Award Abstract # 1756610
Collaborative Research: Quantifying trophic roles and food web ecology of salp blooms of the Chatham Rise

NSF Org: OCE
Division Of Ocean Sciences
Recipient: FLORIDA STATE UNIVERSITY
Initial Amendment Date: January 30, 2018
Latest Amendment Date: February 15, 2022
Award Number: 1756610
Award Instrument: Standard Grant
Program Manager: Cynthia Suchman
csuchman@nsf.gov
 (703)292-2092
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: May 1, 2018
End Date: April 30, 2023 (Estimated)
Total Intended Award Amount: $345,985.00
Total Awarded Amount to Date: $345,985.00
Funds Obligated to Date: FY 2018 = $345,985.00
History of Investigator:
  • Michael Stukel (Principal Investigator)
    mstukel@fsu.edu
Recipient Sponsored Research Office: Florida State University
874 TRADITIONS WAY
TALLAHASSEE
FL  US  32306-0001
(850)644-5260
Sponsor Congressional District: 02
Primary Place of Performance: Florida State University
Tallahassee
FL  US  32306-4520
Primary Place of Performance
Congressional District:
02
Unique Entity Identifier (UEI): JF2BLNN4PJC3
Parent UEI:
NSF Program(s): BIOLOGICAL OCEANOGRAPHY
Primary Program Source: 01001819DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1389, 8811
Program Element Code(s): 165000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Salps are unique open-ocean animals that range in size from a few millimeters to greater than twenty centimeters, have a gelatinous (jelly-like) body, and can form long chains of many connected individuals. These oceanic organisms act as oceanic vacuum cleaners, having incredibly high feeding rates on phytoplankton and, unusual for consumers of their size, smaller bacteria-sized prey. This rapid feeding and the salps' tendency to form dense blooms, allows them move substantial amounts of prey carbon from the surface into the deep ocean, leading to carbon dioxide removal from the atmosphere. However, salps are often considered a trophic dead-end, rather than a link, in the food web due to the assumption that they themselves are not consumed, since their gelatinous bodies are less nutritious than co-occurring crustacean prey. Along with this, salp populations are hypothesized to be increasing due to climate change. This proposal addresses these questions: 1) Do salps compete primarily with crustaceans (as in the prevailing paradigm) or are they competitors of single-celled protists, which are the dominant grazers of small phytoplankton? 2) Do salp blooms increase the efficiency of food-web pathways from tiny phytoplankton to fisheries production in nutrient-poor ocean regions?

This project will support the interdisciplinary education of a graduate student who will learn modeling and laboratory techniques in the fields of biological and chemical oceanography and stimulate international collaborations between scientists in the United States and New Zealand. Additionally, several Education and Outreach initiatives are planned, including development of a week-long immersive high school class in biological oceanography, and education modules that will serve the "scientists-in-the schools" program in Tallahassee, FL.

It is commonly assumed that salps are a trophic sink. However, this idea was developed before the discovery that protists (rather than crustaceans) are the dominant grazers in the open ocean and was biased by the difficulty of recognizing gelatinous salps in fish guts. More recent studies show that salps are found in guts of a diverse group of fish and seabirds and are a readily available prey source when crustacean abundance is low. This proposal seeks to quantify food web flows through contrasting salp-dominated and salp-absent water parcels near the Chatham Rise off western New Zealand where salp blooms are a predictable phenomenon. The proposal will leverage previously obtained data on salp abundance, bulk grazing impact, and biogeochemical significance during Lagrangian experiments conducted by New Zealand-based collaborators. The proposal will determine 1) taxon- and size-specific phytoplankton growth rate measurements, 2) taxon- and size-specific protozoan and salp grazing rate measurements, 3) compound specific isotopic analysis of the amino acids of mesozooplankton to quantify the trophic position of salps, hyperiid amphipods, and other crustaceans, 4) sediment traps to quantify zooplankton carcass sinking rates, and 5) linear inverse ecosystem modeling syntheses. Secondary production and trophic flows from this well-constrained ecosystem model will be compared to crustacean-dominated and microbial loop-dominated ecosystems in similarly characterized regions (California Current, Costa Rica Dome, and Gulf of Mexico).

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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Décima, Moira and Stukel, Michael R. and Nodder, Scott D. and Gutiérrez-Rodríguez, Andrés and Selph, Karen E. and dos Santos, Adriana Lopes and Safi, Karl and Kelly, Thomas B. and Deans, Fenella and Morales, Sergio E. and Baltar, Federico and Latasa, Mike "Salp blooms drive strong increases in passive carbon export in the Southern Ocean" Nature Communications , v.14 , 2023 https://doi.org/10.1038/s41467-022-35204-6 Citation Details
Fender, Christian K. and Décima, Moira and Gutiérrez-Rodríguez, Andres and Selph, Karen E. and Yingling, Natalia and Stukel, Michael R. "Prey size spectra and predator to prey size ratios of southern ocean salps" Marine Biology , v.170 , 2023 https://doi.org/10.1007/s00227-023-04187-3 Citation Details
Lüskow, Florian and Pakhomov, Evgeny A. and Stukel, Michael R. and Décima, Moira "Biology of Salpa thompsoni at the Chatham Rise, New Zealand: demography, growth, and diel vertical migration" Marine Biology , v.167 , 2020 https://doi.org/10.1007/s00227-020-03775-x Citation Details
Stukel, Michael_R and Décima, Moira and Landry, Michael_R and Selph, Karen_E "Nitrogen and Isotope Flows Through the Costa Rica Dome Upwelling Ecosystem: The Crucial Mesozooplankton Role in Export Flux" Global Biogeochemical Cycles , v.32 , 2018 https://doi.org/10.1029/2018GB005968 Citation Details
Stukel, Michael R. and Décima, Moira and Selph, Karen E. and GutiérrezRodríguez, Andres "Sizespecific grazing and competitive interactions between large salps and protistan grazers" Limnology and Oceanography , v.66 , 2021 https://doi.org/10.1002/lno.11770 Citation Details

