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Carbonate chemistry data:
The pH, measured on the total hydrogen ion scale (pHT), was monitored daily at the down-stream end of the flumes with a handheld electrode (DG 115-SC electrode (Mettler-Toledo). Seawater carbonate chemistry and salinity were measured weekly, both in the day (02:00) and night (20:00); salinity was measured using a bench-top conductivity meter (Thermo Scientific, Orionstar A212, Waltham, MA, USA). The parameters of the seawater carbonate system were calculated from measurements of temperature, salinity, pHT, and AT, using the R package seacarb (Lavigne and Gattuso 2013).

Community composition:
~ 25% coral cover, comprised of 11% cover of massive Porites spp., 7% Porites rus, 4% Montipora spp. and 3% Pocillopora spp. There was ~ 7% cover of crustose coralline algae (CCA), with 4% Porolithon onkodes and 3% Lithophyllum kotschyanum, and ~ 5% cover of small pieces (i.e., ~ 1-cm diameter) of coral rubble (Fig. S2, Carpenter et al., 2018).&amp;quot;</gco:CharacterString>
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In recognition of the need for basic research concerning the nature, extent and impact of ocean acidification on oceanic environments in the past, present and future, the goal of the SEES: OA program is to understand (a) the chemistry and physical chemistry of ocean acidification; (b) how ocean acidification interacts with processes at the organismal level; and (c) how the earth system history informs our understanding of the effects of ocean acidification on the present day and future ocean.
Solicitations issued under this program:
NSF 10-530, FY 2010-FY2011
NSF 12-500, FY 2012
NSF 12-600, FY 2013
NSF 13-586, FY 2014
NSF 13-586 was the final solicitation that will be released for this program.
PI Meetings:
1st U.S. Ocean Acidification PI Meeting(March 22-24, 2011, Woods Hole, MA)
2nd U.S. Ocean Acidification PI Meeting(Sept. 18-20, 2013, Washington, DC)
3rd U.S. Ocean Acidification PI Meeting (June 9-11, 2015, Woods Hole, MA – Tentative)
NSF media releases for the Ocean Acidification Program:
Press Release 10-186 NSF Awards Grants to Study Effects of Ocean Acidification
Discovery Blue Mussels &quot;Hang On&quot; Along Rocky Shores: For How Long?
Discovery nsf.gov - National Science Foundation (NSF) Discoveries - Trouble in Paradise: Ocean Acidification This Way Comes - US National Science Foundation (NSF)
Press Release 12-179 nsf.gov - National Science Foundation (NSF) News - Ocean Acidification: Finding New Answers Through National Science Foundation Research Grants - US National Science Foundation (NSF)
Press Release 13-102 World Oceans Month Brings Mixed News for Oysters
Press Release 13-108 nsf.gov - National Science Foundation (NSF) News - Natural Underwater Springs Show How Coral Reefs Respond to Ocean Acidification - US National Science Foundation (NSF)
Press Release 13-148 Ocean acidification: Making new discoveries through National Science Foundation research grants
Press Release 13-148 - Video nsf.gov - News - Video - NSF Ocean Sciences Division Director David Conover answers questions about ocean acidification. - US National Science Foundation (NSF)
Press Release 14-010 nsf.gov - National Science Foundation (NSF) News - Palau's coral reefs surprisingly resistant to ocean acidification - US National Science Foundation (NSF)
Press Release 14-116 nsf.gov - National Science Foundation (NSF) News - Ocean Acidification: NSF awards $11.4 million in new grants to study effects on marine ecosystems - US National Science Foundation (NSF)</gco:CharacterString>
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                            <gco:CharacterString>&lt;p&gt;While coral reefs have undergone unprecedented changes in community structure in the past 50 y, they now may be exposed to their gravest threat since the Triassic. This threat is increasing atmospheric CO2, which equilibrates with seawater and causes ocean acidification (OA). In the marine environment, the resulting decline in carbonate saturation state (Omega) makes it energetically less feasible for calcifying taxa to mineralize; this is a major concern for coral reefs. It is possible that the scleractinian architects of reefs will cease to exist as a mineralized taxon within a century, and that calcifying algae will be severely impaired. While there is a rush to understand these effects and make recommendations leading to their mitigation, these efforts are influenced strongly by the notion that the impacts of pCO2 (which causes Omega to change) on calcifying taxa, and the mechanisms that drive them, are well-known. The investigators believe that many of the key processes of mineralization on reefs that are potentially affected by OA are only poorly known and that current knowledge is inadequate to support the scaling of OA effects to the community level. It is vital to measure organismal-scale calcification of key taxa, elucidate the mechanistic bases of these responses, evaluate community scale calcification, and finally, to conduct focused experiments to describe the functional relationships between these scales of mineralization.&lt;/p&gt;
