lecture 3 ecology Flashcards
(73 cards)
aquatic biomes, what is the key to distribution
the key is the levels of salinity. we have fresh (low salinity) – estuaries (mid salinity) and marine (high salinity)
what does the estuaries act as
it acts as a barrier between the fresh water and saltwater. many organisms cannot cross this barrier, however salmon can
what is the depth of the ocean
it is an important structuring factor
what does depth affect
temperature and light levels. (the deeper you go the darker and colder it gets).
what is another thing that separates the ocean
the distance to shore (intertidal, neritic, oceanic)
intertidal
close to shore, between low and high tides – mostly exzposed to air
neritic
near shore zone
oceanic
off shore
depths on the ocean
photic, aphotic, abyssal, pelagic, mesopelagic, benthic, continental shelf
photic zone
99% of the light around this zone, top 200m – where photosynthesis happens, therefore all photosynthesizing organisms live here.
aphoticx zone
1% of light – beyond light, res of the depth.a
abyssal zone
deep deep ocean – very food limited.
pelagic zone
the water column, basically all zones tg
mesopelagic
200-1000m – intermediate, the twilight zone. entire marine food web lives in this zone
benthic
seafloor – corals attached to the floor
continental shelf
shallow region
different zones summary
benthic vs pelagic – seafloor vs water column
photic vs aphotic – light vs no light
intertidal vs neritic vs oceanic – shore vs near shore vs offshore
Lakes – structre
similar to oceans in depth (photic (more shallow than ocean), aphotic, benthic (lake floor), pelagic(water column)). however distance to shore is diff (naming wise) – Limnetic (open lake (far offshore)) – littoral (close to shore line)
what are aquatic environments in terms of nutrients
nutrien limited – not much productivity. `
what does stratification do / describe
it controls the nutrient availability – basically how ‘fixed’ the water column is.
stratified lake – description
layers sitting on top of each other – not much mixing due to differing densities
Lake stratification (summer)
in the summer – we have 2 layers – warm and cold – the warm layer : is photic, photosynthesis occurs, it is oxygen rich but nutrient poor because all the nutrients are being used for photosynthesis– the cold layer is: aphotic, oxygen poor because no photosynthesis and nutrient rich because not as many organisms are present so it is not used up.
why are there two layers in the sumer
because of the thermocline – this is why they dont mix. this is the zone of rapid temperature change, also known as the gradient of temperature. – the warmer water is less dense so it floats ontop of the colder, more dense water.
lake stratification (fall)
the surface water in the lake cools down – thermocline breaks down therefore no more temperature gradient – this means the water at the surface is getting more dense – eventually surface water will get to sae density, or higher as the bottom layer and they will mix – bottom layer brings up nutrients and top layer will bring down oxygen.