Marine Biology 278
Feb. 11, 2008 REVIEW
OUTLINE--EXAM I
INTRODUCTION
HISTORY of OCEANOGRAPHY —know these; see also READINGS at end of
outline:
4.
Challenger expedition 1872--> 3 years around
globe. Why important?
5.
First Marine Labs: founded 1870s-1910s (skip details, just know general
era)
7. 1940s-70s: why rapid growth in marine exploration ? What major advances?
9. mid90s-2000: why a new burst of marine exploration ? What major advances?
10. NOW: what is the current status of marine science? What major advances are underway or planned?
I. ENVIRONMENTAL FACTORS
A. TECTONIC/GEOLOGICAL FACTORS: -->Generalize
topographies of oceans
PLATE TECTONICS as unifying theory--know basic features, major
examples of these, especially Washington state coastal!!!:
1.
Spreading Centers/Rifts 2.
Collisions: Subduction Zones/Trenches; --land-to-seafloor and seafloor-seafloor
4. Hot Spots --island/seamount chains: how
form
*READ: Discovery of "new" Seamounts etc.
from satellite data.
* BIOLOGICAL IMPLICATIONS
--energy/nutrients for foodwebs; habitat creation/destruction (e.g., terranes,
tsunamis). Distinguish long vs short-term.
B. SURFACE FACTORS (geological and biological)
1.Rock: a)
Geologically produced (igneous, sedimentary, metamorphic);
b)
Biologically produced--limestone and other CaCO3 forms
----------- 2004: asphalt flow in the deep
2. Sediments *SIZE Categories: Cobbles > Sand > Silt > Clay (Clay + Silt = MUD)
a.
Lithogenous--land erosion (& volcanoes)
b.
Biogenous--how form: i)
calcarious; ii) siliceous
3.
Hydrogenous formations: know
how each forms, composition, where
found -- some may be BIOGENOUS
i)
Metal sulfide precipitates at hydrothermal vent areas
ii) Manganese nodules; iii) Methane
hydrates/carbonate rocks--see READING
SUMMARY DIAGRAM
showing distributions of sediments, formations in ocean and WHY
* Biological implications
makes different benthic habitat types; energy sources
(details later)
C.
MOVEMENT FACTORS
1. WAVES, Wind-Driven or earth-movement-driven (tsunami): *Energy distribution=L/2; how leads to cresting/crashing on shoreline
* Biological implications: i) wave shock damage
ii)
help determine surface type: mud, sand, rock iii)
mixed layer--later
2.
CURENTS: VERTICAL CURRENTS
a.
Wind-Driven SURFACE Currents: *WINDS and the CORIOLIS EFFECT: Know how sun, earth's rotation and Coriolis
lead to wind "cells" and the TRADE, WESTERLY and POLAR Easterlies Wind Belts! Then: water pushed to right (or
left in S.hemi.) of wind due to EKMAN effect--how all this creates CURRENT BELT
and the GYRES.
-->know
MAJOR GYRE patterns of all oceans, including NAMES of N. Pacific
currents, the Gulf Stream in the N. Atlantic, and the BELT = Antarctic
Circumpolar
-->COMPLICATIONS: what are EDDIES and how do they form?
b.
Wind-driven Vertical Currents:
i)
UPWELLING: how caused by winds at shoreline; EKMAN effect! ii)
DOWNWELLING
c.
THERMOHALINE Curents = Vertical density-driven currents
--how polar downwelling creates deep waters of the oceans; + upwelling near Antarctica, equator!
d.
Abyssal Currents/Storms--?? later
*BIOLOGICAL IMPLICATIONS of CURRENTS:
----create
major land Climate belts
i)
Surface gyres--major
distribution patterns of plankton; moderation of climate
ii)
Upwelling: nutrient
restoration! Know key areas from lecture
iii)
Downwelling takes O2
deep--prevents stagnation in the deep sea
3.
