
NSF Org: |
OCE Division Of Ocean Sciences |
Recipient: |
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Initial Amendment Date: | September 16, 2012 |
Latest Amendment Date: | September 16, 2012 |
Award Number: | 1220478 |
Award Instrument: | Standard Grant |
Program Manager: |
David Garrison
OCE Division Of Ocean Sciences GEO Directorate for Geosciences |
Start Date: | September 1, 2012 |
End Date: | August 31, 2017 (Estimated) |
Total Intended Award Amount: | $658,994.00 |
Total Awarded Amount to Date: | $658,994.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
1805 N BROAD ST PHILADELPHIA PA US 19122-6104 (215)707-7547 |
Sponsor Congressional District: |
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Primary Place of Performance: |
1900 N 12th St Philadelphia PA US 19122-6078 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): |
ANS-Arctic Natural Sciences, CRI-Ocean Acidification |
Primary Program Source: |
0100XXXXDB NSF RESEARCH & RELATED ACTIVIT |
Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
The Gulf of Mexico deep water ecosystems are threatened by the persistent threat of ocean acidification. Deep-water corals will be among the first to feel the effects of this process, in particular the deep-water scleractinians that form their skeleton from aragonite. The continued shoaling of the aragonite saturation horizon (the depth below which aragonite is undersaturated) will place many of the known, and as yet undiscovered, deep-water corals at risk in the very near future. The most common deep-water framework-forming scleractinian in the world's oceans is Lophelia pertusa. This coral is most abundant in the North Atlantic, where aragonite saturation states are relatively high, but it also creates extensive reef structures between 300 and 600 m depth in the Gulf of Mexico where aragonite saturation states were previously unknown. Preliminary data indicate that pH at this depth range is between 7.85 and 8.03, and the aragonite saturation state is typically between 1.28 and 1.69. These are the first measurements of aragonite saturation state for the deep Gulf of Mexico, and are among the lowest Aragonite saturation state yet recorded for framework-forming corals in any body of water, at any depth. This project will examine the effects of ocean acidification on L. pertusa, combining laboratory experiments, rigorous oceanographic measurements, the latest genome and transcriptome sequencing platforms, and quantitative PCR and enzyme assays to examine changes in coral gene expression and enzyme activity related to differences in carbonate chemistry. Short-term and long-term laboratory experiments will be performed at Aragonite saturation state of 1.45 and 0.75 and the organismal (e.g., survivorship and calcification rate) and genetic (e.g., transcript abundance) responses of the coral will be monitored. Genomic DNA and RNA will be extracted, total mRNA purified, and comprehensive and quantitative profiles of the transcriptome generated using a combination of 454 and Illumina sequencing technologies. Key genes in the calcification pathways as well as other differentially expressed genes will be targeted for specific qPCR assays to verify the Illumina sequencing results. On a research cruise, L. pertusa will be sampled (preserved at depth) along a natural gradient in carbonate chemistry, and included in the Illumina sequencing and qPCR assays. Water samples will be obtained by submersible-deployed niskin bottles adjacent to the coral collections as well as CTD casts of the water column overlying the sites. Water samples will be analyzed for pH, alkalinity, nitrates and soluble reactive phosphorus. These will be used in combination with historical data in a model to hindcast Aragonite saturation state.
Intellectual Merit: This project will provide new physiological and genetic data on an ecologically-significant and anthropogenically-threatened deepwater coral in the Gulf of Mexico. An experimental system, already developed by the PIs, offers controlled conditions to test the effect of Aragonite saturation state on calcification rates in scleractinians and, subsequently, to identify candidate genes and pathways involved in the response to reduced pH and Aragonite saturation state. Both long-term and population sampling experiments will provide additional transcriptomic data and specifically investigate the expression of the candidate genes. These results will contribute to our understanding of the means by which scleractinians may acclimate and acclimatize to low pH, alkalinity, and Aragonite saturation state. Furthermore, the investigators will continue a time series of oceanographic measurements of the carbonate system in the Gulf of Mexico, which will allow the inclusion of this significant body of water in models of past and future ocean acidification scenarios.
