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The parallel reflectors at the top of Fig. 5a from the surface to 1 m depth form the first layer.
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This was the case of several alphaproteobacterial sequences shared by samples coming from 66.2 m to 78.8 m depth that formed 3 OTUs affiliated to the genus Sphingomonas or Sphingobium.
The first one from 20- to 75-m depth was formed by coarse sand and another one from 115- to 230-m depth was formed by fine to medium sand.
No leaching of N (of any form) was found to 2.7 m depth during the three year monitoring period after fertiliser application.
The modeled 3-D subsurface temperature distribution is presented in the form of temperature-depth maps for each 1000 m depth interval (Fig. 10), as well as cross sections (Fig. 11).
The top of the mount forms a plateau at 15 to 25 m depth, with a surface area of 4.5 km2.
The shallow-water form of Saccharina japonica (SHA) inhabits the supralittoral zone (0.1 – 0.5 m depth) and it is widely distributed in the Primorye coast region, the Sea of Japan, including Peter the Great Bay.
Five coalesced vents forming an undulating shallow bowl-shaped diatreme contained within the Gellibrand Marl (240 m depth) were modelled to satisfy the observed magnetic response, while a large sill body at 350 m depth is modelled to satisfy the observed gravity response.
Cenozoic sediment extends to 2800 3000 m depth.
Both were located in 15 20 m depth.
is still lowest around 200 m depth but is higher at depths greater than 600 m than in shallower regions.
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