Abstract

Coastal acidification in southeastern U.S. estuaries and coastal waters is influenced by biological activity, run-off from the land, and increasing carbon dioxide in the atmosphere. Acidification can negatively impact coastal resources such as shellfish, finfish, and coral reefs, and the communities that rely on them. Organismal responses for species located in the U.S. Southeast document large negative impacts of acidification, especially in larval stages. For example, the toxicity of pesticides increases under acidified conditions and the combination of acidification and low oxygen has profoundly negative influences on genes regulating oxygen consumption. In corals, the rate of calcification decreases with acidification and processes such as wound recovery, reproduction, and recruitment are negatively impacted. Minimizing the changes in global ocean chemistry will ultimately depend on the reduction of carbon dioxide emissions, but adaptation to these changes and mitigation of the local stressors that exacerbate global acidification can be addressed locally. The evolution of our knowledge of acidification, from basic understanding of the problem to the emergence of applied research and monitoring, has been facilitated by the development of regional Coastal Acidification Networks (CANs) across the United States. This synthesis is a product of the Southeast Coastal and Ocean Acidification Network (SOCAN). SOCAN was established to better understand acidification in the coastal waters of the U.S. Southeast and to foster communication among scientists, resource managers, businesses, and governments in the region. Here we review acidification issues in the U.S. Southeast, including the regional mechanisms of acidification and their potential impacts on biological resources and coastal communities. We recommend research and monitoring priorities and discuss the role SOCAN has in advancing acidification research and mitigation of and adaptation to these changes.

Highlights

  • Ocean acidification generally refers to the oceanic pH decrease and associated changes in chemical speciation in dissolved inorganic carbon (DIC) that occurs as a result of absorption of atmospheric carbon dioxide

  • Performance declined in moderate hypoxia (50% air saturation), when pCO2 was elevated to 19,700 μatm in the same hypoxic conditions, performance improved

  • Regional scale measurements of seafloor elevation change throughout the Florida Reef Tract (FRT) show significant erosion of coral reefs and the surrounding seafloor that has caused water depths to increase to levels not expected until near the year 2100, indicating that carbonate production is insufficient to keep pace with erosion and sea level rise (Yates et al, 2017)

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Summary

INTRODUCTION

Ocean acidification generally refers to the oceanic pH decrease and associated changes in chemical speciation in dissolved inorganic carbon (DIC) that occurs as a result of absorption of atmospheric carbon dioxide. SOCAN was formed in January 2015 and serves as both an information network and catalyst for discussions among interested parties about the state of acidification science, providing a forum for understanding and addressing coastal and ocean acidification concerns. It aims to foster enhanced communication among stakeholders within the region, including hosting a state-of-the-science webinar series and workshops on acidification. Our understanding of acidification and how to mitigate these changes at a regional scale has evolved recently to consider the global contribution of atmospheric carbon dioxide to the ocean but the many other mechanisms of acidification that can impact coastal waters. ACIDIFICATION IN THE U.S SOUTHEAST: FROM A GLOBAL PROBLEM TO A LOCAL WATER QUALITY ISSUE

Offshore Waters
Inshore Waters
LOW DISSOLVED OXYGEN AND ACIDIFICATION
SOCIOECONOMIC IMPACTS IN THE SOUTHEAST
Establishing SOCAN
Advancing Monitoring Priorities
SOCAN Stakeholders
SOCAN Looking Forward
Findings
AUTHOR CONTRIBUTIONS
Full Text
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