Biogeosciences, 17, 2315–2339, 2020 https://doi.org/10.5194/bg-17-2315-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Ocean deoxygenation and copepods: coping with oxygen minimum zone variability Karen F. Wishner1, Brad Seibel2, and Dawn Outram1 1Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 02882, USA 2College of Marine Science, University of South Florida, St. Petersburg, FL 33701, USA Correspondence: Karen F. Wishner (
[email protected]) Received: 27 September 2019 – Discussion started: 28 October 2019 Revised: 31 March 2020 – Accepted: 2 April 2020 – Published: 24 April 2020 Abstract. Increasing deoxygenation (loss of oxygen) of compression concept). These distribution depths changed by the ocean, including expansion of oxygen minimum zones tens to hundreds of meters depending on the species, oxygen (OMZs), is a potentially important consequence of global profile, and phenomenon. For example, at the lower oxycline, warming. We examined present-day variability of vertical the depth of maximum abundance for Lucicutia hulsemannae distributions of 23 calanoid copepod species in the East- shifted from ∼ 600 to ∼ 800 m, and the depth of diapause for ern Tropical North Pacific (ETNP) living in locations with Eucalanus inermis shifted from ∼ 500 to ∼ 775 m, in an ex- different water column oxygen profiles and OMZ inten- panded OMZ compared to a thinner OMZ, but remained at sity (lowest oxygen concentration and its vertical extent in similar low oxygen levels in