TIDES (Gravity-rotation-driven wave)
a) LUNAR Gravity, Earth-Moon Centrifugal
effect --how these create 2 opposite bulges;
And how b) SOLAR Tides --later; briefly: c) Lunar-orbit precession creates High-Lows, Low-Highs, etc.
D. OTHER PHYSICAL
FACTORS
1.
LIGHT: a. Depth--exponential
decrease with Wavelength variation--red vs. blue-green absorbance!! Open
Ocean vs. Coastal: often green or murky brown in coastal waters
b.
Latitude & seasonal variation; e.g., up to 24-hr light in polar
summers
c.
UV--most absorbed by ozone layer, but some makes it to surface--double
exposure at shore due to water
reflection
*BIOLOGICAL IMPLICATIONS: i) photosynthesis: why chlorophyll of limited use; ii) vision and
bioluminescence best at blue-green wavelengths; iii)
UV damage to DNA -- thymidine dimers
2.
Temperature: a. Depth variation: thermocline in warm areas; cold areas more uniform
b.
Latitude & seasonal variation; distortion of simple latitudinal
pattern by upwelling
c. Long-term variation: El Ni–os, changing sealevel with Ice Ages,
Global warming--Florida example
*BIOLOGICAL IMPLICATIONS:
1) Few extremes compared to
land (exceptions=hotspring vents; seaice extremophiles); Lack of severe cold
allows for polar marine life to be much more prolific than polar land life
2) Basic Temperature effects on biological reaction
kinetics: optima! Know the
basics of the plot!
3) Indirect WARMING effects: i) less O2 dissolving; ii) sealevel rise; and iii) suppressed downwelling--less O2 to deep + climate
effects
3. DENSITY: combination of temperature &
salinity
FW floats on SW; Warm water floats on colder; Ice floats; Salt lowers
Freezing Pt
*BIOLOGICAL IMPLICATIONS: i) buoyancy problems: protein, skeletons/shells
are denser than seawater; ii)
Freezing points
4.
Hydrostatic PRESSURE
DEPTH--1
atm per 10m: e.g. MARIANA
Trench/Challenger Deep ~ 11,000m so Pressure =_____??
E. CHEMICAL FACTORS
1.
Water: key properties for life, from textbook
2. IONS, MAJOR--Know
major ions, but donŐt memorize order except for Cl, Na; and
*
BIOLOGICAL ROLES from TABLE for Na+,
Cl-, SO4=, Ca++, K+, HCO3-
3.
MINOR/TRACE SOLUTES: nitrogen, phosphorus, silicon, iron forms in water;
*
BIOLOGICAL ROLES
from TABLE for
all of these! Can be limiting
factors; e.g., nitrate in N.
central oceans, IRON in S. central
oceans. Plans to fertilize the oceans with iron: what is proposed, what problems might arise! READING
4.
SALINITY: a.
How measured (%o, mM); general seawater contents, average 35%o. Also MOLARITY
(M or mM) and OSMOTIC PRESSURE (mOsm)--NaCl example for all three measures
b.
Altered by: freshwater (rivers, icemelt, rain) or evaporation --examples
*BIOLOGICAL IMPLICATIONS: i) Freezing point
and ii) Osmotic Balance:
"higher" vertebrates vs. most other organisms –know the
differences!
5. GASES:
a.
Oxygen--(i) solubility : 0-10 ml O2 / liter of water vs. 210 ml
in liter air
(ii) Depth--oxygen mimimum or dead
zones: more later (iii)
Temperature--warming DECREASES solubility
b.
CO2: Air: 0.00001
moles/liter; Water: 0.002
moles/liter as HCO3-
*Solubility
and the H20 reaction! know equation
and its implications in forming ACID!
