Climate-driven oscillation of phosphorus and iron limitation in the North Pacific Subtropical Gyre

Ricardo M. Letelier, Karin M. Björkman, Matthew J. Church, Douglas S. Hamilton, Natalie M. Mahowald, Rachel A. Scanza, Niklas Schneider, Angelicque E. White, David M. Karl

Research output: Contribution to journalArticlepeer-review

56 Scopus citations

Abstract

The supply of nutrients is a fundamental regulator of ocean productivity and carbon sequestration. Nutrient sources, sinks, residence times, and elemental ratios vary over broad scales, including those resulting from climate-driven changes in upper water column stratification, advection, and the deposition of atmospheric dust. These changes can alter the proximate elemental control of ecosystem productivity with cascading ecological effects and impacts on carbon sequestration. Here, we report multi-decadal observations revealing that the ecosystem in the eastern region of the North Pacific Subtropical Gyre (NPSG) oscillates on subdecadal scales between inorganic phosphorus (Pi) sufficiency and limitation, when Pi concentration in surface waters decreases below 50–60 nmol·kg−1. In situ observations and model simulations suggest that sea-level pressure changes over the northwest Pacific may induce basin-scale variations in the atmospheric transport and deposition of Asian dust-associated iron (Fe), causing the eastern portion of the NPSG ecosystem to shift between states of Fe and Pi limitation. Our results highlight the critical need to include both atmospheric and ocean circulation variability when modeling the response of open ocean pelagic ecosystems under future climate change scenarios.

Original languageEnglish
Pages (from-to)12720-12728
Number of pages9
JournalProceedings of the National Academy of Sciences of the United States of America
Volume116
Issue number26
DOIs
StatePublished - 2019

Funding

ACKNOWLEDGMENTS. This research was funded by the NSF (HOT, OCE-1260164; Center for Microbial Oceanography: Research and Education, EF-0424599), the Gordon and Betty Moore Foundation’s Marine Microbiology Initiative (D.M.K.; Grant 3794), the Simons Foundation (Simons Collaboration on Ocean Processes and Ecology Award 329108; D.M.K., A.E.W., and M.J.C.), and the Balzan Foundation (D.M.K.). N.S. was supported by NSF Grant OCE-1357015 and by the Japan Agency for Marine–Earth Science and Technology and International Pacific Research Center Joint Initiative. N.M.M., R.A.S., and D.S.H. acknowledge support from the DOE (DE-SC0006791 and DESC0006735), the NSF (AGS-1049033), and high-performance computing from Yellowstone (ark:/85065/d7wd3xhc) provided by the National Center for Atmospheric Research’s Computational and Information Systems Laboratory, supported by the NSF. We are indebted to the research staff, as well as to the captains and crews of the various research vessels involved in supporting the HOT effort.

FundersFunder number
Japan Agency for Marine-Earth Science and Technology
EF-0424599, OCE-1260164
DE-SC0006791, DESC0006735, AGS-1049033, ark:/85065/d7wd3xhc
Simons Foundation329108
3794
National Center for Atmospheric Research
OCE-1357015

    Keywords

    • Atmospheric iron deposition
    • Climate
    • Pacific Decadal Oscillation
    • Pelagic ecosystem
    • Phosphorus limitation

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