![Page 1: CH 15 Ocean Life and Ocean Water Salinity – total amount of dissolved solids in water Expressed in parts per thousand Average salinity of is 35 ppt or](https://reader036.vdocuments.site/reader036/viewer/2022082713/5697c0211a28abf838cd2941/html5/thumbnails/1.jpg)
CH 15 Ocean Life and Ocean Water
Salinity – total amount of dissolved solids in waterExpressed in parts per thousandAverage salinity of is 35 ppt or 3.5 %2 main dissolved solids– Chlorine = 55 % from earth’s interior (volcanoes)– Sodium = 30.6 % from chemical weathering of rocks
carried by rivers
![Page 2: CH 15 Ocean Life and Ocean Water Salinity – total amount of dissolved solids in water Expressed in parts per thousand Average salinity of is 35 ppt or](https://reader036.vdocuments.site/reader036/viewer/2022082713/5697c0211a28abf838cd2941/html5/thumbnails/2.jpg)
Processes Affecting Salinity
Oceans are well mixedPercentages of major components in sea water are constant, but salinity varies from 33 – 38 ppt– Precipitation decreases salinity– Runoff from land decreases– Icebergs melting decreases– Evaporation increases– Formation of sea ice increases
![Page 3: CH 15 Ocean Life and Ocean Water Salinity – total amount of dissolved solids in water Expressed in parts per thousand Average salinity of is 35 ppt or](https://reader036.vdocuments.site/reader036/viewer/2022082713/5697c0211a28abf838cd2941/html5/thumbnails/3.jpg)
Ocean VariationsTemperature– Mostly a function of latitude– A function of depth, too– Thermocline – rapid change in temp as depth changes– Only found in low latitudes
Density– Higher salinity = higher density– Lower temps = higher density– Deeper = more dense– Pycnocline – rapid change in density as depth changes– Only found in low latitudes
![Page 4: CH 15 Ocean Life and Ocean Water Salinity – total amount of dissolved solids in water Expressed in parts per thousand Average salinity of is 35 ppt or](https://reader036.vdocuments.site/reader036/viewer/2022082713/5697c0211a28abf838cd2941/html5/thumbnails/4.jpg)
Ocean Layering
Most parts of the open ocean have a 3 layered structure– Surface zone – warmest; photosynthesis; mixed
zone due to waves, currents, and tides; mostly constant temperatures
– Transition zone – thermocline: pycnocline; halocline– Deep zone – abyss; very cold, very high pressures,
and very dark
![Page 5: CH 15 Ocean Life and Ocean Water Salinity – total amount of dissolved solids in water Expressed in parts per thousand Average salinity of is 35 ppt or](https://reader036.vdocuments.site/reader036/viewer/2022082713/5697c0211a28abf838cd2941/html5/thumbnails/5.jpg)
Ocean Life
Marine organisms are classified according to where they live and how they move
1. Plankton – drift with ocean currents– Phytoplankton/plant and zooplankton/animal
2. Nekton – all animals that can swim/move on their own– Fish, squid, turtles
3. Benthos – living on or in the ocean bottom– Worms, coral, starfish
![Page 6: CH 15 Ocean Life and Ocean Water Salinity – total amount of dissolved solids in water Expressed in parts per thousand Average salinity of is 35 ppt or](https://reader036.vdocuments.site/reader036/viewer/2022082713/5697c0211a28abf838cd2941/html5/thumbnails/6.jpg)
Marine Life Zones
3 factors to divide oceans into marine life zonesA) Availability of sunlight
– Photic; euphotic; aphoticB) Distance from shore
– Intertidal, neritic, oceanicC) Water depth
– Pelagic, benthic, abyssal
![Page 7: CH 15 Ocean Life and Ocean Water Salinity – total amount of dissolved solids in water Expressed in parts per thousand Average salinity of is 35 ppt or](https://reader036.vdocuments.site/reader036/viewer/2022082713/5697c0211a28abf838cd2941/html5/thumbnails/7.jpg)
Other Ocean Stuff to Learn
Hydrothermal ventsCoral reefsAbyssal creaturesSharks
![Page 8: CH 15 Ocean Life and Ocean Water Salinity – total amount of dissolved solids in water Expressed in parts per thousand Average salinity of is 35 ppt or](https://reader036.vdocuments.site/reader036/viewer/2022082713/5697c0211a28abf838cd2941/html5/thumbnails/8.jpg)
Oceanic Productivity
Primary productivity – Production of organic stuff from inorganic stuff…– Photosynthesis - – Chemosynthesis – bacteria and H2S
Productivity in polar oceans – Seasonal variation– Salt concentrating nutrients– Limit of available sunlight
![Page 9: CH 15 Ocean Life and Ocean Water Salinity – total amount of dissolved solids in water Expressed in parts per thousand Average salinity of is 35 ppt or](https://reader036.vdocuments.site/reader036/viewer/2022082713/5697c0211a28abf838cd2941/html5/thumbnails/9.jpg)
Productivity in tropical oceans– Sunlight penetrates far– Thermocline prevents mixing– Lack of nutrients limits production
Productivity in temperate oceans– Sunlight and nutrient supply limit productivity– Each season has its effect– Spring is when the big bloom occurrs.
![Page 10: CH 15 Ocean Life and Ocean Water Salinity – total amount of dissolved solids in water Expressed in parts per thousand Average salinity of is 35 ppt or](https://reader036.vdocuments.site/reader036/viewer/2022082713/5697c0211a28abf838cd2941/html5/thumbnails/10.jpg)
Oceanic Feeding Relationships
Trophic levels– Feeding stages on a food pyramid– Herbivores and carnivores
Transfer efficiency– Energy transfer between trophic levels is very
inefficient…usually about 2 %...wowFood chains and food webs– Yada, yada, yada