
NSF Org: |
OCE Division Of Ocean Sciences |
Recipient: |
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Initial Amendment Date: | August 14, 2018 |
Latest Amendment Date: | August 14, 2018 |
Award Number: | 1830016 |
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: | August 15, 2018 |
End Date: | January 31, 2023 (Estimated) |
Total Intended Award Amount: | $488,427.00 |
Total Awarded Amount to Date: | $488,427.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
1251 MEMORIAL DR CORAL GABLES FL US 33146-2509 (305)421-4089 |
Sponsor Congressional District: |
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Primary Place of Performance: |
4600 Rickenbacker Causeway Miami FL US 33149-1031 |
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): |
BIOLOGICAL OCEANOGRAPHY, Chemical Oceanography |
Primary Program Source: |
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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 biological pump is largely responsible for the vertical transport of organic carbon from the surface to the ocean interior. However, only a small fraction of organic material produced in surface waters is sequestered in the deep ocean. The rest is consumed, or respired, by bacteria and larger organisms. The overarching goal of the proposed work is to characterize the relative influences of bacteria versus larger organisms on the degradation of organic material with depth. Guided by recent results from the subtropical Pacific, the investigators will use measurements of stable isotopes of nitrogen in different amino acids (compound-specific isotopic analysis of amino acids, known as AA-CSIA), along with measurements of the abundances of different forms of amino acids, and other parameters derived from these analyses to identify how the partitioning and flux of large and small particles are affected by different degradation processes. By improving the interpretive power of the AA-CSIA technique the investigators propose to determine: 1) the relative importance of microbial and zooplankton consumption on the efficiency of the biological carbon pump in the subarctic northeast Pacific, and 2) how much microbially-altered small particles fuel the metabolisms of mid-water zooplankton. This work capitalizes on an existing, comprehensive field program (NASA EXPORTS) specifically focused on building a predictive framework relating surface ocean properties to the vertical flux of organic carbon. The tremendous amount of data to be collected on all aspects of the biological pump as part of the EXPORTS program will aid the development and interpretation of the investigators' amino acid isotopic tool. Results will be broadly communicated via production and distribution of several episodes of Voice of the Sea, a local television program that will air in Hawaii and across many Pacific islands. Episodes also will be posted online and publicized through social media to the south Florida community. This project will support a Ph.D. student and an undergraduate student at University of Miami, which serves a 25% Hispanic population, and an M.S. student and an undergraduate student at University of Hawaii, which is a designated minority-serving institution.
The proposed work introduces a new geochemical framework to distinguish microbial versus zooplankton alteration of marine organic matter. Piloted on samples from the subtropical Pacific, this approach interrogates unamended sinking material directly, using amino acid compound-specific isotopic analysis (AA-CSIA) to determine the progressive, cumulative impact of microbial and zooplankton degradative pathways. The proposed work (1) will extend this interpretive framework to explicitly define end-member signatures such as fecal pellets and will apply this refined method to a study site in the subarctic northeast Pacific to (2) determine the vertical progression of degradative mechanisms in an oceanographic location with contrasting productivity and vertical length scales of flux attenuation and (3) determine whether microbially- degraded biomass is important for fueling midwater metazoans under contrasting carbon flux conditions. The proposed work will be conducted in collaboration with the NASA EXPORTS program at the Ocean Station Papa time-series site. Teaming with this program presents a unique opportunity to refine AA-CSIA interpretation in parallel with intensive data collection defining productivity, particle size distribution and flux, and numerous biological parameters. In comparing subtropical and subarctic Pacific locations, the proposed work will test how differences in productivity and plankton community structure influence vertical patterns of consumption and alteration of phytodetritus by microbes and zooplankton, from surface to mesopelagic depths.
This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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PROJECT OUTCOMES REPORT
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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.
Organic matter production in the upper-ocean and its vertical removal to the deep ocean sequesters atmospheric CO2 into long-timescale reservoirs thus removing CO2 from the atmosphere and storing it in the deep ocean. The biological pump is largely responsible for this vertical transport of organic carbon from the surface to the ocean interior. However, only a small fraction of organic material produced in surface waters is sequestered in the deep ocean. The rest is consumed, or respired, by bacteria and larger organisms. The efficiency of organic carbon transfer to the deep ocean is a highly sensitive parameter needed to predict future changes in the global carbon cycle and the ocean?s ability to take up CO2 from the atmosphere.
We used measurements of stable isotope ratios of carbon and nitrogen in different amino acids (compound-specific isotopic analysis of amino acids, known as AA-CSIA) of organic particles and zooplankton in the subarctic Pacific, a region of relatively low carbon flux to the deep ocean, along with measurements of the abundances of different forms of amino acids, and other parameters derived from these analyses to identify different mechanisms of organic matter degradation, with important implications for nutrient availability to deep-water food webs. Our results enabled us to developed two nascent models: (1) a mixing model that uses AA-CSIA to estimate the phytodetritus, fecal pellet, and microbially degraded composition of particles, such that the vertical alteration mechanisms and size distribution of these materials can be detected; and (2) an inverse relationship between carbon flux into the deep ocean and the reliance of deep ocean food webs on small, degraded particles. This work capitalized on existing, comprehensive field programs (NASA EXPORTS) specifically focused on building a predictive framework relating surface ocean properties to the vertical flux of organic carbon. The first EXPORTS field study in the subarctic Pacific provided us the materials from which the models were developed. The tremendous amount of data collected on all aspects of the biological pump as part of the EXPORTS program aided the development and interpretation of our amino acid isotopic tools.
Our work assessed the relative importance of packaging organic matter in fecal material, particle disaggregation, microbial reworking, and zooplankton dietary usage on vertical patterns of particle flux in the subarctic Pacific, using empirical methods independent of incubation techniques or metabolic rate measurements. Application and refinement of our newly-developed isotopic indicators will enable development of a globally generalized isotopic framework for assessing the degradative history of particulate organic matter and its relationship to mesopelagic dietary resources, including small, microbially degraded particles that are often not accounted for as a metazoan dietary resource. The work directly addressed EXPORTS Science Question 2: What controls the efficiency of vertical transfer of organic matter below the well-lit surface ocean? The results of this work additionally will provide observational comparisons to global models of carbon flux composition and pelagic food web resources.
Results of our work have been broadly communicated via production and distribution of several episodes of Voice of the Sea, a local television program that aired in Hawaii and across many Pacific islands. Episodes were also posted online and publicized through social media to the south Florida community, with Spanish translation available. Results have been published in open-access scientific journals and also presented at both national and international scientific meetings. This project supported graduate and undergraduate students at the University of Miami.
Last Modified: 08/15/2023
Modified by: Hilary G Close
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