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The area is at the marine limit and most of the sediments have been deposited in the sea.
Disturbances commonly occurred on slopes between 4 and 15°, below Holocene marine limit, and in areas with low potential incoming solar radiation.
The Holocene marine limit along the Soya Coast is estimated to have been approximately 18 m above the mean sea level (AMSL), based on radiocarbon analyses of in situ bivalve fossils from raised beach deposits (Laternula elliptica; Miura et al. 1998).
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Although a few species of zooplankton, mesopelagic fish, and squids have adapted their metabolism to temporarily (through diel vertical migration) or permanently inhabit OMZs, most marine species limit their distribution to the surface oxygenated layer [5], [6].
Sparse measurements of MeHg concentrations in marine ecosystems limit our ability to relate atmospheric Hg deposition changes to MeHg levels in marine fish (Sunderland et al. 2009).
The evolution of cost efficient swimming in marine mammals: limits to energetic optimization.
Further investigation of hybrid smolt-to-adult survival is needed to determine whether or not the marine phase limits hybrid introgression.
The data presented here support the theory that the marine phase limits hybrid production; testing this would involve genetic analysis of returning adults to determine if the proportion of hybrids decreased from that seen among the smolts.
In constrast, the scarcity of population genetic and phylogeographic studies on Southern Ocean marine organisms limits our understanding of Southern populations.
In contrast to traditional management approaches (including size limits and effort limits), marine reserves for mobile or migratory species may not enhance fisheries or provide effective protection from the ecological consequences of overexploitation (Hannesson 1998; Hilborn et al. 2004; Kaiser 2005).
In this population, pregnant women should choose freshwater over marine fish and limit fish consumption.
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