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The hydrothermal vents are recognized as a type of chemosynthetic based ecosystems (CBE) where primary productivity is fuelled by chemical compounds as energy sources instead of light (chemoautotrophy). [29] Hydrothermal vent communities are able to sustain such vast amounts of life because vent organisms depend on chemosynthetic bacteria for food.
The Dodo and Solitaire hydrothermal vent sites are much closer to the central Indian Ridge spreading center than the Edmond and Kairei vents and have much different fluid chemical compositions. [12] Rimicaris kairei shrimp are present in high numbers and are often the most populous animal on the Edmond and Kairei vent fields, with their highest ...
It was first discovered in 1997 in a black smoker hydrothermal vent at the Mid-Atlantic Ridge, setting the upper-temperature threshold for known life to exist at 113 °C (235.4 °F) with an optimal temperature of 106 °C. [1] This species "freezes" or solidifies and ceases growth at temperatures of 90 °C (194 °F) and below. [3]
Beside being a hotbed for organic compounds, the newfound site in the Arctic Ocean may be rich in copper and gold deposits.
The hydrothermal vent microbial community includes all unicellular organisms that live and reproduce in a chemically distinct area around hydrothermal vents. These include organisms in the microbial mat , free floating cells, or bacteria in an endosymbiotic relationship with animals.
The vents of such geysers are artificial, but are tapped into natural hydrothermal systems. These so-called artificial geysers, technically known as erupting geothermal wells, are not true geysers. Little Old Faithful Geyser, in Calistoga, California, is an example. The geyser erupts from the casing of a well drilled in the late 19th century ...
Pyrococcus furiosus is a strictly anaerobic, heterotrophic, sulfur-reducing archaea originally isolated from heated sediments in Vulcano, Italy by Fiala and Stetter. It is noted for its rapid doubling time of 37 minutes under optimal conditions, meaning that every 37 minutes the number of individual organisms is multiplied by two, yielding an exponential growth curve.
Hydrothermal circulation in the oceans is the passage of the water through mid-oceanic ridge systems.. The term includes both the circulation of the well-known, high-temperature vent waters near the ridge crests, and the much-lower-temperature, diffuse flow of water through sediments and buried basalts further from the ridge crests. [3]