Award Abstract # 2049604
Collaborative Research: US GEOTRACES GP17-OCE: Understanding neodymium isotopes and rare earth element systematics in the South Pacific

NSF Org: OCE
Division Of Ocean Sciences
Recipient: THE TRUSTEES OF COLUMBIA UNIVERSITY IN THE CITY OF NEW YORK
Initial Amendment Date: May 19, 2021
Latest Amendment Date: August 3, 2021
Award Number: 2049604
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, 2021
End Date: September 30, 2025 (Estimated)
Total Intended Award Amount: $469,092.00
Total Awarded Amount to Date: $469,092.00
Funds Obligated to Date: FY 2021 = $469,092.00
History of Investigator:
  • Sidney Hemming (Principal Investigator)
    sidney@ldeo.columbia.edu
  • Yingzhe Wu (Co-Principal Investigator)
Recipient Sponsored Research Office: Columbia University
615 W 131ST ST
NEW YORK
NY  US  10027-7922
(212)854-6851
Sponsor Congressional District: 13
Primary Place of Performance: Lamont-Doherty Earth Observatory
61 Route 9W
Palisades
NY  US  10964-1707
Primary Place of Performance
Congressional District:
17
Unique Entity Identifier (UEI): F4N1QNPB95M4
Parent UEI:
NSF Program(s): Marine Geology and Geophysics,
Special Initiatives,
Chemical Oceanography,
ANT Ocean & Atmos Sciences
Primary Program Source: 01002122DB NSF RESEARCH & RELATED ACTIVIT
0100XXXXDB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1620, 1670, 4444, 5113
Program Element Code(s): 162000, 164200, 167000, 511300
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

The goal of the international GEOTRACES program is to understand the distributions of multiple chemical elements and their isotopes in the oceans. The National Science Foundation is supporting a U.S. GEOTRACES sampling expedition in the South Pacific and Southern Ocean, one of the most remote and poorly sampled ocean regions on Earth. Neodymium (Nd) isotopes and rare earth elements (REE) are important tools used to track water masses along global circulation pathways, trace the sources of continental inputs into the oceans, and constrain biogeochemical processes in the water column. The investigators will analyze Nd isotopes and REE in seawater, suspended particles, and core top sediments on this expedition. The project will support an early career lead investigator, two postdoctoral researchers, and several undergraduate students. Outreach to local high schools and paid undergraduate research positions are designed to broaden participation in geosciences.

The GP17-OCE cruise track is well-designed for illuminating the processes that govern the marine cycling of REE and Nd isotopes, as it (i) covers the oligotrophic South Pacific Gyre, (ii) crosses the sub-tropical, sub-Antarctic and polar fronts, capturing transitions between different productivity regimes, (iii) traverses through the high latitude South Pacific, which hosts areas with extensive deep water upwelling and new water mass formation. It offers a unique opportunity to study biogeochemically important yet largely unsampled regions in the South Pacific at unprecedented detail. The investigators plan to (1) generate seawater Nd isotope and REE data to characterize the intermediate and deep water masses that form in the high latitude South Pacific, (2) decipher the evolution of dissolved Nd isotope and REE abundances across oceanic fronts and atmospheric dust flux gradients, (3) identify the roles of particle abundance, composition, and size in modulating dissolved Nd isotopes and REE, (4) evaluate the effect of REE contributions from the Antarctic and Chilean margins on water column Nd isotopes and REE inventory, (5) evaluate the impacts of the benthic flux of REE, (6) understand the process of signal transfer between the deep water and sedimentary archives (fossil fish teeth, Fe-Mn oxide coatings). This information is important for our understanding of Nd cycling in the global ocean and will also facilitate a thorough evaluation of the use of Nd isotopes as a past water circulation proxy.

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.

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