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Does Presence of a Mid-Ocean Ridge Enhance Biomass and Biodiversity?

Figure 5

Spatial distribution of area backscatter.

Area backscattering coefficient (m2 nautical mile−2), from the mesopelagic deep scattering layer. Recordings from multi-ship surveys using calibrated SIMRAD 38 kHz echosounders integrating down to 750 m depth (1000 m after 1999). Composite image of data from 1996–2009 during June–July.

Figure 5

doi: https://doi.org/10.1371/journal.pone.0061550.g005