-
Ancient Pacific Islanders
- - had detailed knowledge of marine life
- -used clues such as wind, wave, and current patterns to navigate
-
Phoenicians
- -The first accomplished western navigators
- - by 2000 B.C they were sailing around the mediterranean sea, black sea, atlantic ocean
-
ancient greeks
- -Had considerable knowledge of nearshore organisms in te mediterranean
- -Greek plates with marine organisms on them
- -Electrical stimulation therapy form an electrical ray
-
who is considered to be the first marine biologist?
- aristotle
- -described many forms of marine life
- -recognized that gills are the breathing apparatus of fish
-
James Cook
- 1. Arctic to Antarctic
- 2. Alaska toAustralia
- 3. naturalist
- 4. chronometer: determine longitude
-
Darwin
- -Sailed around the world on the HMS beagle
- -Explained the formation of distinctive rings on coral reefs called atolls
- -Captured plankton, barnacles
- -natural selction and evolution
-
Wilkes expedition
- -US government funded
- - 10,000 biological specimens
-
Edward Forbes
- -discovered many unknown organisms
- -recognized that sea floor varies at different depths
- -inspired the Challenger expedition
-
HMS Challenger Expedition
- -British navy suppled a light warship
- -brought back themost information that had ever been recorded in previous history
- -laid foundations of modern marine science
-
The first major american marine laboratory
Marine Biological Laboratory at Woods Hole, Massachusetts
-
Sonar
- Sound navigation ranging
- -developed in WWII in reponse to submarine warfare
- -detection of underwater echoes
-
Modern Marine Biology
- 1. Scuba
- 2. Research vessels
- 3. Remote sensing technology
- 4. Robots
- 5.Critter cams
-
Scientific Method
- 1. Observations
- 2. Questions
- 3. Testable Hypotheses
- 4. Experiments
- 5. Analysis of Results
-
Theory
- explanation supported by reasearch and evidence
- -still subject to revision
-
Anatomy of the Earth
- Crust: outermost, extremely thin
- 1. Lithosphere
- -brittle
- -oceanic(basalt) and continental (granite) plates
- 2. Mantle
- -Upper: Asthenosphere
- -Lower
- 3.Core
- -Hot
- -Iron/nickel
- -Outer: molten mateiral
- -Inner: solid
-
Mid-ocean ridge
continous, submarine range of volcanic mountains that runs through all ocean basins
-
How is the surface of changing?
- 1. Seafloor Spreading
- New ocean floor is made at the ridge center and becomes progressively older moving away from the ridge.
- 2. Erosion/weathering
- 3.Volcanoes
- 4.Earthquakes
-
What forces are driving these changes? (seafloor)
- Cooling oceanic plate(Slab pull) and Convection currents
- -molten material rises from the mantle, spreads the plates apart -cools and spreads, pulls the plate along with it
- -eventually sinks back down and destroyed at trenches
-
How do these changes affect the oceans and organisms that live there?
- 1. Define, Create, Destroy marine habitats
- 2. Influences biodiversity: Speciation
-
Evidence for plate tectonics
- 1. Puzzle pieces
- 2. Volcanoes and earthquakes
- 3.Fossil and coal deposits
- 4. Magnetism
-
The sea floor is divided into two main regions
- 1. The continental margins: submerged edges of the continents
- -boundaries between continental crust and oceanic crust
- 2. Deep-sea floor
-
Hydrothermal vents
- – Cracks and crevices in lithosphere
- – Seawater seeps down and is heatedby mantle (up to350C, 660F
- – Dissolves minerals(sulfides)
- – Rises forming “blacksmokers” or deep sea hot springs
-
Black smokers
chimney-like structures that progressively build up around a vent as minerals solidify
-
When did the earth form?
4.6 billions years ago
-
when did liquid water appear?