&lt;p&gt;This project is a 4-y effort focused on the effects of Ocean Acidification (OA) on coral reefs at multiple spatial and functional scales. The project focuses on the corals, calcified algae, and coral reefs of Moorea, French Polynesia, establishes baseline community-wide calcification data for the detection of OA effects on a decadal-scale, and builds on the research context and climate change focus of the Moorea Coral Reef LTER.&lt;/p&gt;
&lt;p&gt;This project is a hypothesis-driven approach to compare the effects of OA on reef taxa and coral reefs in Moorea. The PIs will utilize microcosms to address the impacts and mechanisms of OA on biological processes, as well as the ecological processes shaping community structure. Additionally, studies of reef-wide metabolism will be used to evaluate the impacts of OA on intact reef ecosystems, to provide a context within which the experimental investigations can be scaled to the real world, and critically, to provide a much needed reference against which future changes can be gauged.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;Datasets listed in the &quot;Dataset Collection&quot; section include references to results journal publications published as part of this project.&lt;/strong&gt;&lt;/p&gt;</gco:CharacterString>
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http://lod.bco-dmo.org/id/dataset-parameter/794277.rdf
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	Units: microatmospheres (μatm)
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http://lod.bco-dmo.org/id/dataset-parameter/794278.rdf
	Name: pCO2_Night
	Units: microatmospheres (μatm)
	Description: &lt;p&gt;pCO2 averaged during nightime hours. Calculated using seacarb by Lavigne and Gattuso 2013.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/794279.rdf
	Name: DIC_24h
	Units: micromoles per kilogram (μmol kg-1)
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http://lod.bco-dmo.org/id/dataset-parameter/794280.rdf
	Name: DIC_Day
	Units: micromoles per kilogram (μmol kg-1)
	Description: &lt;p&gt;DIC averaged during daylight hours. Calculated using seacarb by Lavigne and Gattuso 2013.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/794281.rdf
	Name: DIC_Night
	Units: micromoles per kilogram (μmol kg-1)
	Description: &lt;p&gt;DIC averaged during nightime hours. Calculated using seacarb by Lavigne and Gattuso 2013.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/794282.rdf
	Name: TA_24h
	Units: micromoles per kilogram (μmol kg-1)
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http://lod.bco-dmo.org/id/dataset-parameter/794283.rdf
	Name: TA_Day
	Units: micromoles per kilogram (μmol kg-1)
	Description: &lt;p&gt;Alkalinity averaged during daylight hours. Potentiometric titration.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/794284.rdf
	Name: TA_Night
	Units: micromoles per kilogram (μmol kg-1)
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http://lod.bco-dmo.org/id/dataset-parameter/794285.rdf
	Name: Omega_24h
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	Description: &lt;p&gt;Aragonite saturation state averaged across 24 h. Calculated using seacarb by Lavigne and Gattuso 2013.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/794286.rdf
	Name: Omega_Day
	Units: omega aragonite (Ωa)
	Description: &lt;p&gt;Aragonite saturation state averaged during daylight hours. Calculated using seacarb by Lavigne and Gattuso 2013.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/794287.rdf
	Name: Omega_Night
	Units: omega aragonite (Ωa)
	Description: &lt;p&gt;Aragonite saturation state averaged during nightime hours. Calculated using seacarb by Lavigne and Gattuso 2013.&lt;/p&gt; 
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Carbonate chemistry data:
The pH, measured on the total hydrogen ion scale (pHT), was monitored daily at the down-stream end of the flumes with a handheld electrode (DG 115-SC electrode (Mettler-Toledo). Seawater carbonate chemistry and salinity were measured weekly, both in the day (02:00) and night (20:00); salinity was measured using a bench-top conductivity meter (Thermo Scientific, Orionstar A212, Waltham, MA, USA). The parameters of the seawater carbonate system were calculated from measurements of temperature, salinity, pHT, and AT, using the R package seacarb (Lavigne and Gattuso 2013).

Community composition:
~ 25% coral cover, comprised of 11% cover of massive Porites spp., 7% Porites rus, 4% Montipora spp. and 3% Pocillopora spp. There was ~ 7% cover of crustose coralline algae (CCA), with 4% Porolithon onkodes and 3% Lithophyllum kotschyanum, and ~ 5% cover of small pieces (i.e., ~ 1-cm diameter) of coral rubble (Fig. S2, Carpenter et al., 2018).&amp;quot;</gco:CharacterString>
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