Marine
Biology 278
Feb.
18, 2009 REVIEW
OUTLINE--EXAM I
INTRODUCTION
HISTORY of
OCEANOGRAPHY —know these; see also
READINGS at end of outline:
3.
#arly 1800s: E. ForbesÕ azoic hypothesis
4. Challenger expedition 1872--> 3 years around globe. Why
important?
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.
2001-08: 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/Rift Valleys& MidOcean Ridges 2. Collisions: Subduction
Zones/Trenches; --land-to-seafloor and seafloor-seafloor
4.
Hot Spots --island/seamount
chains: how form
* BIOLOGICAL IMPLICATIONS Distinguish long vs
short-term: habitat creation/destruction (e.g., earthquakes, collisions,
tsunamis, new islands).
--alter climate and currents; .--energy/nutrients for life;
B. SURFACE FACTORS (geological and biological)
1.Rock: a)
Geologically produced (igneous, sedimentary, metamorphic);
b) Biologically
produced--limestone and other CaCO3 forms;
2. Sediments *SIZE Categories: Cobbles > Sand >
Silt > Clay (Clay + Silt = MUD; OOZE=
mud with 30+% organic origin)
a)
Calcareous and b) Siliceous: what each is
3. Hydrogenous
formations: know how each forms, composition, where found -- some may be BIOGENOUS
a) Metal sulfide precipitates at
hydrothermal vent areas
b) Manganese nodules;
c)
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. CURRENTS: 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!
c.
THERMOHALINE Curents = Vertical density-driven currents
--how polar
downwelling creates deep waters of the oceans; + upwelling near Antarctica,
equator!
d.
Abyssal Currents/Storms--?? Mysterious deep storms; vents causing
convection currents in rift valleys
*BIOLOGICAL
IMPLICATIONS of WINDS, CURRENTS:
-- winds create major land Climate zones
i) Surface gyres--major
distribution patterns of plankton; moderation of climate
ii) Upwelling:
nutrient restoration! Be able to relate high upwelling areas to wind belts
iii) Downwelling takes O2 deep--prevents stagnation in the deep sea
iv) Storms/; can also churn up nutrients from deep
3.
TIDES (Gravity-rotation-driven
wave)
a) LUNAR Gravity, Earth-Moon Centrifugal
effect --how these create 2 opposite bulges;
b) SOLAR
Tides –how they add/subtract with lunar tides to create Neap and Spring
tides:
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
tropical areas, and in temperate-zone summers; cold areas more uniform
b.
Latitude & seasonal variation; Few extremes compared to land
(exceptions= vents). Basic latitudinal pattern of colder away from equator;
altered by upwelling (cold).
El Ni–o: what happens to Pacific currents
c. Long-term variation: changing sealevel with Ice Ages, warming: trends
for last 400,000 years
* BIOLOGICAL
IMPLICATIONS:
i) Basic
Temperature effects on biological reaction kinetics and complex biological
molecules: optima! Know the
basics of the plot!
ii) less O2 dissolving;
iii) sealevel rise; and iv) suppressed
downwelling--less O2 to deep + climate effects
3. DENSITY: combination of
temperature & salinity; DENSER THINGS SINK
FW floats on SW; Warm water floats on
colder; BUT Ice floats
*BIOLOGICAL IMPLICATIONS: i) buoyancy problems:
protein, skeletons/shells are denser than seawater; ii) Subsurface never freezes!
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 donÕt memorize order
except for Cl, Na; and
*
BIOLOGICAL ROLES from TABLE for Na+, Cl-, 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) Osmotic
Balance and ii) Freezing point:
OSMOCONFORMERS vs OSMOREGULATORS
–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! Know equation and effect on shells
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
-- OCEAN vs Land; why complex due to microscopic
producers and filter feeders;
with up to 6 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)--skip
D.
BIOSPHERE level: BIOGEOCHEMICAL CYCLES--Global
recycling
5 possible recycling
paths: i) Fast Surface loop in mixed layer; ii) Upwelling Loop=
sinking and upwelling; iii) deposition then release (from land, oil): iv)
Tectonic loop via subduction, uplift -- rock/soil or volcanoes; v)
Tectonic loop at 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 including
atmospheric CO2 plus limestone, chalk, oil, methane and CaCO3 skeletons/shells
----Phosphorus: know pathways
including bird guano and CaPO4 bone
--Salt Ions: know
pathways for positive and negative major ones
III. ORGANISMAL MARINE BIOLOGY-- MARINE LIFE
A.
DOMAINS, KINGDOMS: Archaea, Bacteria,
Eukarya = Protista, Fungi, Plantae, Animalia -- Know
basics of each
*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:
leaves non-adaptive vestiges, e.g., whale pelvises
CRAIG
MATKIN: ECOLOGY OF ORCAS AND GREY WHALES IN ALASKA: know
how the orcas feed
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 and Plankton food 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:
FACTORS and ADAPTATIONS:
apply esp. with sluggish/sessile organisms:
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 canÕt run or fight well
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
BIOMIMIMETICS: practical
usages of nacre-like ceramics
b)
CAMOUFLAGE: Static anatomy such
as flounderÕ
--also
can have dynamic/physiological camouflage such as octopod chromatophores
---and behavioral
camouflage such as decorator crabs
c) TOXINS/Noxious
compounds
in animals like plants on land; often ADVERTISE with bright colors: why?
