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The first principal component calculated from species abundances separated the two transects from the 1000 1500 m depth stratum from the others indicating that sediment food supply influences community structure and composition.
Perhaps the most interesting pattern relates to the 151 300 m depth stratum.
On the shelf (here the 50 150 m depth stratum) both AvTD and VarTD increased with latitude, as seen with macrobenthos on the Norwegian and European shelves.
This likely optimizes the overall conditions at the 1 m depth stratum for macroalgae, with variations to this pattern based on locally different conditions.
Peaks were found in the mid latitudes around 45 60°N, with a sharp drop at 70°N in the Arctic (only at the 5 m depth stratum).
For example, only the 5 m depth stratum was sampled in the Arctic Beaufort Sea as this is the only depth with hard substrate for macroalgal growth.
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A different rocky shore study that was restricted to the Gulf of Alaska [38] and included macroalgae, polychaetes, echinoderms and molluscs, concluded that, while these groups as a whole showed greatest richness at the low intertidal and 1 m depth strata, regional variation within and among different taxa prevented a generalization of trends for each of the four taxonomic groups across the region.
The sampling design adopted was random-stratified according to the following depth strata: 400 600 m; 600 800 m; 800 1,000 m; 1,000 1,200 m.
The soil is idealized by single homogeneous strata of 30 m depth beneath the foundation.
Freshwater is the major recharge source in the upper section of the Holocene strata, between the surface and 8.00 m depth, and the hydrochemical type has changed from ClNa to Cl·HCO3Na.
The ITS network shows a clear distinction between shallow (<600 m), mid (1000 1500 m) and deep water (>1500 m) populations of D. dianthus (Fig. 2b) with no haplotypes found in more than one depth stratum, suggesting genetic differentiation is more tightly linked to depth than geographic region.
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