Award Abstract # 1316047
Ocean Acidification: Collaborative Research: Quantifying the potential for biogeochemical feedbacks to create 'refugia' from ocean acidification on tropical coral reefs

NSF Org: OCE
Division Of Ocean Sciences
Recipient: UNIVERSITY OF CALIFORNIA SAN DIEGO
Initial Amendment Date: July 1, 2013
Latest Amendment Date: September 12, 2014
Award Number: 1316047
Award Instrument: Standard Grant
Program Manager: Henrietta Edmonds
hedmonds@nsf.gov
 (703)292-7427
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: July 1, 2013
End Date: June 30, 2018 (Estimated)
Total Intended Award Amount: $751,301.00
Total Awarded Amount to Date: $751,301.00
Funds Obligated to Date: FY 2013 = $751,301.00
History of Investigator:
  • Jennifer Smith (Principal Investigator)
    smithj@ucsd.edu
  • Todd Martz (Co-Principal Investigator)
Recipient Sponsored Research Office: University of California-San Diego Scripps Inst of Oceanography
8622 DISCOVERY WAY # 116
LA JOLLA
CA  US  92093-1500
(858)534-1293
Sponsor Congressional District: 50
Primary Place of Performance: UCSD, Scripps Inst. of Oceanography
9500 Gilman Dr., MC 0210
La Jolla
CA  US  92093-0210
Primary Place of Performance
Congressional District:
50
Unique Entity Identifier (UEI): QJ8HMDK7MRM3
Parent UEI: QJ8HMDK7MRM3
NSF Program(s): CRI-Ocean Acidification
Primary Program Source: 01001314DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1382, 1670, 4444
Program Element Code(s): 800100
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Rising sea surface temperatures and ocean acidification (OA) may threaten the ability of calcified organisms to build carbonate reefs, but it is unclear if particular reefs have the capacity to tolerate global change. Current understanding of the effects of OA on coral reefs originates from single-species laboratory studies largely focused on scleractinian corals. Traditionally, these experiments attempt to mimic static future conditions under the assumption that coastal regimes are as constant as -- and will acidify at the same rate as -- open ocean surface waters. Predictions based on these oversimplified scenarios are unrealistic because numerous benthic organisms, including calcifiers and primary producers, significantly alter the bulk seawater carbonate chemistry over a diurnal cycle. Further, the prevalence of recently appreciated extreme diel fluctuations in pH across some reefs suggests that benthic species may be acclimated to future carbonate conditions.

To look for potential OA refugia on reefs, a research team from the Scripps Institute of Oceanography (University of California at San Diego) and the Lamont Dougherty Earth Observatory (Columbia University) will undertake a unique mechanistic study on Palmyra Atoll, a remote uninhabited island in the central Pacific that lacks degradation from local human influence. They will explore the strengths and controls of biogeochemical feedbacks from coral reef benthic community assemblages to the seawater chemistry above and experimentally determine how this natural fluctuation affects physiological responses of key taxa to OA. Specifically they will: (1) tightly integrate a novel benthic flux technique in situ that allows continuous, high-temporal resolution measurements of net ecosystem metabolic rates (production and calcification) with an ongoing high spatial resolution benthic community dynamics study to quantify feedbacks of known species assemblages to observed natural spatiotemporal variability in seawater carbonate chemistry; and (2) use small scale common garden CO2 enrichment experiments and productivity/respiration assays in the lab paired with reciprocal transplant experiments in situ to empirically quantify the effects of elevated and/or fluctuating pCO2 on growth, calcification and photophysiology of common framework building organisms and their benthic competitors. This should allow them to examine the coupled interactions between OA and diverse benthic coral reef organisms in their natural environment in the absence of other confounding human impacts.