*BIOLOGICAL IMPLICATIONS:
Oxygen: i) needed for
respiration; ii) Minimum or DEAD zones: limiting factor
CO2: i) for photosynthesis; ii) buffering;
iii) carbonate in shells; ACID can dissolve
CLIMATE CHANGE concerns: 1) TEMPERATURE: heats the Earth! Know how greenhouse effect works and new concerns; 2) ACIDIFICATION!
F. BIOTIC FACTORS--how
organisms in the environment interact
1. Predation
& other foodweb interactions -- define broadly, e.g., herbivores prey on
producers
2. Competition--rivals
for space, mates, other resources ;+/-
or -/-
3. Mutualism;
+/+
4. Parasitism/disease
: +/-
5.
Commensalism/Amensalism: +/0
and 0/0
II. MARINE ECOLOGY: HIGHER LEVELS OF ORGANIZATION
A. POPULATION--know
definition; B. COMMUNITY level--know definition
C. ECOSYSTEM level:
regional/habitat communities with all abiotic & biotic components
1. ABIOTIC Components: many, but the essential are:
--a. ENERGY: must be renewed
because energy is lost as unusable heat: Energy lost at each food-chain step is
80-90%. *2 forms:
---- i) Solar Light--photosynthesi;s ii) Geochemical--chemosynthesis &
reduced mineral energy
-- b. NUTRIENTS & water--not lost
but must be recycled through "biogeochemical cycles"
2. BIOTIC Components: TROPHIC Interactions = Foodwebs
-- Know Marine vs Land; why complex due to microscopic producers and filter feeders; with 4 or more levels in the oceans often
QUANTITATIVE ECOSYSTEM TERMS: 1. Abundance (and Productivity); 2. Richness; 3.
Diversity -- know DEFINITIONS
--What determines ABUNDANCE/RICHNESS/DIVERSITY?
1. ABUNDANCE/Productivity--LIMITING
FACTORS i) Energy & ii) Nutrients--why important! Examples of
habitats iii) Other harsh abiotic, biotic factors, e.g., Temperature--freezing
as crucial threshold
2. RICHNESS & DIVERSITY: know concept, example of each
-- a. Temporal Stability Hypothesis
-- b. Spatial Heterogeneity Hypothesis
-- c. Disturbance Hypotheses! how INTERMEDIATE differs from SEVERE disturbances
in affecting diversity
-- d. Energy-flow Hypothesis: briefly
--e. AREA Hypothesis (island effect)
D. BIOSPHERE level: BIOGEOCHEMICAL
CYCLES--Global recycling
4 possible recycling paths: i) Fast Surface loop in mixed layer; ii)
Upwelling Loop= sinking and upwelling; iii) Tectonic loop via subduction,
uplift -- rock/soil or volcanoes; iv) Tectonic loop at rift / ridge
--vents, lava
EXAMPLES--Major Ions: recycled every 10
million years via cycles iii) & iv) including erosion: know basic cation
and anion pathways
--C, H, N, O, P, S cycle through
all four pathways--KNOW THESE:
----Carbon: know pathways
i)ii)iii) including atmospheric CO2 plus limestone, chalk, oil, methane and
CaCO3 skeletons/shells
----Phosphorus: know pathways
i)ii)iii), including bird guano and CaPO4 bone
III.
ORGANISMAL MARINE BIOLOGY-- MARINE LIFE
A.
DOMAINS, KINGDOMS: Archaea, Bacteria,
Protista, Fungi, Plantae, Animalia -- Know basics of each
*Extremophiles: New discoveries
*VIRUSES: very common; may kill and thus recycle up to 25% of marine organic
material
B. TROPHIC ROLES
1. Producers: = Archaea, Eubacteria, Protista (Micro, Macroalgae), Plantae. Basic Autotroph mechanisms
All
need Process 1: *Energy & *inorganic H+
e- source to make NADPH, ATP from NADP, ADP;
*PHOTOSYNTHESIS: uses *light and *H/e source = HnX (examples: H2O, H2S)
*CHEMOSYNTHESIS: use *oxidation of H-e source = reduced geochemicals e.g., H2S + O2
Process
2: CO2 and other inorganic nutrients: NADPH and ATP
used to convert them to organic
molecules
RUBISCO used by all to fix CO2
2. Decomposers: = Archaea, Eubacteria, Fungi!!
* basic equations of heterotrophy using organic matter
with oxidizers: Know equations for O2, SO4, as oxidizers!
