The bathyal zone, also called the bathypelagic zone, is the layer of open ocean spanning roughly one thousand to four thousand meters in depth, lying between the sunlit mesopelagic zone above and the abyssal zone below. It is sometimes called the midnight zone because no sunlight penetrates this far, which rules out photosynthesis and the plant life that depends on it. Temperature stays almost constant near four degrees Celsius, salinity holds steady between thirty three and thirty five grams per kilogram, and pressure ranges from about one hundred to four hundred atmospheres. Bioluminescence provides the only light most organisms here ever encounter. Conditions in this zone have stayed largely unchanged for thousands of years, and its sheer volume, larger than all the sunlit ocean layers above it combined, remains poorly explored because of the difficulty of studying water this deep.
Facts
Climate
Typical Low Temperature (C)Source describes the bathypelagic (bathyal) zone as a nearly constant temperature of about 4C rather than a range; the same figure is used for both the low and high value. Typical High Temperature (C)Source describes the bathypelagic (bathyal) zone as a nearly constant temperature of about 4C rather than a range; the same figure is used for both the low and high value. Cross-Tradition Connections
Sources
1. Bathyal Zone (Wikipedia)
WikipediaArticle body, opening description, temperature and salinity sentenceQuote, Article body, opening description, temperature and salinity sentence
The bathypelagic zone is characterized by a nearly constant temperature of approximately 4 °C (39 °F) and a salinity range of 33-35 g/kg.
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