BIOPRODUCTS: READING on practical uses of
ÒDRUGS from the DEEPÓ – why examine marine animals for pharmaceuticals
when we usually examine plants on land?
d) Anti-fouling. Anti-competitor compounds—bryozoa, sponges,
bacteria that inhibit mussel, barnacle larvae, etc.
BIOPRODUCTS READING--use on ship
hulls?
e) Autotomy ,
self-evisceration: examples
of seastars, brittlestars, cucumbers: how useful
f) BEHAVIOR: Clamming up/retreating; etc.; Burrowing as an example; boring in rock
--ESCAPE
RESPONSES: some Sluggish,
sessile animals sometimes have
unexpected, fast, innate, predator-triggered maneuvers; e.g., Jumping clam!
3. BIOTIC interactions --OFFENSES
a)
BEHAVIOR Carnivore Behaviors:
hunt&chase (raptorial); ambush; creeping; sedentary/opportunistic
b) CRUSHING/SMASHING
devices -
-i) crab
claws; ii) fish jaws; iii) mantis
shrimp! Know how each work. BIOMIMETICS why the interest in mantis shrimp
claws?
c) AMBUSH/GRIPPING 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?
4. WAVES/CURRENTS: resisting or avoiding
ARMOR
BIOLOGICAL
GLUES --- BIOPRODUCTS e.g., mussel glue
5.
LIFE-CYCLE Adaptations:
r- vs K-selected (or strategies): apply cost-benefit idea!
Modes: a.
Asexual (clonal) growth: mutual protection from predation, waves, etc.; rapid colonization
b.
Planktonic Larval Stage: r-strategy:
know this lifecycle, outcome, how larvae settle
--sluggish/sedentary
spp need means of DISPERSAL
--and
ways to RECOLONIZE habitats after destruction of adults
c.
Direct Development: K-strategy; or mixed r- and K: many
fishes, crabs, mammals
--mobile adults care for eggs, or put
more energy into them as yolk, etc.
--young and old
both usually mobile enough to disperse readily
ALSO: Sex-Reversal
in some animals, e.g., clownfish: why useful; magic number in READING
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: *GREEN BUSH: what did
Pres. Bush do?
*TROUBLED
WATERS—what are some of the key ocean crises?
*STARS IN THE SEA: what is the Census of
Marine Life, and some key discoveries?
*STATIONS
IN THE SEA.. what are some of the ocean monitoring systems under development?
*ROBOT
GLIDERS are being designed to do what?
Lecture #2: *DEEP-SEA BIOLOGY--What
is the extent of our ignorance about the oceans? How did Forbes and Thomson
alter the course of marine science?
*US
SHIP HEADS.. and CANADA BEGINS MAPPING..why the sudden interest in the Arctic
seafloor?
Lecture #3: *DEEP SEA, ARCTIC
MAY...what are gas hydrates and why of interest?
*DEEP
SEA-CRETS : why were these researchers both exhilarated and disheartened?
*THE
NEXT LAND RUSH: why is the Arctic seafloor suddenly of international interest?
Lecture #4: *FEARS
SURFACE..why this concern about methane hydrates?
*CONDITIONS
BOOST..what is the importance of upwelling here?
Lecture #5: *IS ÔTHE DAY
AFTERÕ ..how does salinity of the Arctic affect European climate?
*FLOATING
TEXAS-SIZED GARBAGE..what is this patch and why is it there?
*PERFECT
STORM – how do storms boost fisheries?
Lecture #6: *AS OCEANS WARM
-- what is the impact on food chains?!
*OZONE
HOLE and UV are doing what to Antarctic sea life?
*HOT
WATERS MAKE IT..what for fish and why?
*ARCTIC
ICE MELTING..what is happening?
Lecture #7: *SEVERAL
ARTICLES: what are some effects of warming on sea life?
*SEVERAL
ARTICLES..what are the issues regarding oceanic iron and the plans to fertilize
the oceans?
*SOUTHERN
OCEAN.. what is the concern here?
Lecture #8: *CONCLUSIVE
PROOF: what is this evidence that global warming is human-caused?
*WHY
do JELLIES love warming?
*SCIENTISTS
ALARMED..what is causing Dead Zones?
Lecture #9: *ARTICLE ON on
dumping excess CO2 into the deep-sea floor: why?
Lecture #10: ¥OCEAN STUDY YIELDS: what is
the basic finding on ocean microbes?
Lecture #11: *INDUCIBLE DEFENSES: Examples
of cost-benefit tradeoffs: intertidal mussels
*PREDATORS
RETURN: why might this happen to Antarctica, and why might some life there be
vulnerable?
*MAKING
THE MOST OF IT: what are some biomaterial properties of sponges and mollusks
and some practical uses?
Lecture
#12: *Two articles: what has NACRE inspired scientists to create?
*RESEARCHERS
DOCUMENT RAPID..what rapid change took place in stickleback and why?
*DEEP
SEA DENIZEN--what is it about cucumbers that is of practical interest?
*DRUGS
FROM THE DEEP and PRIMORDIAL OCEAN OOZE: why are researchers seeking drugs in
the sea, and with what success?
Lecture #13: --SNAIL VENOM: why medically of
interest?
--BIOLOGY
REVEALS: what are some applications of marine anchoring mechanisms?
--SNAIL
SPEWS: how does the snapping shrimp stun its prey?