Anthropogenic iron alters the spring phytoplankton bloom in the North Pacific transition zone

N Nicholas J. Hawco (Department of Oceanography, University of Hawai’i at Mānoa) T Tim M. Conway (College of Marine Science, University of South Florida) S Sacha N. Coesel (School of Oceanography, University of Washington) B Benedetto Barone (Department of Oceanography, University of Hawai’i at Mānoa) E Emily A. Seelen (Department of Earth Sciences, University of Southern California) S Shun-Chung Yang (Department of Earth Sciences, University of Southern California) R Randelle M. Bundy (School of Oceanography, University of Washington) P Paulina Pinedo-Gonzalez (Department of Earth Sciences, University of Southern California) X Xiaopeng Bian (Department of Earth Sciences, University of Southern California) M Matthias Sieber (College of Marine Science, University of South Florida) N Nathan T. Lanning (Department of Oceanography, Texas A&M University) J Jessica N. Fitzsimmons (Department of Oceanography, Texas A&M University) R Rhea K. Foreman (Department of Oceanography, University of Hawai’i at Mānoa) D Daniela König M Mora J. Groussman (School of Oceanography, University of Washington) J James G. Allen (Department of Oceanography, University of Hawai’i at Mānoa) L Lauren W. Juranek (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University) A Angelicque E. White (Department of Oceanography, University of Hawai’i at Mānoa) D David M. Karl (Department of Oceanography, University of Hawai’i at Mānoa) E E. Virginia Armbrust (School of Oceanography, University of Washington) S Seth G. John (Department of Earth Sciences, University of Southern California)

Abstract

Industrial activities have increased the supply of iron to the ocean, but the magnitude of anthropogenic input and its ecological consequences are not well-constrained by observations. Across four expeditions to the North Pacific transition zone, we document a repeated supply of isotopically light iron from an atmospheric source in spring, reflecting an estimated 39 ± 9 % anthropogenic contribution to the surface ocean iron budget. Expression of iron-stress genes in metatranscriptomes, and evidence for colimitation of ecosystem productivity by iron and nitrogen, indicates that enhanced iron supply should spur spring phytoplankton blooms, accelerating the seasonal drawdown of nitrate delivered by winter mixing. This effect is consistent with regional trends in satellite ocean color, which show a shorter, more intense spring bloom period, followed by an earlier arrival of oligotrophic conditions in summer. Continued iron emissions may contribute to poleward shifts in transitional marine ecosystems, compounding the anticipated impacts from ocean warming and stratification.

Article Details

Volume / Issue Vol. 122, Issue 23
Published June 10, 2025
ISSN 0027-8424
Publisher National Academy of Sciences

Authors (21)

N

Nicholas J. Hawco

Department of Oceanography, University of Hawai’i at Mānoa

T

Tim M. Conway

College of Marine Science, University of South Florida

S

Sacha N. Coesel

School of Oceanography, University of Washington

B

Benedetto Barone

Department of Oceanography, University of Hawai’i at Mānoa

E

Emily A. Seelen

Department of Earth Sciences, University of Southern California

S

Shun-Chung Yang

Department of Earth Sciences, University of Southern California

R

Randelle M. Bundy

School of Oceanography, University of Washington

P

Paulina Pinedo-Gonzalez

Department of Earth Sciences, University of Southern California

X

Xiaopeng Bian

Department of Earth Sciences, University of Southern California

M

Matthias Sieber

College of Marine Science, University of South Florida

N

Nathan T. Lanning

Department of Oceanography, Texas A&M University

J

Jessica N. Fitzsimmons

Department of Oceanography, Texas A&M University

R

Rhea K. Foreman

Department of Oceanography, University of Hawai’i at Mānoa

D

Daniela König

M

Mora J. Groussman

School of Oceanography, University of Washington

J

James G. Allen

Department of Oceanography, University of Hawai’i at Mānoa

L

Lauren W. Juranek

College of Earth, Ocean, and Atmospheric Sciences, Oregon State University

A

Angelicque E. White

Department of Oceanography, University of Hawai’i at Mānoa

D

David M. Karl

Department of Oceanography, University of Hawai’i at Mānoa

E

E. Virginia Armbrust

School of Oceanography, University of Washington

S

Seth G. John

Department of Earth Sciences, University of Southern California