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88 Cards in this Set

  • Front
  • Back

unifying underlying mechanisms of species

1. capturing and storing energy


2. manufacturing proteins


3. transmitting info between generations

evolution

maintenence of life under changing conditions by continuous adaptation of successive generations of a species to its environment

Darwins Natural selections (5 steps)

1. more offspring are produce then can survive


2. random variations occur (some inheritable)


3. some inheritable traits make an organism better suited to its environment


4. favorable traits accumulate; unfavorable traits weeded out by competition


5. physical and biological environemnt does natural selection

spontaneous mutation

inheritable change in an organism's genes (usually unfavorable)

adaptation

accumulation of eneficial interitable

nucleic acids

use sequences of these molecules to determine organisms genetic heritage


3 domains

1. bacteria


2. archaea


3. eukarya

bacteria

lack distinct compartments within their cells


no cell nucleus or organelles (prokaryote)


(some photosynthetic, some heterotrophic)


heterotrophic: decomposers and disease agents

archaea

lack distinct compartments within their cells


no cell nucleus or organelles (prokaryote)


some are extremophiles


share many biochemical characteristics as eukarya

eukarya

cells with a nucleus (eukaryotes)


multicellular


some protists, all animals and plants


scientific name

genus + species name

living vs. non living

1. ability to capture, store, and transmit energy


2. ability to reproduce

Photosynthesis

CO2 + H20 --> (CH20)x + O2


energy from sunlight used to bond six separate carbon atoms (derived from CO2) into single energy rich six carbon molecule (glucose)


pigment chlorophyll absorbs and briefly stores light energy


water broken down and oxygen released


dominates ocean surface productivity


in vents: vents radiate dark red light

Chemosynthesis

CO2 + H2S --> (CH20)x + (SO42) (sulfate)


6 molecules of CO2 combine with 6 molecules of oxygen and 24 molecules of Hydrogen sulfide to form glucose


energy to bond carbon atoms into glucose comes from breaking chemical bonds holding sulfur and hydrogen atoms together in hydrogen sulfide (oxidation of inorganic molecules)


where: hydrothermal vents, deep in marine


sediments


chemosynthic extremophiles mostly in archaea domain

primary producers

chlorophyll in these organisms trap light energy and change to chemical energy


breakdown food and produce waste heat


size: 10x mass of carbon it has bound into carbohydrates

consumers

eat primary producers for energy

primary productivity

gC/m2/yr (grams of carbon bound into organic material)


organic material produced: carbohydrate glucose


1. phytoplankton: 90-96%


2. seaweeds: 2-5%


3. chemosynthetic organisms: 2-5%

total ocean productivity

75-150gC/m2/yr


rapid turnover time compared to terrestrial productivity

heterotrophs

consumers

autotrophs

primary producers

top consumer

top carnivore

trophic pyramid

feeding hierachy:


each level is about 1/10 the mass of the level directly below

which 4 elements make up 99% of mass of all living things

Carbon, oxygen, hydrogen, nitrogen

classes of biological chemicals (by combining major elements)

carbohydrates, lipids (fats, waxes, oils), proteins, nucleic acids (DNA)

representative use of Nitrogen

proteins, nucleic acids, chlorophyll

dissolved CO2 forms:

HC03


carbon dioxide converted to into bicarbonate ions and incorporated into shells of organisms


shells compress to form limestone

carbon and carbon cycle

can form long chains to which other atoms can attach


basic building block of life


CO2 can easily dissolve in water


carbon release: respiration of living organisms, volcanic eruptions, burning fossil fuels

MICROBIAL LOOP (of carbon)

DOC - bacteria eats - protozoans eat - zoo plankton eat


<1% CaCo3 (calcium bicarbonate) from shells sink to seabed

Nitrogen

48% of dissolved gases in seawater


organisms cannot use free nitrogen --> must be fixed with oxygen or hydrogen first by specialized organims (ex. ammonium & nitrate)


ocean regions frequently nitrogen limited

why coastal waters support more plankton than open ocean

nitrate runoff provides nutrients

physical factors:

1. light


2. temperature


3. dissolved nutrients


4. salinity


5. dissolved gases


6. acid-base balance


7. hydrostatic pressure

biological factors

1. diffusion


2. osmosis


3. active transport


4. surface-to-volume ratio

depth of penetration of light depends on

low angle reflects (sunrise/sunset, polar regions)


blue light penetrates to greatest depth


red light absorbed near surface


# particles (lots of particles absorb blue light and combine with green reflection from chlorophyll --> green coastal waters)

light zones


1. photic: euphotic zone to about 70 m (photosynthesis and vision)


2. photic: disphotic zone to about 600m (vision only)


