Documentary overview

About Hydrothermal Vents | Oases in the Deep Sea

The process of chemosynthesis is similar to photosynthesis. Both can be defined as the creation of organic matter from the fixation of inorganic carbon using energy. But what differs is the source of that energy. In parts of the deep sea, primary production is fuelled by chemical energy, rather than energy from the sun. But this can only take place at certain sea-floor environments where the required chemicals are released into the water. The two main examples of such environments are hydrothermal vents, and cold seeps. The former were only discovered in 1977 when scientists were exploring an oceanic spreading ridge near the Galapagos Islands. What they discovered was a hidden world that revolutionised our understanding of how and where life on Earth can exist. Since then, hundreds more vent field have been discovered, often at depths of 2km or more, along Earth’s convergent plate boundaries and at sea-floor spreading regions where the oceanic crust is moving apart. Written, Narrated and Edited by Leo Richards Vent Animation custom made by Fabio Albertelli and Jakub Misiek I do not own any

Hydrothermal Vents | Oases in the Deep Sea is presented by Natural World Facts. Its listed runtime is 20 minutes. The source link and publisher attribution are provided with the embedded film.

As a society documentary, Hydrothermal Vents | Oases in the Deep Sea uses hydrothermal, vents, oases as its central frame. Social documentaries work best as invitations to examine systems through lived experience. Distinguish individual testimony from wider claims, and consider which institutions, incentives and inequalities shape the choices shown.

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  1. What evidence, testimony or observation does the film use to explain hydrothermal, vents, oases?
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Film information

Documentary details and original source

Title
Hydrothermal Vents | Oases in the Deep Sea
Category
Society
Runtime
20 minutes
Language
English

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