Award Abstract # 1136345
Dimensions: Collaborative Research: Functional Diversity of Marine Eukaryotic Phytoplankton and Their Contributions to the C and N Cycling

NSF Org: OCE
Division Of Ocean Sciences
Recipient: THE TRUSTEES OF PRINCETON UNIVERSITY
Initial Amendment Date: September 22, 2011
Latest Amendment Date: March 15, 2016
Award Number: 1136345
Award Instrument: Standard Grant
Program Manager: David Garrison
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: January 1, 2012
End Date: June 30, 2016 (Estimated)
Total Intended Award Amount: $1,399,879.00
Total Awarded Amount to Date: $1,401,584.00
Funds Obligated to Date: FY 2011 = $1,399,879.00
FY 2016 = $1,705.00
History of Investigator:
  • Bess Ward (Principal Investigator)
  • Daniel Sigman (Co-Principal Investigator)
Recipient Sponsored Research Office: Princeton University
1 NASSAU HALL
PRINCETON
NJ  US  08544-2001
(609)258-3090
Sponsor Congressional District: 12
Primary Place of Performance: Princeton University
NJ  US  08544-1042
Primary Place of Performance
Congressional District:
12
Unique Entity Identifier (UEI): NJ1YPQXQG7U5
Parent UEI:
NSF Program(s): Dimensions of Biodiversity,
BIOLOGICAL OCEANOGRAPHY
Primary Program Source: 01001112DB NSF RESEARCH & RELATED ACTIVIT
01001617DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1650, 9117, 9169, EGCH, 7968
Program Element Code(s): 796800, 165000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Intellectual Merit: Phytoplankton form the basis of the marine food web and thus are a crucial element in the biological pump whereby CO2 from the atmosphere is sequestered in the deep ocean. For decades, biological oceanography focused on the eukaryotic phytoplankton. In the 1970-80s, it was discovered that the single celled picocyanobacteria are numerically dominant in the oceans and are responsible for a large fraction of ocean photosynthesis. What ensued was the growth of a new paradigm in which the picocyanobacteria dominate upper ocean biology and biogeochemistry. In fact, new data support the classic view that the eukaryotic phytoplankton are disproportionately important in both N and C cycling, even in regions where very small cells dominate the biomass and where the eukaryotes themselves are in the "pico" size fraction. In oligotrophic environments, where very small cells dominate, in situ recycling appears to supply most of the nitrogen (i.e., ammonium) required for primary production. New nitrate supply must balance N loss from the system, however, and new data suggest that this nitrate is an important contribution to phytoplankton N, even in the oceanic deserts. It is not known whether the nitrate supply in these systems is used by the entire assemblage or predominantly by larger phytoplankton (essentially entirely eukaryotic). On the basis of still quite limited molecular surveys, we now recognize that the diversity of both large and small eukaryotic phytoplankton is greater than previously thought and that the most abundant and widespread eukaryotes are probably not in culture and may not be closely related to known cultivated organisms. This project will investigate the taxonomic, genetic and functional diversity of eukaryotic phytoplankton at two North Atlantic sites (subarctic and subtropical) in two seasons.
The PIs will use diagnostic microarrays for community analysis based on functional genes (both DNA and RNA) and next generation sequencing (i.e., transcriptomics using 454 technology) to identify the players, both in terms of community composition and activity, and to explore the functional diversity of the natural assemblage. In order to identify which groups are active in C and N assimilation and which N source is being utilized by the different size and functional groups, both filter-separated and flow cytometry-sorted samples will be used to 1) measure 13C primary production and 15N assimilation by incubations with isotope tracers, 2) measure the natural stable N isotope signatures of different taxonomic groups and 3) link the molecular diversity to the functional diversity in C and N transformations. Using flow cytometry linked to mass spectrometry, these investigators have found an unexpectedly strong differentiation in the form of N assimilated by prokaryotes and eukaryotes, with eukaryotes being more dynamic.

Integration: This project will investigate the taxonomic, genetic and functional diversity of eukaryotic phytoplankton and to link this diversity and assemblage composition to the carbon and nitrogen biogeochemistry of the surface ocean. Taxonomic diversity will be investigated by identifying the components of the phytoplankton assemblages using molecular, chemical and microscope methods. Genetic diversity will be explored at several levels, including direct sequencing of clone libraries of key functional genes and metatranscriptomic sequencing and microarray analysis of size fractionated/sorted phytoplankton assemblages. Using natural abundance and tracer stable isotope methods, genetic and taxonomic diversity will be linked to functional diversity in C and N assimilation in size- fractionated and taxon-sorted populations.

Broader Impacts: The broader impacts of this project include contributions to fundamental research and education: 1) continued development of new advanced methods of isotope analysis in environmental samples, with increasing breadth of applications in biogeochemistry and biodiversity; 2) undergraduate teaching in foundation courses on climate and environmental science to recruit freshmen and sophomore students into the science majors; 3) undergraduate research experience through internships and senior thesis research (a requirement at Princeton) for upper level undergraduates; 4) training the next generation of microbial ecology/ biogeochemistry researchers through classroom and research experience at the graduate level. In addition, a new module will be created (The Forests and Deserts of the Ocean) for the Princeton outreach program for middle school teachers (QUEST, Questioning Underlies Effective Science Teaching).

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Smart, S. M., S. E. Fawcett, S. J. Thomalia, M. A. Weigand, C. J. C. Reason, D. M. Sigman. "Isotopic evidence for nitrification in the Antarctic winter mixed layer." Global Biogeochemical Cycles , 2015 10.1002/2014GB005013
Fawcett, S. E., B. B Ward, M. W. Lomas, D. M. Sigman "Vertical decoupling of nitrate assimilation and nitrification in the Sargasso Sea" Deep Sea Research Part 1: Oceanographic Research Papers , 2015 10.1016/j.dsr.2015.05.004
Ward, B. B. and N. C. Van Oostende "Phytoplankton assemblage during the North Atlantic spring bloom assessed from functional gene analysis." Journal of Plankton Research , 2016 10.1093/plankt/fbw043
Treibergs, L. A., S. E. Fawcett, M. W. Lomas, D. M. Sigman "Nitrogen isotopic response of prokaryotic and eukaryotic phytoplankton to nitrate availability in Sargasso Sea surface waters." Limnology and Oceanography , 2014 10.4319/lo.2014.59.3.0972
Fawcett, S. E., B. B Ward, M. W. Lomas, D. M. Sigman "Vertical decoupling of nitrate assimilation and nitrification in the Sargasso Sea" Deep Sea Research Part 1: Oceanographic Research Papers , 2015 doi: 10.1016/j.dsr.2015.05.004
Fawcett, S. E., M. W. Lomas, B. B. Ward and D. M. Sigman. "The counterintuitive effect of summer-to-fall mixed layer deepening on eukaryotic new production in the Sargasso Sea" Global Biogeochemical Cycles , 2014 10.1002/2013GB004579
Fawcett, S. E., M. W. Lomas, B. B. Ward and D. M. Sigman. "The counterintuitive effect of summer-to-fall mixed layer deepening on eukaryotic new production in the Sargasso Sea" Global Biogeochemical Cycles , 2014 doi: 10.1002/2013GB004579

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