Vertical zonation and distributions of calanoid copepods through the lower oxycline of the Arabian Sea oxygen minimum zone

By K. Wishner, C. Gelfman, M. Gowing, Dawn M. Outram, Mary Rapien, Rebecca Williams. 2008

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Zooplankton in the eastern tropical north Pacific: Boundary effects of oxygen minimum zone expansion (2013, unknown): “…oxygen gradients (oxyclines) at the upper and lower boundaries create microhabitats of differing oxygen concentration that are characterized by layers of high zooplankton biomass and abundance, with distinct species zonation (Saltzman and Wishner, 1997a,b; Wishner et al., 1995, 1998, 2000, 2008).”
Impacts of hypoxia on the structure and processes in pelagic communities (zooplankton, macro-invertebrates and fish) (2009, background): “Oxygen minimum zones (OMZ) have an important impact on the vertical distribution and migratory patterns of pelagic organisms (Saltzman and Wishner, 1997a, b; Wishner et al., 2008).”
Mesopelagic zone ecology and biogeochemistry - a synthesis (2010, background): “…currents, shear zones, internal tides and eddies, as well as the microhabitats created by suspended and sinking particles, aggregates, colloids, gels and chemical plumes (Sameoto, 1986; Turley and Stutt, 2000; Kiørboe and Jackson, 2001; Pearre, 2003; Azam and Malfatti, 2007; Wishner et al., 2008).”
Ocean oxygen minima expansions and their biological impacts (2010, background): “Differential tolerance of major taxa yields dominance of specific copepods, pyrosomes, salps, and jellyfish in the hypoxic water column (Childress and Siebel, 1998; Wishner et al., 2008) and dominance of nematodes and small annelids in hypoxic sediments (Levin, 2003).”