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.

Salps are unique open-ocean animals that range in size from a few millimeters to greater than twenty centimeters, have a gelatinous (jelly-like) body, and can form long chains of many connected individuals (Figure 1). These oceanic organisms act as oceanic vacuum cleaners, having incredibly high feeding rates on algae (phytoplankton) and, unusual for consumers of their size, smaller bacteria-sized prey.  This rapid feeding and the salps? tendency to form dense blooms, allows them to move substantial amounts of prey carbon from the surface into the deep ocean (leading to carbon dioxide removal from the atmosphere).  However, salps are often considered a trophic dead-end, rather than a link, in the food web due to the assumption that they themselves are not consumed, since their gelatinous bodies are less nutritious than co-occurring crustacean prey.  Along with this, salp populations are hypothesized to be increasing due to climate change. 

Working with colleagues from New Zealand and the University of Hawaii, we have conducted the first whole ecosystem comparative food web analyses in similar regions with and without salp blooms.  Our research traced foodweb flows from nutrients through phytoplankton, protozoans, zooplankton, salps, and eventually into the deep sea.  This allows unprecedented understanding of the ecological and biogeochemical roles of these fascinating organisms.  Our findings include:

  • By measuring sinking particle rates beneath water with and without salps, we determined that the presence or absence of salps has a greater impact on marine carbon sequestration through sinking particles than changes in the taxonomic composition or net primary production of phytoplankton communities (Figures 2 and 3).  This suggests that marine biogeochemists need to focus more attention on potential future changes in zooplankton food web structure in order to predict alterations in the biological pump and global carbon cycle.
  • Using a suite of different measurement types including measurements of phytoplankton photosynthesis, zooplankton and salp grazing, and the trophic levels of different organisms in the ecosystem, we found that salp blooms increase the efficiency of trophic transfer because of their very high predator:prey size ratios (Figures 4 - 6).  This likely leads to higher biomass production of commercially valuable fish when salps are present than in their absence. 
  • By comparing salp grazing rates to the grazing rates of heterotrophic protists, we found that salps and protists engage in intraguild predation and can have different competitive/predatory interactions depending on the stage of a salp bloom.  When salp communities are dominated by adult taxa, the salps may primarily act as predators of protistan grazers (including mixotrophs and obligate heterotrophs).  We hypothesize that their intense grazing pressure on protistan communities may enhance the net growth rates of picoplankton.  These picoplankton can then serve as abundant prey for the subsequent generations of young salps.
  • All 7 species of salps preferentially retained nanoplankton (2 - 20 microns in diameter) relative to smaller picoplankton or larger microplankton.  This led to high predator:prey size ratios typically ranging from 1000:1 to 10,000:1.  For perspective, a 1000:1 predator:prey size ratio would be the equivalent of a lion feeding on a flea, while a 10,000:1 predator:prey size ratio would equate to a lion feeding on an amoeba (Figure 4).

These results are included in the 6 peer-reviewed manuscripts that have currently been published from this project, the one manuscript currently in review, and/or the four manuscripts that are in preparation for submission soon.  This project has also contributed to the education of three Ph.D. students.  18 datasets from this project are freely available through the BCO-DMO data archive: https://www.bco-dmo.org/project/754878

This project also supported the development of a week-long immersive high school class in biological oceanography (in partnership with the Illinois Math and Science Academy).  The course involved daily (~one-hour long) lectures about limitation in the pelagic ocean, phytoplankton production, and the biological carbon pump.  Following each lecture, the students were split into groups and given oceanographic datasets to analyze (including data from this project) to investigate the relationships driving primary production and export.  Groups then presented their results to each other.

Results from this project have been incorporated into three different courses taught at FSU (two graduate courses, and one undergraduate course).  The two graduate courses are plankton ecology and a biogeochemical modeling course   The undergraduate course was a newly-designed "flipped-classroom" course entitled "Applied mathematics for environmental and earth scientists".  Salp biology was introduced to these (non-oceanography) students through examples centered around using matrices to investigate changes in population structure and food webs, and included real problems based on our results from this project.  These topics were used to engage students with interesting oceanographic topics, while introducing them to key aspects of matrix algebra. 

 


Last Modified: 08/25/2023
Modified by: Michael R Stukel

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