3. aphotic zone below 600 m (no sunlight)

ectothermic

"cold blooded"


most marine organisms


internal temp about same as surroundings


can tolerate a narrow range of external temp

endothermic

"warm blooded"


stable, high internal temp


can tolerate extreme range of external temp


thermal regulation mechanisms


high metabolic rates


high demands of food supply and gas transport

How does dissolved CO2 influence ocean's acid-base balance

strong acids/bases distort enzymes and proteins


affects formation of calcerous materials (shells)


seawater slightly alkaline (ph 8)


much less variable than soil


some dissolved CO2 becomes carbonic acid and can lower pH of water


respiration increases Co2


photosynthesis decreases Co2

diffusion

substance distributed evenly in water


warmer water, faster diffusion


transfers material from region fo high concentration to region of low concentration


osmosis

diffusion of water through a membrane


most simple marine organisms are isotonic (same concentrations of dissolved substances as sea water0


hypotonic: water moving in


would be hypertonic (water moving out) in freshwater (water would flow out of cells causing organism to dehydrate and collapse

marine environment's distinct zones

pelagic: open water


- neritic (nearshore over continental shelf)


- oceanic zone beyond continental shelf


- epipelagic zone (lighted photic zone)


- mesopelagic (aphotic)


- bathypelagic (aphotic)


- abyssopelagic (aphotic, in deep trenches)


benthic: bottom divisions


- litteral zone (intertidal)


- bathypelagic zone (sea bed on slopes down to great depths)


- abyssopelagic zone


- hadal zone (deepest seabed, trench walls and floors)


plankton common feature

inability to move consistently laterally through the ocean (many move vertically through water column)


grazing


predation


paratism


competition


phytoplankton

autotrophic


euphotic zone


generate lots of atmospheric oxygen through photosynthesis

picoplankton

.2-2 micro meters


extremely small


many cyanobacteria


100 million in every liter of seawater

cyanobacteria

autotrophs


absorb dim blue light in deep euphotic zone

Viruses:


1. bacteriophages


2. phycoviruses

1. viruses that infect bateria


2. viruses that infect phytoplankton



no metabolism; must rely on hosts for energy-requiring processes like reproduction

diatoms

increase proportion of free oxygen in Earth's atmosphere (excess oxygen released through perforations n frustule into water)


cell wall: frustule consists of silica divided between 2 halves (valves)


efficient energy conversion (clear protective window like glass)


besides pigment chlorophyll, also acompannied by yellow or brown pigments that store energy as fatty acids and oils (since these are lighter, easier to float)



dinoflagellates

single-celled autotrophs


live free in water


flagella: two whiplike progections; adjust orientation and vertical position for best photosynthetic use of light


bioluminescence


responsible for HAB (harmful algal bloom) "red tide"


HABS can be dangerous: potent toxin by-products of metabolism

coccolithophores

small, single celled autotrophs


disks of calccium carbonate fixed to outside of cell walls


live near surface in brightly lighted areas (translucent cell coverings shade cell)


milky or chalky Mediterranean and Sargasso seas


build seabed deposits of ooze

4 main ingredients to produce carbohydrates

1. water


2. carbon dioxide


3. inorganic nutrients


4. sunlight

role of nutrients

construct large organic molecules that make primary productivity possible


construct skeletons and protective shells

nonconservative nutrients

change in concentration with biological activity


nitrate


phosphate


iron


silicate

exchange of nutrients (from high to low concentrations)

upwelling


high in antarctic


relatively high where there is little or no thermocline


low in tropical ocean (with distinct horizontal layers) --> clear blue ocean


red light

abosrbed by chlorophyll and converted into heat near ocean's surface


compensation depth

where production equals consumption


break even depth marks bottom of euphotic zone


diaton depth>dinoflag depth b/c of greater efficiency


open tropical seas have deepest depths but lack nutrients

most abundant zooplankters

microflagellates


microciliates

copepods

70% of larger consumers


shrimplike animals


crustaceans (like crabs, lobsters, and shrimp)

largest zooplankton

giant jellyfish

macroplankton

plankton larger than 1 cm

holoplankton

spend whole lives in plankton community

meroplankton

later adopt a benthic or nektonic lifestyle

krill

pelagic (near shore or bottom) arthropod (exoskeleton)


keystone of antarctic ecosystem


Weddell Sea


daily vertical migration


planktonic foraminifera

snare food with long protoplasmic filaments


have calcium carbonate shells

adaptations of seaweeds to environment

flexible bodies


easily able to absorb shock


resistant to abrasion


streamlined to reduce water drag


very strong


rare in warm nutrient poor waters


most in chilly temperate and subpolar zones of nutrient upwelling


because of weak anchorage, sandy or muddy bottom unsuitable

marine vascular plants

descended from land ancestors and live in shallow coastal water


sea grasses


mangroves

oxygen revolution

2 billion - 400 million years ago


first organisms absorb organic molecules formed spontaneously in ocean


more organisms --> more competition for food


food would run out without photosynthesis because primary producers convert inorganic molecules to organic molecules for food


first animals: single celled organisms


autotrophs (probably cyanobacteria) change amount of free oxygen in atmosphere from 1% to 20%



ozone layer derived from this oxygen

invertebrates

more than 90% of all living and fossil animals


rigid internal skeleton for attachment of muscles


protective outer covering (continuous or segmented)

Phylum porifera

invertebrate


sponges


10,000 species


suspension feeders: strain plankton from water


diffusion: excretion and movement of gasses in and out of animal


diagram on pg. 441


skeletal network of spicules (needles) of calcium carbonate (CaCo3)