4.3 billion years ago
-
first forms of life appeared
- 3 billion years ago
- -single-celled organism
-
Multicelled creatures appear
1 billion years ago
-
Vertebrates appear about
500 millions years ago
-
land plants appear about
400 million years ago
-
human beings appear
2-4 milion years ago
-
Oxygen appear
2 billion years ago
-
modern human(homo sapiens) appear
500,000 years ago
-
Plate boundaries
- 1.Convergent
- 2.Divergent
- 3.Transform
-
Transform boundary
- ex. san andreas fault
- - fault between offset segments of a spreading ridge
- -move horizontally in opposite directions
- -shear boundary
-
Convergent Plate boundaries
- • Lithospheric plates move toward each other
- • Higher density oceanic crust overridden by low density continental crust
- • Subduction zone forms and produces a trench
- •Subduction of older oceanic crust balances the spreading seafloor equation
- • Subduction zones are active geologic places
- oVolcanism
- oEarthquakes
- oIsland arc formation
-
Divergent Plate boundaries
- – Lithospheric plates move apart; form oceanic ridges
- – Upwelling of asthenosphere injects magma forming oceanic ridges and new oceanic crust
- – New oceanic crust cools through Curie Point and takes on present magnetic field direction
-
Convergence: Subduction Zones
- 1.Oceanic-continental
- • Trench formation
- • Earthquakes, volcanic ridges
- • Hydrothermal vents
- • Oceanic crust destroyed
- 2.Oceanic-oceanic
- • Trench formation
- • Earthquakes, volcanic islands
- 3.Continental-continental
- • Mountain formation
-
lithogenous sediment
weathering
-
Biogenous sediment
- Marine organisms
- • Calcareous (foraminiferans, coccolithophorids, shells)
- • Siliceous (diatoms, radiolarians, sponge spicules)
-
Microfossils
- 1.climate (species, Mg:Ca, Sr:Ca),
- 2. ageing (carbon dating)
- 3. ancient atmosphere(bubbles in sea ice)
-
Why is water so special?
- Only substance naturally occurring in all 3 states on Earth
- • High heat capacity
- – Highest of all common liquids and solids
- • Incredible solvent
- – Dissolves more substances than any other common liquid
- • High heat of vaporization
- – Highest of common liquids
- • High Surface tension
-
Water as a Solvent
Water molecules surround ions causing dissociation
-
Sea water becomes_____as it cools, until it freezes, it becomes ____
Sea water becomes denser as it cools, until it freezes, it becomes less dense
-
Sources of salts in Sea water
- 1. Weathering
- 2. Hydrothermal vents
- 3. 85% NaCl
-
Salinity
Grams of salt per 1000 grams of evaporated seawater
-
How do variations in salinity affect living organisms?
- -Most marine organisms die in fresh water
- -organism evolved specific mechanisms
-
The average salinity of the ocean is
35%
-
Important gases used and produced by living things are dissolved in seawater?
- 1. Oxygen
- 2. carbon dioxide
- 3. Nitrogen
-
Important nutrients used and produced by living things are dissolved in seawater?
- 1. Nitrogen
- 2. Phosphorus
- 3. Iron
-
What causes salinity to fluctuate?
- 1. Precipitation-evaporation ratio
- 2. Freshwater loss: Increases salinity
- -Evaporation
- -Freezing
- Freshwater Input: Decreases salinity
- -Precipitation
- -Glacial melt
- 3. Weather
- 4. Seasons
- 5. Climate
- 6. Currents
-
How do temperature and salinity influence density?
- Colder=denser
- Saltier=denser
-
How does temperature vary throughout the ocean?
- Open ocean: 28F to 86F (-2C to 30C)
- -Ocean is less prone to freezing because salt water freezes at colder temperature than pure water
- • Salt decreases freezing temperature,increases boiling temperature
- -Gets colder with depth
- -exception: hydrothermal vents
-
Estuaries
large fluctuations in salinity
-
What drives the movement of water throughout the world ocean?
- Surface: Wind(Sun)
- Deep: Density driven(Thermohaline Circulation)
-
How does pressure change with depth?
Pressure increases with depth because the amount of water above gets greater
-
Doldrums
Region near equator of light and variable winds
-
Trade winds
- approach the equator of about 45o
- -steadiest winds on earth
-
Coriolis effect
curve due to rotating sphere deflects winds and currents to the right in the northern hemisphere and to the left in the southern hemisphere
-
Westerlies
- -lie at middle latitudes
- -move in opposite direction of trade winds
-
Polar easterlies
- -Most variable of all winds
- -high latitude
-
Ekman spiral
Each layer pushes lower layer at additional angle with less speed
-
Gyres
Large circular systems formed when currents combine
-
Waves
- • Caused by winds
- • Carry energy but do not transport water
-
Fetch
the span of open water over which the wind blows
-
Size of wave depends on
fetch
-
Waves apporach shore
- – Elliptical water particle motion
- – Decrease speed
- – Wavelength decreases, height increases
- – Break when too tall
-
100+ ships lost at sea every year
– Reinforcement: “rogue waves”
-
Tides
- Rhthmic pattern of rising and falling sea surface
- - Casued by Gravitational pull of the sun and moon on the Earth and rotations of the earth and moon
-
when does high/low tide occur
- High: Bulge of water toward moon
- Low: Bulge away from moon
- -Earth rotates resulting in high and low tides
- New and Full Moon: Sun and Moon are in line
- -largest tidal bulge
-
What wavelengths of light travel farthest in seawater?
