When scientists first dove in Alvin and witnessed hydrothermal vents, they were not surprised by the eruptions of hot water. But they never anticipated finding life there. Without sunlight, they knew that photosynthesis could not be the basis of this community. Eventually they discovered a different way of producing food, chemosynthesis. Many more hydrothermal vents were discovered and many more types of vent organisms.
Conditions in the intertidal zone change rapidly as water covers and uncovers the region and waves pound on the rocks. A great abundance of life is found in the intertidal zone (Figure below). High energy waves hit the organisms that live in this zone, so they must be adapted to pounding waves and exposure to air during low tides. Hard shells protect from waves and also protect against drying out when the animal is above water. Strong attachments keep the animals anchored to the rock.
Organisms in a tide pool include sea stars and sea urchins.
In a tide pool, as in the photo, what organisms are found where and what specific adaptations do they have to that zone? The mussels on the top left have hard shells for protection and to prevent drying because they are often not covered by water. The sea anemones in the lower right are more often submerged and have strong attachments but can close during low tides.
Many young organisms get their start in estuaries and so they must be adapted to rapid shifts in salinity.
Corals and other animals deposit calcium carbonate to create rock reefs near the shore. Coral reefs are the “rainforests of the oceans,” with a tremendous amount of species diversity (Figure below).
Coral reefs are among the most densely inhabited and diverse areas on the globe.
Reefs can form interesting shapes in the oceans. Remember that hot spots create volcanoes on the seafloor. If these volcanoes rise above sea level to become islands, and if they occur in tropical waters, coral reefs will form on them. Since the volcanoes are cones, the reef forms in a circle around the volcano. As the volcano comes off the hot spot, the crust cools. The volcano subsides and then begins to erode away (Figure below).
In this image of Maupiti Island in the South Pacific, the remnants of the volcano are surrounded by the circular reef.
Eventually, all that is left is a reef island called an atoll. A lagoon is found inside the reef.
The open ocean is a vast area. Food either washes down from the land or is created by photosynthesizing plankton. Zooplankton and larger animals feed on the phytoplankton and on each other. Larger animals such as whales and giant groupers may live their entire lives in the open water.
How do fish survive in the deepest ocean? The few species that live in the greatest depths are very specialized (Figure below). Since it’s rare to find a meal, the fish use very little energy; they move very little, breathe slowly, have minimal bone structure and a slow metabolism. These fish are very small. To maximize the chance of getting a meal, some species may have jaws that unhinge to accept a larger fish or backward-folding teeth to keep prey from escaping.
An 1896 drawing of a deep sea angler fish with a bioluminescent “lure” to attract prey.
Hydrothermal vents are among the most unusual ecosystems on Earth since they are dependent on chemosynthetic organisms at the base of the food web. At mid-ocean ridges at hydrothermal vents, bacteria that use chemosynthesis for food energy are the base of a unique ecosystem (Figure below). This ecosystem is entirely separate from the photosynthesis at the surface. Shrimp, clams, fish, and giant tube worms have been found in these extreme places.
Giant tube worms found at hydrothermal vents get food from the chemosynthetic bacteria that live within them. The bacteria provide food; the worms provide shelter.
A video explaining hydrothermal vents with good footage is seen here:
Use this resource to answer the questions that follow.
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| Credit: Courtesy of the National Science Foundation Source: http://www.nsf.gov/news/overviews/earth-environ/assets/interact06.jpg License: Public Domain | ||
| Credit: Flickr:mountainamoeba Source: http://www.flickr.com/photos/mountainamoeba/696520153/ License: CC BY 2.0 | ||
| Credit: NOAA's National Ocean Service Source: http://www.flickr.com/photos/usoceangov/11177135805/ License: CC BY 2.0 | ||
| Credit: Courtesy of Robert Simmon and NASA's Earth Observatory Source: http://earthobservatory.nasa.gov/IOTD/view.php?id=41320 License: Public Domain | ||
| Credit: G Brown Goode and Tarleton H Bean Source: http://commons.wikimedia.org/wiki/File:Ceratias_holboelli.jpg License: Public Domain | ||
| Credit: Courtesy of the National Science Foundation Source: http://www.nsf.gov/news/overviews/earth-environ/assets/interact06.jpg License: Public Domain |
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