Also called swim bladder or fish maw Low density Adjustable Most ostei... (bony fish) Lost secondarily in some species |
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