- Blue: Longest
- Red: the shortest
-
what are some ways living things influenced by tides?
- Ex.Grunion
- – Come on shore with highest high tides
- – Females dig hole and layeggs
- – Males curl around females to fertilize
- – Eggs hatch with return of high spring tides
- The intertidal zone is exposed at low tide and covered at high tide
-
Why are certain areas of the ocean more productive (more living things) than other regions?
- • Photosynthesis:
- -Photic zone: upper 200m
- • No sunlight penetrates beyond 1,000m
- -less productivity
-
How does pressure affect organisms?
- As pressure increases----gas-filled structured are compressed which could kill you. Lungs could collapse
- -Or if taken to areas with less pressure, Ex. Longfin Grouper,then swim bladder could expand and explode
-
What are the different habitats found in the ocean?
What sorts of challenges do living things face in these different habitats?
- 1. Intertidal Zone
- - This zone is covered with water at high tide, and exposed to air at low tide.
- -Must be able to retain moisture and protect from sunlight burn
- -Waves: Kelps has holdfast
- 2. Coral Reefs
- -sensitive to climate change
- 3. Pelagic Zone(Open Ocean)
- 4. Deep ocean
- -hard to find mates:Use sense of smell
- -cold, dark, strong pressure
-
Levels of Organization
- 1. Ecosystem
- 2. Community
- 3. Population
- 4. Individual
- 5. Organ
- 6. Tissue
- 7. Cell
- 8. Organelle
- 9. Molecule
- 10. Atom
-
Characteristics of Living Things
- • Organization: Cellular composition
- • Use energy (Metabolism)
- • Maintain homeostasis
- • Ability to sense and react to environment
- • Growth
- • Reproduction → capacity to evolve
-
Building blocks of life:
- • Carbon
- • Hydrogen
- • Oxygen
-
how are building blocks used by living things?
Energy storage and release
-
Organic molecules
- • Carbohydrates
- • Lipids
- • Proteins
- • Nucleic Acids (Genetic Information)
-
Carbohydrates
- • Simple sugars- metabolism
- – Glucose (C6H12O6)
- • Complex carbohydrates- energy storage
- – Starches
- – Chitin- exoskeletons
- – Cellulose- plant cell walls
-
Lipids
- • Glycerol and Fatty acids
- • Fats, oils, waxes
- – Cell membranes
- – Energy storage
- – Insulation
- – Waterproofing
- – Buoyancy
- – Hormones
-
Proteins
- • Amino acids
- – C,H,O + Nitrogen
- – Essential Amino Acids
- – Structure
- – Enzymes
- – Hormones
-
Nucleic Acids
- • Nucleotides
- – C,H,O,N + Phosphorus
- – 4 nitrogenous bases: Adenine, Cytosine, Thymine, Guanine
- • DNA
- • RNA– Uracil
-
• Prokaryotic cells:Bacteria
- • No nucleus and few organelles
- • Cell wall and cellmembrane
- • Circular DNA
- • Some are autotrophic
- • Some are motile
- • Unicellular
-
• Eukaryotic cells:
- • Complex organelles
- ie. Nucleus,Mitochondria
- • Chromosomes
- • Unicellular ormulticellular
-
• Animal cells
- – Cell membrane only
- – No chloroplasts
- – Small vacuoles
-
Plant cells
- – Cell wall (and cell membrane)
- – Chloroplasts (chlorophyll)
- – Central vacuole
-
Homeostasis
- • Maintain stable internal conditions
- – Water content
- – Salt/nutrient content
- – Temperature
- – Pressure
- • Requires energy (ATP)
-
Ectotherms
- - Body heat matches external temperature
- - most heat is lost to environment
-
Endotherms
- Retain significant metabolic heat
- -internal temperature stays warmer than external
-
Poikilotherms
Temperature varies with external temperature
-
Homeotherms
Regulate body temperature so it doesnt vary as much as external temperature
-
How do cells replicate themselves or produce gametes?
