June 2024

Special Issue on Twenty Years of GEOTRACES: An International Study of the Marine Biogeochemical Cycles of Trace Elements and Isotopes

IN

PROGRESS

TWENTY YEARS OF GEOTRACES

AN INTERNATIONAL STUDY OF THE MARINE BIOGEOCHEMICAL

CYCLES OF TRACE ELEMENTS AND ISOTOPES

Oceanography

THE OFFICIAL MAGAZINE OF THE OCEANOGRAPHY SOCIETY

VOL. 37, NO. 2, JUNE 2024

June 2024 | Oceanography

SPECIAL ISSUE ON

TWENTY YEARS OF GEOTRACES

6 FROM THE GUEST EDITORS. Introduction to the Special Issue

By T.M. Conway, J.N. Fitzsimmons, R. Middag, T.L. Noble, and H. Planquette

8 PERSPECTIVE. GEOTRACES Reflections

By R.F. Anderson

13 PERSPECTIVE. A Young Scientist’s Perspective on GEOTRACES

By D.J. Halbeisen

17 PERSPECTIVE. The Value of Going To Sea on Big Ships and the Advantage

of Multiple Tracers for GEOTRACES Style Programs

By C. Jeandel

21 PERSPECTIVE. Intercalibration: A Cornerstone of the Success of the

GEOTRACES Program

By A. Aguilar-Islas, H. Planquette, M.C. Lohan, W. Geibert, and G. Cutter

25 The GEOTRACES Intermediate Data Products: Rich Resources for Research,

Education, and Outreach

By R. Schlitzer and S. Mieruch-Schnülle

34 SPOTLIGHT. Three-Minute Videos to Learn About Marine Geochemistry

By E. Masferrer Dodas, C. Jeandel, and A. Artis

35 PERSPECTIVE. GEOTRACES: Ironing Out the Details of the Oceanic

Iron Sources?

By T.M. Conway, R. Middag, and R. Schlitzer

46 The Southern Ocean Hub for Nutrients, Micronutrients, and Their Isotopes

in the Global Ocean

By G.F. de Souza and A.K. Morrison

60 Shelf-Basin Connectivity Drives Dissolved Fe and Mn Distributions in the

Western Arctic Ocean: A Synoptic View into Polar Trace Metal Cycling

By L. Jensen and M. Colombo

72 On the Variability of Equatorial Pacific Nitrate and Iron Utilization

By P.A. Rafter

85 Advances in Understanding the Marine Nitrogen Cycle in the

GEOTRACES Era

By K.L. Casciotti, T.A. Marshall, S.E. Fawcett, and A.N. Knapp

102 The “Net” Impact of Hydrothermal Venting on Oceanic Elemental

Inventories: Contributions to Plume Geochemistry from the International

GEOTRACES Program

By J.N. Fitzsimmons and J.M. Steffen

116 PERSPECTIVE. GEOTRACES: Fifteen Years of Progress in Marine Aerosol

Research

By C.S. Buck, S. Fietz, D.S. Hamilton, T.-Y. Ho, M.M.G. Perron, and R.U. Shelley

120 An Ocean of Particles: Characterization of Particulate Trace Elements by

the GEOTRACES Program

By B.S. Twining

contents VOL. 37, NO. 2, JUNE 2024

102

46

60

June 2024 | Oceanography

Oceanography | Vol. 37, No. 2

238U

234Th

234U

230Th

Dust/

Minerals

232Th

228Th

224Ra

Porewater

Release

232Th

228Ra

234Pa

228Ra

228Th

228Ac

Sinking Particle

Removal

Sinking Particle

Removal

Sinking Particle

Removal

24 days

76 kyr

1.8 yr

4.5 Gyr

250 kyr

1.2 min

14 Gyr

6.2 hrs

5.8 yr

3.7 days

1.8 yr

14 Gyr

5.8 yr

156

AAIW

NADW

AABW

131 Novel Insights into Ocean Trace Element Cycling from

Biogeochemical Models

By A. Tagliabue and T. Weber

142 New Insights into the Organic Complexation of Bioactive Trace Metals

in the Global Ocean from the GEOTRACES Era

By H. Whitby, J. Park, Y. Shaked, R.M. Boiteau, K.N. Buck, and R.M. Bundy

156 PERSPECTIVE. Timekeepers for Trace Elements in the Global Ocean:

The Thorium Stopwatches

By C.T. Hayes

162 PERSPECTIVE. The Dawn of the BioGeoSCAPES Program: Ocean

Metabolism and Nutrient Cycles on a Changing Planet

By M.A. Saito, H. Alexander, H.M. Benway, P.W. Boyd, M. Gledhill, E.B. Kujawinski,

