Award Abstract # 1232814
GEOTRACES Pacific Section: Characterizing biogenic trace elements across productivity and oxygen gradients in the eastern South Pacific

NSF Org: OCE
Division Of Ocean Sciences
Recipient: BIGELOW LABORATORY FOR OCEAN SCIENCES
Initial Amendment Date: September 19, 2012
Latest Amendment Date: September 19, 2012
Award Number: 1232814
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: October 1, 2012
End Date: September 30, 2016 (Estimated)
Total Intended Award Amount: $399,960.00
Total Awarded Amount to Date: $399,960.00
Funds Obligated to Date: FY 2012 = $399,960.00
History of Investigator:
  • Benjamin Twining (Principal Investigator)
    btwining@bigelow.org
Recipient Sponsored Research Office: Bigelow Laboratory for Ocean Sciences
60 BIGELOW DR
EAST BOOTHBAY
ME  US  04544-5700
(207)315-2567
Sponsor Congressional District: 01
Primary Place of Performance: Bigelow Laboratory for Ocean Sciences
ME  US  04575-0475
Primary Place of Performance
Congressional District:
01
Unique Entity Identifier (UEI): DRTAEZWWJHM8
Parent UEI:
NSF Program(s): Chemical Oceanography
Primary Program Source: 01001213DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 9150, 9189, EGCH
Program Element Code(s): 167000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Incorporation of trace elements (TE) into plankton, and the chemical, geological, biological and biochemical mechanisms which influence this process, are of central importance to our understanding of the biogeochemical functioning of the oceans. Bioactive TEs such as Fe, Zn, Co, Cu and Ni have the potential to control ocean productivity, ecosystem structure, and the utilization of macronutrients in large regions of the global ocean. Numerous laboratory studies have been performed to study the responses of cellular TE quotas in model strains to varying environmental conditions, but accurate measurements of TE stoichiometries in cells and biogenic material collected from natural communities are rare. Measurements of bulk particulate TE stoichiometries typically rely on comparison to laboratory results to assess the biogenic component, precluding study of cellular responses to geochemical gradients.

In this project, investigators at the Bigelow Laboratory for Ocean Sciences and the University of Maine will measure TEs in plankton cells representing major functional groups and in bulk particulate matter along the US GEOTRACES South Pacific Zonal Transect from Peru to Tahiti in 2013. U.S.GEOTRACES is the US component of the international GEOTRACES program which was initiated to advance our knowledge of the concentrations, physical and chemical speciation, and spatial distributions of TEs in the ocean. The Pacific transect will run from a highly productive eastern boundary upwelling system with an intense oxygen minimum zone to the southeast Pacific gyre, one of the world's most oligotrophic regimes. Specifically, the investigators expect to accomplish the following objectives: (1) Measure cellular quotas of P, Si, Mn, Fe, Co, Ni, Cu and Zn in major functional groups of phytoplankton across horizontal productivity gradients in the eastern tropical South Pacific Ocean; (2) Measure cellular quotas of P, Si, Mn, Fe, Co, Ni, Cu and Zn in phytoplankton and bacteria across vertical redox gradients in the OMZ of the eastern tropical South Pacific Ocean; ( 3) Measure total and labile concentrations of Al, Ti, P, Mn, Fe, Co, Ni, Cu, Zn, Cd, V and Mo in bulk particulate material collected from the upper 500 m with GO-Flo bottles.

Broader Impacts: The broader impacts and environmental relevance of this research will be communicated to educators and the general public through a dedicated webinar series to be organized in coordination with COSEE-Ocean Systems. This series will involve 5 webinars delivered sequentially and covering the science results produced by this project, as well as results and synthesis from four other GEOTRACES projects from the South Pacific cruise. These seminars will describe the broader goals and significance of the international GEOTRACES program, promoting this global geochemical program to educators and citizens, as well as synthesizing findings on various aspects of the project (dissolved, particulate, and biogenic trace metals; metal binding ligands; natural radionuclide tracers). Information from GEOTRACES will also be introduced to undergraduate students through Bigelow's REU program and through an undergraduate course being taught to students at nearby Colby College.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Ohnemus, D. C., Rauschenberg, S., Cutter, G. A., Fitzsimmons, J. N., Sherrell, R. M. and Twining, B. S. "Elevated trace metal content of prokaryotic communities associated with marine oxygen deficient zones" Limnology and Oceanography , 2016 doi:10.1002/lno.10363, 2016

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.

