The California Current System (CCS) contains one of the five major
coastal upwelling zones in the world's oceans, and hosts a great diversity and abundance of marine life [1].
Not exact matches
These include eastern boundary current
upwelling systems such as those off the U.S. west coast along
coastal California, Oregon and Washington, deep - sea and subsurface oxygen minimum
zones, and
coastal waters that are already experiencing excess nutrient levels (eutrophication) and low dissolved oxygen (hypoxia) due to human - driven nutrient pollution from land - based activities.
However, the conditions predicted for the open ocean may not reflect the future conditions in the
coastal zone, where many of these organisms live (Hendriks et al. 2010a, b; Hofmann et al. 2011; Kelly and Hofmann 2012), and results derived from changes in pH in
coastal ecosystems often include processes other than OA, such as emissions from volcanic vents, eutrophication,
upwelling and long - term changes in the geological cycle of CO2, which commonly involve simultaneous changes in other key factors affecting the performance of calcifiers, thereby confounding the response expected from OA by anthropogenic CO2 alone.
Since phytoplankton form the base of marine food webs, the world's most productive fisheries are located in areas of
coastal upwelling that bring cold nutrient rich waters to the surface (especially in the eastern boundary regions of the subtropical gyres); about half the world's total fish catch comes from
upwelling zones.