“…However, the rapid retreat of summertime sea ice cover has exposed these waters to the atmosphere, allowing for enhanced air-sea exchange, and increased the sink for atmospheric CO 2 from 24 TgC yr -1 to 66 TgC yr -1 over the past three decades . Furthermore, melting of sea ice reduces the CaCO 3 saturation state of seawater, primarily by reducing alkalinity (Steinacher et al, 2009 Polar marine invertebrates often exhibit low metabolic rates (Bluhm et al, 1998;Peck and Conway, 2000) and very slow development and growth (Pearse et al, 1991;Arntz et al, 1994;Coyle and Highsmith, 1994) are increasing in the north (Grebmeier et al, 2006, Cui et al, 2009), whereas ampeliscid amphipods that are the prey of gray whales are declining (Moore et al, 2003;Coyle et al, 2007). Whether these crustaceans will be impacted by increasing CO 2 levels in bottom waters is unknown.…”