1_Oceanography (Introduction)
Overview of Planet Earth
Planet Earth is largely covered by water, with 71% of its surface being water and 29% land.
If all Earth’s water was condensed into a bubble, it would measure only 1,385 kilometers in diameter, highlighting the vastness of the planet.
Land Surface Composition
The land on Earth includes mountains, plateaus, and plains, with coastal plains extending as ocean floors.
Ocean Floor Divisions
Major Divisions
Continental Shelf:
An underwater landmass extending from continents, characterized by relatively shallow waters (30 meters to 600 meters deep).
The average width is about 80 kilometers, with variations; notably, the Siberian shelf in the Arctic Ocean is the largest at 1,500 kilometers wide.
Continental Slope:
Connects continental shelf to ocean basin; depth ranges from 200-3,000 meters, marked by a steep drop-off known as the shelf break.
Deep Sea Plains:
These are the flattest areas of the ocean basin, reaching depths up to 9,000 meters and covered with fine sediments like clay and silt.
Oceanic Deeps:
The deepest ocean sections, significant for plate tectonics due to associations with volcanoes and earthquakes.
Relief Features
Major and minor features include ridges, hills, seamounts, guyots, trenches, and canyons.
Coastal Regions
Littoral Zone
The littoral zone comprises regions close to shore, from the high water mark to submerged areas.
Subregions include:
Supralittoral Zone: Above the spring high tide line; regularly splashed but not submerged.
Eulittoral Zone (Intertidal Zone): Between high and low tide lines, regularly exposed and submerged.
Sublittoral Zone: Located below the eulittoral zone, remains submerged and aligns with the neritic zone around the continental shelf.
Pelagic Zone
The pelagic zone includes the water column in the open ocean, extending through various regions:
Epipelagic Zone: Surface to 200 meters, receives sunlight, allowing photosynthesis; known as the sunlight zone.
Mesopelagic Zone: Ranges from 200 to 1,000 meters; referred to as the twilight zone, home to bioluminescent organisms.
Bathypelagic Zone: Extends from 1,000 to 4,000 meters, characterized by immense pressure and dark conditions.
Abyssopelagic Zone: Encompasses depths over 4,000 meters, home to few species adapted to extreme conditions.
Oceanic Trenches and the Hadal Zone
Oceanic trenches are the deepest parts of the ocean, 3-5 kilometers deeper than the surrounding floor, significant for geological studies.
Key trenches include: Mariana Trench, Peru-Chile Trench, and Japan Trench.
The hadal zone encompasses extreme depths, characterized by high pressure and darkness, with few species, but hydrothermal vents support diverse life forms.
Hydrothermal vents release heated water and gases, hosting unique organisms like tube worms and clams.