Pathway for denitrifiers
3. Consumers: = Protista (Protozoa) and Animalia!
C.
ADAPTATION: Interactions
of organisms with abiotic/biotic factors lead to adaptation
*Species adapt WITH these types of features/strategies (some overlap
among): know example of each
1)
Mechanical/Anatomical; 2)
Physiological/Biochemical 3)
Behavioral;
4) Lifecycle
*Two very different time courses of adaptation:
1)
Within lifetime: El Ni–o example!
Migratory fish and squid left (survived); seals starved
2)
Evolutionary time: new adaptations
from natural selection = different genes. EXAMPLE of LDH/temperature adaptation
*KEY PRINCIPLES of Adaptation
1. Co-evolution: how this causes ongoing
adaptations. VIDEO example of snail shells and crab claws/fish jaws
2. Cost/benefit tradeoffs: "Enough but not too much"
Principle! EXAMPLES!
Concept
that many adaptations cost energy, may divert energy from another adaptation
3. Historical
Constraints/Accidents: leaves non-adaptive vestiges, e.g., whale pelvises
ECOLOGY AND
BIOLOGY OF SALMON: know key
stages in the lifecycle
BENTHIC BIOLOGY and
HABITATS
i)
local producer-->herbivore-->carnivore (1 or more levels):
ii)
plankton-->local filter feeder--->carnivore (1 or more levels)
iii)
detritus-->local deposit/scavenger feeder--->carnivore (1 or more levels)
iv)
pelagic animal-->local pelagos-eating benthic carnivore--->carnivore (1
or more levels)
v)
local mutualism, e.g. animal/alga -->carnivore (1 or more levels)
OVERVIEW of BENTHIC ADAPTATIONS: Why Movement Factors
favor the evolution of sluggish, sessile animals using COST-BENEFIT idea. Thus marine animals are sometimes
plantlike! Note how the following adaptations are often analogous to land plant
adaptations:
ADAPTATIONS: apply esp. to sluggish/sessile:
1. Light/ENERGY/ Food/Nutrients
a)
Branching structures in filtering animals [also in algae]=high surface
area!
b)
Macroalgae blades with symmetrical structure for photosynthesis; specialized PIGMENTS
that enhance light absorption beneath the surface better than chlorophyll! Macroalgae=
RHODO-, CHLORO-, PHAEO-phyta
2. BIOTIC interactions --DEFENSES if you canŐt run or fight well
ANATOMICAL:
a)
Armor: coiled shells light but strong; spines. READING on nacre:
brick / beams and mortar microanatomy of mollusc shells! Recall co-evolution with crushing carnivores!--jaws, claws.
b)
Camouflage:
Static anatomy such as
flounderŐ
--also
can have dynamic/physiological camouflage such as octopod chromatophores
---and behavioral camouflage such
as decorator crabs
BIOMIMIMETICS: practical usages of nacre-like ceramics
PHYSIOLOGICAL/BIOCHEMICAL:
a)
TOXINS/Noxious compounds in animals like plants on land; often ADVERTISE with
bright colors: why? (BIOPRODUCTS: READING on practical uses of
ŇDRUGS from the DEEPÓ – why examine marine animals for pharmaceuticals
when we usually examine plants on land?
b)
Anti-fouling. Anti-competitor compounds—bryozoa,
sponges, bacteria that inhibit mussel, barnacle larvae, etc.