Much like crops in a field that need fertilizer to grow, microscopic plants in the oceans (called phytoplankton) also require nutrients from their environment. Growing phytoplankton cells consume nutrients and carbon dioxide from the atmosphere to build their bodies. After these cells die, some of the associated nutrients and carbon sink into the ocean, feeding fisheries and subsurface ecosystems and removing carbon from the atmosphere. Because of the enormous size of the oceans—and the Pacific in particular, which is larger than all the continents combined—phytoplankton growth affects the entire planet’s biological and elemental cycles.  Some nutrients, especially metals such as iron, zinc, nickel, copper and cobalt, are very rare in the oceans because of their solubility and low abundance in terrestrial material, so their availability is known to be a major factor in how much and which types of phytoplankton grow in parts of the ocean. Through our laboratory’s participation in the international GEOTRACES program, funded by this NSF grant award, we studied how organisms in the vast and understudied South Pacific utilize metals and other nutrients in building their bodies. This research allows us and other scientists to better understand how ocean ecosystems of different types (near-shore, offshore, near-surface, deep) function and to predict how the ocean and planet will respond to environmental conditions in the future.

 

Our lab develops and uses state-of-the-art techniques to collect phytoplankton (and other marine particles) from the ocean and to examine their metal content without contaminating them. In one technique, phytoplankton are filtered from seawater onto clean filters that are later treated with a range of acids and other chemicals to determine the bulk amount of metals associated with particles in a given volume of seawater. In another technique, we examine single phytoplankton cells of a range of types (both large and small cells from a range of taxonomic groups) and examine them individually using x-rays at the Advanced Photon Source, a synchrotron facility run by the Department of Energy. Statistical techniques and data analyses over the large natural gradients of the South Pacific—and comparison with data collected by other GEOTRACES-participating laboratories—showed several surprising trends in metal utilization. We learned that organisms living in the low-oxygen subsurface waters of a huge portion of the east Pacific use much higher levels of metals than phytoplankton growing at the surface. This discovery changes how we think about the biological requirement for these metals in other ocean regions with low-oxygen waters, including many coastal ecosystems important to human industry and health. We showed that different metals are returned to seawater at different rates and depths, which affects how quickly they can be re-used. We also applied new statistical techniques to show the distributions of various chemical forms of the particulate metals. These distributions improve our ability to understand and predict how ocean ecosystems fundamentally work. We also learned that phytoplankton in the open Pacific Ocean have much lower concentrations of some metals such as iron and zinc than phytoplankton collected near the coast. This information helps us to model the behavior of metals and phytoplankton in computer simulations of the ocean.

 

In addition to the scientific advances, this project helped train several college researchers, local high school students, and post-doctoral researchers in Maine. Students and researchers attended international science meetings to present their findings. The project strengthened inter-state and international research collaborations and allowed participation by American scientists in worldwide research efforts including GEOTRACES. Public talks and lectures via Bigelow’s Café Scientifique and open house events and a publicly-available webinar program distributed by collaborators at the University of Maine were given as part of the project. These activities advanced public understanding of the scientific process and the environment. Data gathered by the project was also incorporated into college course materials via Bigelow’s collaboration with Colby College.

 

The data collected as part of this project are publically available online:

http://www.bco-dmo.org/dataset/643270

http://www.bco-dmo.org/dataset/648543

http://www.bco-dmo.org/dataset/639847


Last Modified: 01/02/2017
Modified by: Benjamin S Twining

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