- 1.Asexual
- • Identical copies of parent cell
- – Fission, budding
- 2. Sexual
- • Combination of genetic information from 2 parents
- – Production of haploid gametes through meiosis
- – Fertilization forms a genetically unique zygote
- 3. Bacteria
- - Binary Fission: asexual reproduction in which an organism splits into two
-
Osmosis
- Diffusion of water
- - Across a semi-permeable membrane
-
Osmoconformer:
- • Conforms internal concentration to salinity of environment
- – Will gain or loose water when conditions change
-
Osmoregulator:
- Maintains constant internal water/solute level regardless of environment
- – Requires energy
-
Osmoregulation
- In seawater:
- • Water leaves the body, must excrete salts
- In freshwater:
- • Water enters the body, must absorb salts
-
Osmoregulation mechanisms:
- – Kidneys: excretory system
- – Salt glands
- – Alter blood chemistry (urea) ionoregulation
-
• Broadcast spawning
– Millions of gametes released
-
How does reproduction facilitate evolution?
- • The best adapted individuals produce more offspring
- -Evolution: change over time
- -Mutation, Divergence &Natural selection
-
How do we classify living organisms?
- Taxonomy
- 1. Genus: group of very similar species
- 2. species
Ex. Homo sapiens
-
Why are phylogenetic trees (cladograms) useful?
- -find out relatedness
- -share a common ancestor/trait
-
What are the major groups of marine microbes?
- 1. Viruses
- 2. Prokaryotes (bacteria, archea)
- 3. Eurkaryotes
-
What are the major groups of algae?
-
What are the major groups of plants?
-
Viruses
- -No cellular structure
- - not alive
- - Reproduce only byinfecting a living cell
- –Small amount ofgenetic material
- • Create dissolved organic matter(DOM)
- - when viruses infect bacteria, organic matter burst out
-
Prokaryota:
- • Oldest and simplest forms of life on Earth
- • Two domains:
- – Bacteria
- – Archaea
- • Shapes
- – Spheres
- – Spirals
- – Rods
- – rings
- • Size
- – Most microscopic
-
Bacteria
- Structurally simple
- • Genetically distant from archaea and eurkaryotes
- • Break down oil
- • Base of food web
-
Decay bacteria
Break down waste products and dead organic matter and recycle nutrients into the environments
-
• Types of symbiotic relationships:
- – Parasitism
- – Commensalism
- – Mutualism ☺☺
-
Cyanobacteria
- • “Blue-green algae” (photosynthetic bacteria)
- • Chlorophyll a and phycocyanin(blue) and phycoerythrin(red)
- • Formed stromatolites(calcareous mounds) 3 billion years ago
- • Accumulation of oxygen in atmosphere
-
Epiphytes
Photosynthetic organisms that live on algae or plants
-
Endophytes
Organisms that live inside algae
-
Archea
- • Similar to 3.8 billion year old fossils
- • Evolution of life, eukaryotes
- • Thought to be bacteria until late 70s
- – as different as both are from us!
