Award Abstract # 1443474
Collaborative Research: Investigating Iron-inding Ligands in Southern Ocean Diatom Communities: The Role of Diatom-Bacteria Associations

NSF Org: OPP
Office of Polar Programs (OPP)
Recipient: UNIVERSITY OF RHODE ISLAND
Initial Amendment Date: June 10, 2015
Latest Amendment Date: June 10, 2015
Award Number: 1443474
Award Instrument: Standard Grant
Program Manager: Paco Moore
fbmoore@nsf.gov
 (703)292-5376
OPP
 Office of Polar Programs (OPP)
GEO
 Directorate for Geosciences
Start Date: July 15, 2015
End Date: June 30, 2020 (Estimated)
Total Intended Award Amount: $400,430.00
Total Awarded Amount to Date: $400,430.00
Funds Obligated to Date: FY 2015 = $400,430.00
History of Investigator:
  • Bethany Jenkins (Principal Investigator)
    bjenkins@uri.edu
Recipient Sponsored Research Office: University of Rhode Island
75 LOWER COLLEGE RD RM 103
KINGSTON
RI  US  02881-1974
(401)874-2635
Sponsor Congressional District: 02
Primary Place of Performance: University of Rhode Island
120 Flagg Road
Kingston
RI  US  02881-2015
Primary Place of Performance
Congressional District:
02
Unique Entity Identifier (UEI): CJDNG9D14MW7
Parent UEI: NSA8T7PLC9K3
NSF Program(s): ANT Organisms & Ecosystems
Primary Program Source: 0100XXXXDB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 9150
Program Element Code(s): 511100
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.078

ABSTRACT

This project focuses on an important group of photosynthetic algae in the Southern Ocean (SO), diatoms, and the roles associated bacterial communities play in modulating their growth. Diatom growth fuels the SO food web and balances atmospheric carbon dioxide by sequestering the carbon used for growth to the deep ocean on long time scales as cells sink below the surface. The diatom growth is limited by the available iron in the seawater, most of which is not freely available to the diatoms but instead is tightly bound to other compounds. The nature of these compounds and how phytoplankton acquire iron from them is critical to understanding productivity in this region and globally. The investigators will conduct experiments to characterize the relationship between diatoms, their associated bacteria, and iron in open ocean and inshore waters. Experiments will involve supplying nutrients at varying nutrient ratios to natural phytoplankton assemblages to determine how diatoms and their associated bacteria respond to different conditions. This will provide valuable data that can be used by climate and food web modelers and it will help us better understand the relationship between iron, a key nutrient in the ocean, and the organisms at the base of the food web that use iron for photosynthetic growth and carbon uptake. The project will also further the NSF goals of training new generations of scientists and of making scientific discoveries available to the general public. The project supports early career senior investigators and the training of graduate and undergraduate students as well as outreach activities with middle school Girl Scouts in Rhode Island, inner city middle and high school age girls in Virginia, and middle school girls in Florida.

The project combines trace metal biogeochemistry, phytoplankton cultivation, and molecular biology to address questions regarding the production of iron-binding compounds and the role of diatom-bacterial interactions in this iron-limited region. Iron is an essential micronutrient for marine phytoplankton. Phytoplankton growth in the SO is limited by a lack of sufficient iron, with important consequences for carbon cycling and climate in this high latitude regime. Some of the major outstanding questions in iron biogeochemistry relate to the organic compounds that bind >99.9% of dissolved iron in surface oceans. The investigators' prior research in this region suggests that production of strong iron-binding compounds in the SO is linked to diatom blooms in waters with high nitrate to iron ratios. The sources of these compounds are unknown but the investigators hypothesize that they may be from bacteria, which are known to produce such compounds for their own use. The project will test three hypotheses concerning the production of these iron-binding compounds, limitations on the biological availability of iron even if present in high concentrations, and the roles of diatom-associated bacteria in these processes. Results from this project will provide fundamental information about the biogeochemical trigger, and biological sources and function, of natural strong iron-binding compound production in the SO, where iron plays a critical role in phytoplankton productivity, carbon cycling, and climate regulation.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Alderkamp A.C., van Dijken, G.L., Lowry, K.E., Lewis, K.M., Warren, H.J., van de Poll, W., Laan, P., Gerringa, L., Delmont. T., Jenkins, B.D., Arrigo, K.R. "Effects of iron and light availability on phytoplankton photosynthetic properties in the Ross Sea" Marine Ecology Progress Series , 2019 10.3354/meps13000

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.

Intellectual Merit: Diatoms are a group of highly diverse microscopic marine organisms that convert light energy into cellular carbon and produce oxygen via photosynthesis. Diatoms are responsible for 40% of the carbon fixed in the ocean and a quarter of the oxygen we breathe on earth. Diatoms also are important food that sustains life amongst larger organisms in the marine food chain. In the Southern Ocean proximal to Antarctica, diatoms are an important food source for krill a favored food for whales and penguins. Diatoms are sensitive to their surrounding nutrients that they need for growth. In the Southern Ocean, most nutrients are ample but a critical nutrient for photosynthesis, iron, is at growth limiting conditions.  Experiments conducted by other researchers have shown that when exogenous Fe is supplied to this region, large diatoms blooms and can carry their carbon to the deep ocean where it serves as a carbon sink. The research in this award sought to understand diatom populations, how they change in different iron concentrations and how different species are distinct in their genetic responses to iron. We worked collaboratively in a team of molecular biologists and ocean chemists to do this work.

The Jenkins lab has deep expertise in molecular biology and we applied these tools to understand not only diatoms but bacteria that associate with them and may influence iron supply to the diatoms. We used methods such as molecular barcoding to delineate diatom populations, and analysis of global gene expression in lab experiments (transcriptomics) and in communities (metatranscriptomics) to understand diatom response to environmental conditions and nutrient concentrations. We found that iron along with salinity gradients structure diatom populations. We found that different diatoms remodel their metabolism in distinct ways in response to iron supply, for example modulating nitrogen metabolism. We found that distinct diatom species associate with distinct bacteria, indicating that there may be ecological stability in these associations and these bacterial associations might be part of a microbiome to help diatoms get the iron they need for growth. Our work helps us understand when a diatom species is present how it might be adapted to certain conditions and as environments change can speak to species that may become more or less prevalent under changing conditions. Species composition and function can have significant implications for the marine carbon cycle as well as food web dynamics in the Southern Ocean.

 Broader Impacts: This research was used as content for high enrollment microbiology courses at the University of Rhode Island. It was used to train the next generation of STEM students at the elementary school, middle school, high school, undergraduate and graduate levels. Elementary school and middle school students were brought to our lab at URI through Science and Math Investigative Learning Experience (SMILE) Fourth Grade Ecology Days and junior high Girl Scouts of Rhode Island. High School curricula and students were significantly enriched through a partnership between the Jenkins lab and the classrooms of Ms. Cara Pekarcik at N. Quincy High School in MA supported through the PolarTREC program. Ms. Pekarcik sailed on our research cruise and together we supported blogs and live streamed media accessible to her students and others through the internet. Undergraduate and Graduate students, including those from traditionally underrepresented groups in STEM were trained directly on the research in this project. Graduate students traveled to the Southern Ocean aboard the US Icebreaker Nathaniel B. Palmer and directly mentored undergraduates in the Jenkins lab prior to and after the research expedition.

 


Last Modified: 01/14/2021
Modified by: Bethany D Jenkins

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