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Lying hundreds of metres below the sea and deeper still below sediments, fire ice is exceedingly difficult to extract.
To investigate the reflection retrieval from interfaces below sediments, an effective method involves the investigation of the characteristics of the synthetic waveform/ACF calculated with a more realistic velocity model rather than the previous simulations.
As will be discussed below, sediment resuspension, which provide active denitrifiers from benthic hotspot, accounts for the "driving force" of severe N removal within overlying oxygenated water.
Metals were generally below sediment quality guidelines except for nickel and arsenic.
Sediment coring is needed to determine if peat is in fact held in below-surface sediments (e.g., [18, 22, 42]).
They probably were formed by the melting of ice driven from the poles and deposited at lower latitudes during periods of high obliquity (see below Polar sediments, ground ice, and glaciers).
Below the sediments, the crystalline basement is encountered at 1.4- to 5.0-km depth (Figure 1) and exhibits several indications of convection associated with the fracture system that ranges from micro-cracks to local faults.
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