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bacteria
simple, life forms without nuclei
archaea
simple, microscopic creatures
eukarya
complex, multicellular organisms
eubacteria
single celled organisms that lack nuclei
(includes cyanobacteria)
archaebacteria
microscopic, bacteria-like organisms
(includes methane producers & sulfur oxidizers of deep sea vents)
plantae
multicelled, photosynthesis plants
(surf grass, eelgrass, mangrove, & marsh grasses)
animalia
multicelled organisms, range from simple sponges to complex vertebrates
protista
singlecelled and multicelled with nucleus
*algae & protozoa fall under this category
fungi
mold & lichen
taxonomy
systematic classification of organisms
taxonomy order
kingdom—>phylum—>class—>order—>family—>genus—>species
plankton
floaters (there’s literally 8 types I’m not abt to make a flashcard for each of them)
nekton
independent swimmers
most adult fish & squid
marine mammals
marine reptiles
benthos
bottom dwellers
live in perpetual darkness, coldness, and stillness
*most abundant in shallower water
epifauna
live on the surface of the sea floor
infauna
live buried in sediments
nektobenthos
swim or crawl through water above seafloor
broadcast spawning
eggs & sperm directly released into seawater
isotonic
organism’s body fluid salinity same as ocean
hypertonic
organism’s fluids have higher salinity than ocean
hypotonic
organism’s fluids have lower salinity than ocean
camouflage
through color patterns
countershading
dark on top, light on bottom
epi
= surface, full light
meso
= middle, twilight light
aphotic
= no light/ everything deeper
gills
animals extract dissolved oxygen from seawater through these
stenothermal
organisms withstand small variation in temp
*driven by heat capacity
typically live in open ocean
eurythermal
organisms withstand large variation in temperature
*driven by heat capacity
typically live in coastal waters
stenohaline
organisms withstand only small variation in salinity
typically live in open ocean
euryhaline
organisms withstand large variation in salinity
typically live in coastal waters, like estuaries
cube a
greater resistance to sinking per unit of mass than cube c
adaptations of marine organisms
high surface area to volume ratio
as size goes down, surface area goes up
a smaller organism has an easier time getting the nutrients they need
Deep Scattering Layer (DSL)
daily migration of many organisms to deeper, darker, parts of the ocean (can protect some species from predators)
neritic province
from shore seaward, all waters <200m deep
oceanic province
depth increases beyond 200m
Pelagic
open sea
Benthic
sea floor
epipelagic
only zone to support photosynthesis
dissolved oxygen decreases around 200m
mesopelagic
organisms capable of bioluminescence are common
contain dissolved oxygen minimum layer (OML)
supralittoral (Benthic Environments)
transition from land to sea floor above spring high tide line; spray zone
subneritic (Benthic Environments)
spring high tides shoreline to zoom about ½ the continental shelf
littoral (Benthic Environments)
intertidal zone
sublittoral (Benthic Environments)
shallow subtidal zone
bathyal
continental slope
abyssal
more than 80% of benthic environment
animal tracks in abyssal clay
hadal
below 600m
only deep trenches on continental margins
Euphotic
surface to where enough light exists to support photosynthesis
*ocean zones based on light availability
Disphotic
small but measurable quantities of light
Aphotic
no light
primary productivity
rate at which energy is stored in organic matter
photosynthesis
uses solar radiation
chemosynthesis
uses chemical reactions
plankton nets
used to capture plankton
satellites
used to monitor ocean color
Moderate Resolution Imaging Spectroradiatiometer (MODIS)
measures 36 spectral wavelengths
factor affecting primary productivity
nutrient availability
eutrophication
enrichment of ecosystem with chemical nutrients
compensation depth
net productivity becomes zero
(productivity - respiration = compensation depth)
anthophyta
sea-beaming plants
only in shallow coastal waters
primarily grasses & mangroves
important source of food &n protection for near shore animals
macroscopic algae
(large) algae
green, red, & brown algae
microscopic algae
(small) algae
produce food for 99% of marine animals
mostly planktonic (drifters)
golden algae
diatoms
tests (shells) made of silica, accumulated shells produce diatomaceous earth
coccolithophores
plates of calcium carbonate
red tides
harmful algae blooms (HABs)
humans who eat affected fish may get paralytic shellfish poisoning (PSP)
cultural eutrophication
speeding up natural eutrophication through human activities
dead zones
hypoxic (oxygen-poor) water or anoxia (no O2)
mouths of major rivers
spring runoffs
suffocates bottom dwellers
how dead zones form
nutrient over enrichment
phytoplankton bloom
eutrophication
decay
what do phytoplankton need to thrive?
sunlight & nutrients
winter low
many nutrients & little sunlight
spring high
spring bloom
summer low
few nutrients & abundant sunlight
fall high
fall bloom
producers
autotrophic
consumers
heterotrophic
decomposers
heterotrophic
feeding strategies
suspension feeding or filter feeding
trophic levels
about 10% of energy transferred to the next trophic level
standing dock
the mass present in the ecosystem at any given time
Maximum Sustainable Yield (MSY)
max amount of fish biomass that can be removed yearly & still allow sustainable population
bycatch
non-commercial species are taken incidentally by commercial fishers
distribution of benthic organisms
more than 98% of approximately 230,000 known marine species live in or on ocean floor
Epifauna
attached to substrate
move over sea floor
spray zone
above spring tide zone
high tide zone
relatively dry
middle tide zone
covered by all high tides/ exposed by all low tides
low tide zones
usually wet
infauna
burrowing animals
subtidal zone
rocky bottom
sessile
refer to those that are permanently attached to substrate, such as rocks & move freely
polyps
individual corals animals
zooxanthellae
symbiotic photosynthesis microscopic algae in coral tissues
hermatypic coral
mutualistic relationship with algae
fringing reef
develop along margin of landmasses
ideal temp, salinity, & turbidity conditions
barrier reefs
follows fringing reef stage
grows upward as landmass subsides
atoll
follows barrier reef stage
volcano submerges completely after millions of years, circular reef that grows upwards is left behind
coral bleaching
symbiotic zooxanthellae (what give coral color) die, leave, or become toxic
swim bladders
change in depth, expands or contracts
slow moving fish
copepods
*most of ocean’s zooplankton biomass
microscopic
shrimp-like crustaceans
cnidarians
soft bodies, stinging tentacles