Long Distance Transport of Subsurface Sediment‐Derived Iron From Asian to Alaskan Margins in the North Pacific Ocean

Abstract The international GEOTRACES program has been instrumental in demonstrating how marine sediments are a critical source of dissolved Fe to the world's oceans. Here, we present dissolved iron (dFe) from the GEOTRACES North Pacific GP15 section, which, alongside other sediment‐source tracers (including dissolved δ 56 Fe, Mn, 228 Ra, and particulate Fe), allows for identification of the dFe provenance of three distinct dFe depth maxima at the Alaskan margin. Two of these (shelf and abyssal depths) are of local Alaskan sedimentary origin. The third, a mid‐depth dFe maximum with an absence of 228 Ra, is an advected signal that, based on tracer data from Western Pacific GEOTRACES transects and circulation models, must be advected from sedimentary sources on the Asian margin, ∼5,000 km away. This study illustrates the importance of measuring diagnostic sedimentary tracers like radium when assigning local margins as sedimentary sources of marine trace metal budgets.

Authors

Institutions

Publication Details

Journal
Geophysical Research Letters
Published
2024-10-14
DOI
https://doi.org/10.1029/2024gl110836
Citations
7
Primary Topic
Geochemistry and Elemental Analysis
Type
article
Field-Weighted Citation Impact
2.42

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Long Distance Transport of Subsurface Sediment‐Derived Iron From Asian to Alaskan Margins in the North Pacific Ocean

Nathan T. Lanning, Tim M. Conway, Janelle Steffen, G. Weiss et al.
7 citations
Geophysical Research Letters
Geochemistry and Elemental Analysis
2.42
article

Long Distance Transport of Subsurface Sediment‐Derived Iron From Asian to Alaskan Margins in the North Pacific Ocean

Nathan T. Lanning, Tim M. Conway, Janelle Steffen, G. Weiss, Hannah R. Hunt, Jong‐Mi Lee, Jessica N. Fitzsimmons, Matthew A. Charette, Mariko Hatta, Willard S. Moore, Seolyn Yang, Susan Hautala, Phoebe J. Lam, Xiaopeng Bian, Seth G. John, Matthias Sieber
article en
7 citations

Abstract

Abstract The international GEOTRACES program has been instrumental in demonstrating how marine sediments are a critical source of dissolved Fe to the world's oceans. Here, we present dissolved iron (dFe) from the GEOTRACES North Pacific GP15 section, which, alongside other sediment‐source tracers (including dissolved δ 56 Fe, Mn, 228 Ra, and particulate Fe), allows for identification of the dFe provenance of three distinct dFe depth maxima at the Alaskan margin. Two of these (shelf and abyssal depths) are of local Alaskan sedimentary origin. The third, a mid‐depth dFe maximum with an absence of 228 Ra, is an advected signal that, based on tracer data from Western Pacific GEOTRACES transects and circulation models, must be advected from sedimentary sources on the Asian margin, ∼5,000 km away. This study illustrates the importance of measuring diagnostic sedimentary tracers like radium when assigning local margins as sedimentary sources of marine trace metal budgets.

Geophysical Research LettersVol. 51(20)
University of Southern California (US), Statewide California Earthquake Center (US), Japan Agency for Marine-Earth Science and Technology (JP), University of Hawaii System (US), University of South Carolina (US), University of California, Santa Cruz (US), University of Washington (US), University of South Florida (US), Massachusetts Institute of Technology (US), Woods Hole Oceanographic Institution (US), College of Marin (US), Texas A&M University (US)
National Science Foundation, Goddard Space Flight Center
Life below water
Openalex Percentile: Top 12%
Geochemistry and Elemental Analysis
2.42
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.