Phylum Cnidaria

coral, jellies, sea anenomes, siphonophores


cnidoblasts: large stinging cells that eject coiled threads to poison and entangle prey


2 body plans: medusa (bell shaped + tentacles) and polyp (no skeleton; sea anenomes + corals)


symbiotic photosynthetic zooxanthellae


ex. hermatypic coral (mound builders) w/ masses of symbiotic dinoflagellates within host


--depend on light and warmth (clear water best)


--mucous coating "suntan lotion"


-- prefer slightly elevated salinity


2 structural cell layesr: inner partition and epidermal tissue

worm body plan

bilateral symmetry


head


waste and digestive system


phylum platyhelminthes

flatworms: simplest worms


some parasitic of vertabrates


shady underside of intertidal rocks


most primitive organism w/ central nervous system


light-sensitive eyespot


no excretory or respiratory system - use diffusion to eliminate waste

phylum nematoda

round worms


flow-through digestive system (mouth and anus)


most are free-living and microscopic


in garden soil and marine sediments

phylum annelida

segmented worms


metamerism: segmentation; convenient strategy to increase size


most evolutionary advanced worms


each segment has their individual systems

phylum polychaeta

many bristles


largest, most important and most diverse class of annelids


brightly colored


iridescent worms


pairs of bristly projection


well developed heads with prominent sense organs


efficient predators

phylum mollusca

"soft bodied"


chitons, snails, bivalves, copepods, krill


external or internal shell


bilaterally symmetrical


obvious heads


flow through digestive tracts


well-developed nervous systems


exhibit great structural diversity


3 classes: Gastropoda, Bivalvia, Cephalopoda

phylum mollusca class gastropoda

snails


inhabit large shells (largest class)


rocky bottoms and firm substrates


shells coiled to compress mass and allow for easier maneuverability


3 layers of shell


- fibrous outer covering (distribute shock)


- strong crystalline layer of calcium bicarbonate (strength)


- inner layer of smooth CaCo3


gastropod foot cannot attach to sand or mud


bivalves surrender mobility for protection and suspension feeding


most evolved: cephalopods


- head surrounded by foot divided into tentacles


- catch prey with suction cups


- ex. squid and octopuses


- clouds of ink to confuse predators


phylum arthropoda

lobsters, shrimp, crabs, krill, barnacles


most successful animal group


body plan: clear segmentation with pair of appendages per segment


bilaterally symmetrical


exoskeleton made of chitin (nitrogen rich carbohydrate), strong, lightweight


--> shed (aka molted) at regular intervals


striated muscle: quick, strong, lightweight


articulation: ability to bend appendages at specific points


largest class: crustacea

class crustacea, phylum arthropoda

largest class of arthropoda


ex. shrimp, crab, krill, barnacles


16-20 segments


appendages specialized for sensing


70% are copepods that graze on diatoms and dinoflagellates


largest: king crab

Phylum Echinodermata

exclusively marine


lack eyes or brain


radially symmetrical


5 sections or projections


move slowly


3 most familiar classes:


1. asteroidea


2. ophiuroidea


3. echinoidea

phylum echinodermata, class asteroidea

seastars


5+ arms


spiny projections on top


delicate tube feet underneeth


water-vascular system: complex filled water canals, valves, for locomotion and feeding


expels its stomach from mouth to eat

phylum echinodermata, class opiuroids

brittle starts


long slender arms


can detach arm to escape from predator


beneath intertidal and subtidal rocks

phylum echinodermata, class echinoids

"hedgehog"


five-sided symmetry overlain by a few bilaterally symmetrical features

phylum chordata

includes both vertebrate and invertebrate classes


stiffening notochord (internal mechanical foundation for skeletal and muscle development)


tubular dorsal nervous system


gill slits


5% loves notochord as they develop: invertebrate chordates


95% vertebrate chordates (fish, reptiles, birds, mammals)

tunicates

invertebrate chordates have these suspension feeders that superficially look and function like sponges


mucus nets trap plankton


salps: take in water, filter it, and expel it on other end

vertebrate chordates

have internal skeleton or calcified bone or cartilage provides support during growth


skull: brain, eyes, other sense organs --> intelligence


pairs of nerves passing between vertebral segments


successful: fish


least successful: amphibians

fish

ectothermic (cold blooded)


most numerous on bottom or in productive seawater over continental shelves


first fishes without jaws


earliest jawed fish had paired fins to stabilize movement

phylum chordata, class chondrichthyes

sharks, skates, rays


skeleton made of cartilage


no true bone, despite some calcification of cartilate


jaws with teeth


paired fins


active lifystyle


sharks


phlyum cordata, class chondrichthyes

most dangerous: great white sharks


- open water, sense water vibrations w/ sensitive organs


- genus carcharodon


largest: whale sharks


- genus Rhincodon


- 18 meters


- docile, no threat


- eat plankton w/ gill rakers

phylum chordata, class osteichthyes

hard, lightweight, strong skeleton


most numerous of fish most abundant found in almost every marine habitat


order Teleostei: cod, tuna, halibut, goldfish


- independently movable fins


- great speed


- highly effective camouflage


- social organization


- orderly patterns of migration