(BIOPRODUCTS READING--use on ship
hulls?)
c)
Autotomy , self-evisceration: examples of seastars, brittlestars, cucumbers: how
useful
BEHAVIORAL
a)
Clamming up/retreating;
etc.
b)
Burrowing
as an example; boring in rock
c)
ESCAPE RESPONSES: some Sluggish, sessile animals sometimes
have unexpected, fast, innate, predator-triggered maneuvers; e.g., Jumping
clam!
3. BIOTIC interactions --OFFENSES
BEHAVIORAL
Carnivore
Behaviors: hunt&chase (raptorial); ambush; creeping;
sedentary/opportunistic
ANATOMICAL & PHYSIOLOGICAL/BIOCHEMICAL:
a)
Crushing/smashing device - -i) crab
claws; ii) fish jaws; iii) mantis
shrimp! Know how each work. BIOMIMETICS why the interest in mantis shrimp
claws?
b)
Ambush weapons:
harpooning/paralyzing/stunning/poisoning/suckeringÉ.
i) Cnidaria nematocysts; ii) cone
snail harpoon; iii) snapping shrimp claw jet burst ; iv) octopods
-- suckers know how each works!!!
BIOPRODUCTS: why interest in cone-snail toxins?
TEXT: key figures (and associated text, lecture) to understand were given in lecture!
READING on
LECTURE HANDOUTS--be
able to answer these questions:
Lecture #1: *IN
DEPTH ACCOUNTING and DEEP SEA FULL.. what is the Census of Marine Life
*OCEAN
OBSERVING NETWORK.. and WHERE DEEP SPACE.. what are some of the ocean
monitoring systems under development?
Lecture #2: *NEW
CENTER TO FOCUS.. what is this about and why are they building it?
*A
NEW VIEW. .: how are new seamounts
and deep-sea mountain ranges being discovered from space?
*SEA
ANIMALS GET TAGGED...how are these animal tags being used for multiple roles?
*DEEP-SEA
BIOLOGY--What is the extent of our ignorance about the oceans? How did Forbes
and Thomson alter the course of marine science?
Lecture #3: *UNDERWATER
PAVEMENT: What was this unique discovery in 2004?
*POPULAR
MECHANICS article: what are methane hydrates and why so much interest?
*THE
NEXT LAND RUSH: why is the Arctic seafloor suddenly of international interest?
Lecture #4: *GLOBAL
WARMING IS SPEEDING.. up what and why?
Lecture #5: *
EUROPE COULD CATCH--how does salinity of the Arctic affect European climate?
Lecture #6: *
HOT WATERS MAKE IT HARD--for what and why?
*OZONE
HOLE and UV are doing what to Antarctic sea life?
*YES
IT'S BEEN GETTING: know the basic 'hockey stick' graph
*AS
OCEANS WARM -- what is the impact on food chains?!
Lecture #7: *WHY
do JELLIES love warming?
*CO2/ACID
article -- what is the concern here?
*SHOULD
OCEANOGRAPHERS PUMP IRON...what are the issues regarding oceanic Fe?
Lecture #8: *OCEAN
DEAD ZONE what causes low oxygen zone
*ISLAND
LAW -- affects diversity hows
*WHAT
DETERMINES DIVERSITY ?
Lecture #9: *ARTICLE
ON on dumping excess CO2 into the deep-sea: what are the issues?
*SEEPS
NEAR SANTA BARBARA -- what is the oil source?
Lecture #10: *INDUCIBLE
DEFENSES: Examples of cost-benefit tradeoffs: intertidal mussels
*Three
articles: Know some recent findings about marine microbes and viruses!
Lecture #11: *Dr. Eva Enders: know key stages in salmon lifecycle!
Lecture #12: *Diagrams for
macroalgae
*MAKING
THE MOST OF IT: what are some biomaterial properties of sponges and mollusks and
some practical uses?
Lecture #13: *DRUGS
FROM THE DEEP and PRIMORDIAL OCEAN OOZE: why are researchers seeking drugs in
the sea, and with what success?