Anagram & Information om | Engelska ordet APHOTIC

Exempel på hur man kan använda APHOTIC i en mening

• Above the aphotic zone is the photic zone, which consists of the euphotic zone and the disphotic zone.
• The mesopelagic zone (Greek μέσον, middle), also known as the middle pelagic or twilight zone, is the part of the pelagic zone that lies between the photic epipelagic and the aphotic bathypelagic zones.
• The off shore areas may be called the pelagic zone, the photic zone may be called the limnetic zone and the aphotic zone may be called the profundal zone.
• Extant carychiid snails inhabit aphotic and permanently wet epigean (Carychium) or subterranean (Zospeum) environments throughout their Holarctic distribution.
• The ocean zones can be grouped by light penetration into (from top to bottom): the photic zone, the mesopelagic zone and the aphotic deep ocean zone:.
• The correct words spelled by Kneale also included: fatigue, conceit, opalescent, carafe, egalitarian, supernumerary, persiflage, literati, aphotic, bellipotent, physiolatry, demulcent, hagiology, and sauerbraten.
• " PopMatters gave a positive assessment of the album, writing that "despite the songs' uniformity and very minimal use of codas rich in aphotic atmospheres, there is serious songcraft to be found within the shifting ferocity Watain emphasize since it is extremely difficult to arrange jolting transitions to flow together seamlessly.
• In the aphotic (lightless) part of caves, short-term growth of photosynthetic plants is possible thanks to the seed's nutritive tissue.
• It has been found that the hadal depth's prokaryotic SSU rRNA gene communities in the challenger deep are dominated by the bacteria SAR406 and bacteroidetes, and the deepest depths have an increase in gammaproteobacteria, which both contrast with the aphotic waters above that are dominated by SAR11 and thaumarchaeota.
• However, unlike the Sannine Formation sites, which were deposited in relatively shallow waters near the shore on the inner continental shelf, Sahel Alma was deposited in a deepwater habitat off the continental slope, at depths estimated to be greater than , likely at the transition between the sublittoral and bathyal zones in dysphotic or aphotic conditions.

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