- • Extremophiles
- – deep, hot, acidic, alkaline, saline
- • Also in mild environments
- – water column, sediments,symbiotic
- • Like bacteria can be spherical,spiral or rod-shaped
-
Prokaryota:Reproduction
- – Asexual
- – Horizontal transfer
- Ex. resistance
-
Protista
- -Eukaryotic
- -diverse evolutionary histories
- • Unicellular or multicellular
- • Autotrophic and/or heterotrophic
- • Example: Diatoms & Dinoflagellates
-
• Unicellular Algae
- – Autotrophic primary producers
- – Chloroplasts containing chlorophyll and other pigments
- – Planktonic, motile, sessile, symbiotic
-
Diatoms
- – Frustule(glassy shell): Silica (SiO2)
- – Carotenoid pigments + chlorphyll a,c
- – Most planktonic, may aggregate
- – Temperate and polar regions
- – Autotrophic (few heterotrophic): Major primary producers
-
Diatom reproduction:
– Asexual or sexual
-
Diatomaceous Earth
- – Siliceous ooze
- – Mined for:
- -Filters (pool, beer, sugar, syrup, oil)
- -Insulators (temp, sound)
-
Dinoflagellates
- – 2 flagella for omnidirectional movement
- – Cellulose plates
- – Carotenoid pigments + chlorphyll a,c
- – Eye spot
- – Autotrophic and/or heterotrophic
- – Warm water primary production
- – Red tide blooms, some toxic or bioluminescent
-
Silicoflagellates
- -start shaped
- – Silica, important primary producers
-
Coccolithophorids
- – Calcium carbonate coccoliths
- – Major blooms and chalk deposits
-
Cryptophytes
- – Small,
- -no skeleton,
- -reduced symbiotic eukaryotic cell containing chloroplast
-
Protozoa
- -Anima-like protists
- • Evolutionarily diverse group
- • Most single celled (some colonial)
- • Heterotrophic, some also autotrophic
-
Foraminiferans
- – Calcium carbonate shell(test), chambers
- – Pseudopodia: capture food
- – Feed on diatoms and other small planktonic organisms
- – Planktonic, benthic (bottom) and free or attached
-
Radiolarians
- – Elaborate silica shells and pseudopodia
- - Planktonic, shallow to deep
- – Form deep water siliceous ooze, microfossils
- - more resistant to dissolving
- -Giants in protozoans
-
Ciliates
- – Cilia used for locomotion and feeding
- - Highly complex single cells
- – Live on algae, sediments, in animals (clam gills, sea urchin intestines,fish skin), or attached to substrate, some planktonic (ex. Tintinnids).
- – Reproduce sexually and asexually
-
Fungi
- • Eukaryotic
- • Mostly multicellular (except molds, yeast)
- • Multicellular: hyphae filaments
- • Contain cell walls
- • Important decomposers,particularly of cellulose(plant material)
- • Also break down oil and toxins
-
Mutualistic: lichens(Fungi)
- • Fungi + Cyanobacteria or green algae
- • Hyphae provide support and protection, autotrophs provide food
- • Live on/in rock, barnacle or limpet shells
- • Potential source of antibacterial, antiviral, and antiprotozoal compounds
-
Macroalgae
- 1.Red (Rhodophyta)
- 2.Brown (Phaeophyta)
- 3.Green (Chlorophyta)
- • Eukaryotic, diverse evolutionary histories
- • Unicellular or multicellular
- • Autotrophic and/or heterotrophic
- • Not true plants, no true leaves, stems, roots,specialized transport tissues
-
Brown algae (Phaeophyta)
- -the biggest of all algal species
- Synthesize alginate – makes these seaweeds sticky and gooey
- - Make use of chl a and c, cartenoids (including fucoxanthin)
-
Green algae (Chlorophyta)
- -Gave rise evolutionarily to terrestrial plants
- -Contain the same photosynthetically active pigments, chl a and b,
- -Like land plants, greens store starch and cellwalls are made of cellulose
- - Useful as bioindicators of habitat degradation
-
Red algae (Rhodophyta)
- -Make use of chl a and phycobiliproteins(phycoerythrin, phycocyanin)
- - Can live at deeper depths than other algae
- - Calcium carbonate secretions by red algae contribute more to building tropical reefs
-
Plantae
- Surf grass and eel grass
- • True leaves, stems, and roots
- • Low intertidal and shallow water subtidal habitats
- • Trap sediments, stabilize sandy substrates, source of food(urchins), shelter from wave exposure
-
Animalia
- • Eukaryotic
- • Multicellular
- • Heterotrophic
- • Invertebrates vs. vertebrates
-
Porifera: Sponges
- • Organization: Cellular level
- • Symmetry: None
- • Aggregations of specialized cells withouttrue tissues
- • Sessile, benthic
- • Nearly all marine
- • Filter feeders
-
Cnidaria
- • Organization: Tissue level
- • Symmetry: Radial
- • Centrally located mouth
- • Tentacles with stinging cells (nematocysts)
- • Filter feeders, algae symbionts, drifting predators
- • Sessile (hydroid, anemone, coral) or mobile(jellies)
- • Colonial or solitary• Nerve net, photoreceptors
-
Basic body plans: Polyp
- -Attached
- -Mouth and tentacles away from substrate
-
Basic body plans: Medusa
- -Free swimming
- -Tentacles away from direction ofswimming
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