bi303 marine dynamics

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16 Terms

1
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learning outcomes

  • what drives the dirstibution of ocean biomes/biodiversity

  • how extensive is ocean biodiversity and how much do we know?

2
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earths surface vs ocean

71% ocean, 97% of all water on earth is in the ocean

beginning of all terrestrial life

primary protein source

3
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elements that make up living things =/= elements that make up earths crust

most common in living things are mostly soluble in saltwater, most comes from the ocean

4
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soluble in saltwater

inside the square arent soluble, water as a sieve for elements //rewatch

<p>inside the square arent soluble, water as a sieve for elements //rewatch</p>
5
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marine biodiversity

lower than terrestrial biodiversity (1.5mil species richness vs 5mil) - not necessarily true, this is all the species that we know of. we know more about terrestrial organisms

mostly invertebrates, have microorganisms as well

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marine biomes driven by

who is the primary producer!!

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mangrove vs kelp

sort of complete each other irt the americas, mangrove located around the equator and kelp around the tropics

based on currents, upwelling, deep trench water

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drivers of marine biodiversity

  • temperatures

  • currents and circulation

  • nutrients (upwelling/downwelling)

  • primary productivity

  • light

  • salinity

9
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temperature

latitude based, cold at the poles, warm at the equator

graph is sea surface temperature vs amt of biodiversity * increasing diversity with increasing temperature

pinnipeds adapted to colder environments

<p>latitude based, cold at the poles, warm at the equator</p><p>graph is sea surface temperature vs amt of biodiversity * increasing diversity with increasing temperature</p><p>pinnipeds adapted to colder environments</p>
10
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currents and circulation

coriolis effect - wind moves clockwise in north hemi and ccw in south hemi

<p>coriolis effect - wind moves clockwise in north hemi and ccw in south hemi</p>
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nutrients (upwelling/downwelling)

movement of water upwards/downwards - as water comes from land into more open ocean, deep water comes up and causes upwellings

nutrients at depth, so upwelling brings nutrients upwards while downwelling brings nutrients to deep water

<p>movement of water upwards/downwards - as water comes from land into more open ocean, deep water comes up and causes upwellings</p><p>nutrients at depth, so upwelling brings nutrients upwards while downwelling brings nutrients to deep water</p>
12
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primary productivity

ultimate limit on abundance and diversity

CHLOROPHYLL as a proxy of primary productivity - pigment of phytoplankton

graph of surface chlorophyll matches with areas of upwelling

<p>ultimate limit on abundance and diversity</p><p>CHLOROPHYLL as a proxy of primary productivity - pigment of phytoplankton</p><p>graph of surface chlorophyll matches with areas of upwelling </p>
13
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light

photic zone - 0-200m

not all light penetrates down to 200m

why coastal light doesnt reach 200m - lot of stuff in the way (phytoplankton, silt, dust, more particles essentially) so it physically cant reach

<p>photic zone - 0-200m</p><p>not all light penetrates down to 200m</p><p>why coastal light doesnt reach 200m - lot of stuff in the way (phytoplankton, silt, dust, more particles essentially) so it physically cant reach</p>
14
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salinity

less variation 32 to 38ppt

35 ppt - average

<p>less variation 32 to 38ppt</p><p>35 ppt - average</p>
15
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whats the most important variables for predicting marine biodiversity?

  • depth

  • water temp

  • sunlight

<ul><li><p>depth</p></li><li><p>water temp</p></li><li><p>sunlight</p></li></ul><p></p>
16
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whats the most important variables for predicting terrestrial biodiversity?

  • sunlight

  • air temp

  • precipitation

(sunlight determines temperature)

<ul><li><p>sunlight</p></li><li><p>air temp</p></li><li><p>precipitation</p></li></ul><p>(sunlight determines temperature)</p>

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