Abstract

Ocean acidification (OA) will have a predominately negative impact on marine animals sensitive to changes in carbonate chemistry. Coastal upwelling regions, such as the Northwest coast of North America, are likely among the first ecosystems to experience the effects of OA as these areas already experience high pH variability and naturally low pH extremes. Over the past decade, pH off the Olympic coast of Washington has declined an order of magnitude faster than predicted by accepted conservative climate change models. Resource managers are concerned about the potential loss of intertidal biodiversity likely to accompany OA, but as of yet, there are little pH sensitivity data available for the vast majority of taxa found on the Olympic coast. The intertidal zone of Olympic National Park is particularly understudied due to its remote wilderness setting, habitat complexity, and exceptional biodiversity. Recently developed methodological approaches address these challenges in determining organism vulnerability by utilizing experimental evidence and expert opinion. Here, we use such an approach to determine intertidal organism sensitivity to pH for over 700 marine invertebrate and algal species found on the Olympic coast. Our results reinforce OA vulnerability paradigms for intertidal taxa that build structures from calcium carbonate, but also introduce knowledge gaps for many understudied species. We furthermore use our assessment to identify how rocky intertidal communities at four long-term monitoring sites on the Olympic coast could be affected by OA given their community composition.

Highlights

  • Ocean acidification (OA) is known to adversely affect the calcification, survival, metabolism, growth, development, and pH balance of many marine benthic (Orr et al, 2005; Kroeker et al, 2013; Gazeau et al, 2013) and pelagic (­Iglesias-Rodriguez et al, 2008; Riebesell and Tortell, 2011) organisms

  • The majority of all Olympic National Park (ONP) species are located in the low intertidal zone (71%), followed by the mid (21%) and high (8%) intertidal zones respectively

  • Eighty percent of ONP species are vulnerable to OA, with scores less than 0, and the other 20 percent are relatively invulnerable to OA, with scores ranging from 0 to 0.55 (Figure 2)

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Summary

Introduction

Ocean acidification (OA) is known to adversely affect the calcification, survival, metabolism, growth, development, and pH balance of many marine benthic (Orr et al, 2005; Kroeker et al, 2013; Gazeau et al, 2013) and pelagic (­Iglesias-Rodriguez et al, 2008; Riebesell and Tortell, 2011) organisms. In addition to natural processes, the contribution of anthropogenic CO2 to the ocean has increased since the Industrial Revolution (Le Quére et al, 2016) and accounts for roughly 70% of the dissolved inorganic carbon in upwelled surface water in the California Current (Feely et al, 2016). Taken together, these natural and human-derived stressors amplify the impacts of OA on the exceptionally biodiverse outer Washington coast

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