Broader Impacts: Results that combine the study of ongoing ocean acidification in the Gulf of Mexico with the physiological and genetic responses of the corals to low saturation state will be presented at conferences, seminars, and published in high-impact and open-access publications. Raw and processed data will be made available in existing databases including NCBI (genetic and genomic data), and through the Biological and Chemical Oceanography Data Management Office (BCO-DMO). All project data will also be made available via a local ftp server linked to each of the PIs websites. The PIs are committed to the inclusion of under-represented minorities in their research, and have a proven record of mentoring undergraduates at Temple University, one of the most diverse institutions in the U.S. A two-day workshop for 20 Gulf Coast high school teachers, and also including students from Temple, will be led by the PIs and coordinated by Dr. Shelia Brown at the Gulf Coast Research Lab in Ocean Springs, MS to provide teachers with the background and materials needed to bring curricula based on these results directly into their classrooms. A high school teacher will also participate in the cruise. Through these efforts, the investigators hope to raise public consciousness of the issue of ocean acidification, increase the level of awareness of the presence of deep-water coral communities in U.S. waters, and to inspire the next generation of scientists.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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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.
This study examined the effects of ocean acidification, the decline in pH that results as increasing levels of anthropogenic CO2 in the atmosphere equilibrate with the surface layers of the ocean. The first deep-water measurements of pH and aragonite saturation state (a measure of the relative availability of the mineral that corals use to make their skeleton) revealed that many deep-sea corals are living very close to the limits of what they can tolerate.
The principal aim of this project was to characterize the response of the deep-water coral Lophelia pertusa to the effects of ocean acidification. The first component of this work involved continuing our monitoring of ongoing ocean acidification in the deep Gulf of Mexico. Here, corals were collected and preserved at depth to examine their current physiological state and to compare differences in gene expression from sites with different aragonite saturation states. The second component of this project was to transplant live corals to the laboratory and maintain them in recirculating aquaria as part of a series of controlled experiments to determine the physiological (e.g., survivorship and growth) and gene expression responses to known aragonite saturation states. All together, this study provided our first comprehensive view of ocean acidification and deep-sea corals in US waters.
Since the initiation of this award, we have conducted several laboratory experiments on Lophelia pertusa. Using corals collected on research cruises prior to the start of the study, we completed a series of short-term (2 weeks) experiments on L. pertusa at a range of pH values. These experiments showed that different individual corals had different responses to low pH. We also included respirometry, growth, and feeding, and one of the graduate students on the study traveled to Sweden to complete the same experiments on the L. pertusa colonies from those waters. Surprisingly, corals from these populations responded very differently to lower pH, with the Gulf of Mexico corals slowing their metabolism and reducing feeding and growth rates, while the corals from the Tisler reef in Sweden elevated their feeding rate to provide the resources necessary to maintain calcification at low pH.
To assess whether L. pertusa is capable of acclimating to acidified conditions over longer time scales, we completed a six-month experiment to monitor changes in calcification and gene expression under control (pHT=7.9, Ωarag=1.5) and highly acidified (pHT=7.6, Ωarag=0.8) conditions. In 2014, we collected fresh coral colonies from the Gulf of Mexico for use in this experiment, and established two large experimental aquaria capable of being precisely controlled for temperature (±0.5°), salinity (±0.5 psu), pH (±0.04), and total alkalinity (±50 µmol kg-1). The corals were fragmented and six different genotypes were placed in each tank. The most significant finding of this study was that different coral colonies (genotypes) responded differently to lower pH and saturation state, providing a genetic basis for resilience to OA and the potential for adaptation. This was corroborated by the RNAseq results, which revealed the greatest variability among genotypes rather than among pH treatments. These results provide insight into the energetic mechanisms that currently allow L. pertusa to calcify at low saturation states, as well as its long-term potential for growth and survival under future acidification scenarios.
This study, representing the first characterization of the carbonate system in the deep Gulf of Mexico, has greatly expanded our understanding of the genetic and physiological mechanisms underlying the response of scleractinian corals to ocean acidification. The discovery of a significant genetic basis to the response to low pH and saturation state may be the most significant single finding of the project. This is a subject that is still being debated in the community, but the results of our series of experiments clearly show that, for this species anyway, there is ample genetic variability to provide an adaptive capacity to deal with ongoing ocean change.
This study also represents the first published transcriptome of the “lab rat” of deep-sea corals, Lophelia pertusa, and the first to examine changes in gene expression with altered pH. The major finding here was the significant difference in the transcriptomic response of the different genotypes, mirroring the differences in the physiological responses measured among the same genotypes. The identification of the genes underlying these responses will inform future research on shallow-water corals, since this system has the advantage of removing interference from the eukaryotic zoothanthellae that complicate the analysis of these data in scleractinian corals that rely on photosynthesis.
We have also collaborated on a documentary film about ocean acidification and deep-sea corals, which provided uniquely personal views of the inner workings of a large oceanographic research cruise. This film, “Acid Horizon” is currently in the application stages for major film festivals around the country and internationally and should appear in one or more of these venues in 2018.
Last Modified: 10/25/2017
Modified by: Rob J Kulathinal
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