BROADER IMPACTS. Ocean acidification is expected to affect a number of ecosystem goods and services that human societies have come to depend on. Specifically, the physical protection that coral reefs provide from coastal erosion will be reduced, potentially exacerbating the effects of sea level rise, and the effects of OA on fisheries and tourism are yet to be determined. One central goal is to work with local communities and organizations to better educate the public about how OA will affect people, societies and the natural resources they use and to give individuals tools that can allow them to be part of the solution. To that end, the research team has established strong partnerships with a local non-profit public broadcasting service KPBS, San Diego to develop novel products for OA communication and education. Further, they will work with the Birch Aquarium at SIO to develop an exhibit that communicates the results of the project. Finally, the project will directly train interns, students and researchers and will promote diversity through a variety of outreach activities including public lectures, training of aquarium docents and the development of web-based educational materials.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Johnson M.D., Price N.N., Smith J.E. "Contrasting effects of ocean acidification on tropical fleshy and calcareous algae." PeerJ 2:e411. , 2014 , p.http://dx
Kram SL, Price NN, Donham Em, Johnson MD, Kelly ELA, Hamilton SL and Smith JE "Variable responses of temperate calcified and fleshy macroalgae to ocean acidification and warming" ICES Journal of Marine Science. Special Issue on Ocean Acidification , 2015
Smith, J.E., S.A. Sandin, P.S. Vroom, I. Williams, E. Sala, D. Obura, R. Brainard, A. Carter, S. Grillo, C. Edwards, L. Lewis, J. Harris "Baselines and evidence of human impact on coral reefs across the central Pacific" Proceedings of the Royal Society, Biology , 2016 , p.DOI: 10.1
Takeshita, Y. "Understanding feedbacks between ocean acidification and coral reef metabolism" Journal of Geophysical Research-Oceans, , 2017 , p.doi:10.10
Takeshita, Y., C. A. Frieder, T. R. Martz, J. R. Ballard, R. A. Feely, S. Kram, S. Nam, M. O. Navarro, N. N. Price, and J. E. Smith "Including high frequency variability in coastal ocean acidification projections" Biogeosciences , 2015 , p.doi:10.51
Takeshita, Y., Cyronak, T., Martz, T. R., Kindeberg, T., and Andersson, A. J. "Drivers of coral reef carbonate chemistry variability at different functional scales." Frontiers in Marine Science. , 2018 , p.doi:10.33
Takeshita, Y., McGillis, W., Briggs, E. M., Carter, A., Donham, E. M., Martz, T. R., Price, N. N., and Smith, J. E. "Assessment of net community production and calcification of a coral reef using a boundary layer approach." Journal of Geophysical research-Oceans , v.121 , 2016 , p.1-17 doi:10.1002/2016JC011886
Takeshita, Y., W. McGillis, E. M. Briggs, A. Carter, E. Donham, T. R. Martz, N. N. Price, and J. E. Smith "Assessment of net community production and calcification of a coral reef using a boundary layer approach" Journal of Geophysical Research-Oceans , 2016 , p.doi:10.10
Yuichiro Takeshita "Understanding feedbacks between ocean acidification and coral reef metabolism" Journal of Geophysical Research: Oceans , v.122 , 2017 , p.1639 doi:10.1002/2017JC012740

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

The ability of coral reef ecosystems to "build reefs" is determined by their ability ro deposit calcium carbonate over time. This ‘net calcification’, is a key process that is fundamental for coral reef health. Ocean acidification is thought to reduce net calcification rates on coral reefs by lowering seawater pH, making it either harder for corals to deposit skeletons, or easier for existing skeletons to dissolve. However, the tools to measure net calcification rates in the field are time and labor intensive, usually requiring collection of water samples and returning them to the lab for analysis using sophisticated instrumentation. This limits our ability to detect and study how ocean acidification is impacting coral reefs in the natural world.

In this project, we developed the Benthic Ecosystem Acidification Measurement System (BEAMS), a fully autonomous system that measures in situ net calcification rates in coral reefs. BEAMS utilizes chemical sensors to measure net calcification rates at ~15 minute intervals for weeks to months. We tested and validated this new method on Palmyra Atoll, a pristine coral reef atoll in the central Pacific. Surprisingly, we found no relationship between seawater pH and net calcification rates over a 2 week period, highlighting the importance of making in situ measurements to accurately assess the impacts of ocean acidification on net calcification. We have deployed BEAMS in over a dozen reefs worldwide, and are currently working on adapting the method for other coastal ecosystems.

 


Last Modified: 09/24/2018
Modified by: Jennifer E Smith

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