N.M. Levine, M. Maheigan, A. Marchetti, I. Obernosterer, A.E. Santoro, D. Shi, K.Suzuki,

A. Tagliabue, B.S. Twining, and M.T. Maldonado

DEPARTMENTS

5 QUARTERDECK. A Needle in the Haystack

By C. Benitez-Nelson

167 DIY OCEANOGRAPHY. The OpenCTD: A Low-Cost, Open-Source CTD for

Collecting Baseline Oceanographic Data in Coastal Waters

By A. Thaler, S.K. Sturdivant, R.Y. Neches, and J.J. Levenson

174 DIY OCEANOGRAPHY. Design Update to “The Pressure of In-Situ Gases

Instrument (PIGI) for Autonomous Shipboard Measurement of Dissolved O2

and N2 in Surface Ocean Waters”

By B. Lowin, R. Izett, E. Taylor, C. Robertson, and S. Rivero-Calle

180 TRIBUTE. A Tribute to Richard W. Eppley

Compiled and edited by P.G. Falkowski

186 THE OCEANOGRAPHY CLASSROOM. Interviews!

By S. Boxall

188 FROM THE TOS JEDI COMMITTEE. In Pursuit of Conference Equity

By I.M. Martínez-Farrington, L. Martell Bonet, A. Alemán-Díaz, H.J. Ballenger, D. Ebanks,

M. Behl, S. Kolesar, S. Cooper, C. Garza, J.C. Lewis, M.B. Jones, and L. White

190 CAREER PROFILES. Trisha Bergmann, International Affairs Specialist, NOAA

National Ocean Service | Meredith Jennings, Senior Research Associate,

Houston Advanced Research Center

ON THE COVER

Deployment of the "trace metal clean" rosette

at 78°N from USCGC Healy as part of the 2015

US GEOTRACES GN01 cruise to the Arctic

Ocean. Water from this cast yielded data for

key biogeochemical parameters such as iron,

aluminum, radium, metal isotopes, and major

nutrients. Photo credit: Katlin Bowman Adamczyk,

US Geological Survey

SPECIAL ISSUE SPONSOR

Support for production of this special issue was

provided by the US National Science Foundation,

award OCE-2219888 to Robert Anderson.

SPECIAL ISSUE GUEST EDITORS

Tim Conway, University of South Florida

Jessica Fitzsimmons, Texas A&M University

Rob Middag, Royal NIOZ

Taryn Noble, University of Tasmania

Hélène Planquette, University of Brest

180

131

IN

PROGRESS

TWENTY YEARS OF GEOTRACES

AN INTERNATIONAL STUDY OF THE MARINE BIOGEOCHEMICAL

CYCLES OF TRACE ELEMENTS AND ISOTOPES

Oceanography

THE OFFICIAL MAGAZINE OF THE OCEANOGRAPHY SOCIETY

VOL. 37, NO. 2, JUNE 2024

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June 2024 | Oceanography

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informs the public about ocean research, innovative tech-

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Background photo credit: Merr Watson/Ocean Image Bank

June 2024 | Oceanography

For the past 20 years, the GEOTRACES program has produced trans-

formative insights into the cycling of trace elements and isotopes (TEIs)

in the ocean. Modeled after the 1970s GEOSECS (Geochemical Ocean

Sections Study) program, the goals of this ambitious study were to con-

duct large-scale measurements of TEI concentrations and to deter-

mine the biogeochemical processes that controlled their distributions

throughout the global ocean. Perhaps the biggest hurdle to overcome

was how to accurately measure less than nanomolar concentrations of

TEIs from the deck of a 3,000 gross tonnage steel ship. Contaminants

were literally everywhere, requiring scientists and crew to become inno-

vative in their attempts to maintain clean conditions for sample collec-

tion, storage, and measurement. GEOTRACES encouraged interna-

tional partnerships while instilling a collaborative approach in the next

generation of scientists. The practices GEOTRACES developed led to

consistent high-quality measurements across diverse lab groups and

provided an extensive and open database. GEOTRACES has truly been

a labor of love among all the scientists and crews involved, and the pro-

gram continues as a lofty example of the discoveries possible when con-

ducting such wide-ranging collaborative research.

Claudia Benitez-Nelson

Associate Editor, Oceanography

D   https://doi.org/10.5670/oceanog.2024.422

QUARTERDECK

A NEEDLE IN THE HAYSTACK

Physical Oceanography of

Continental Shelves

K.H. Brink

An authoritative graduate textbook and

professional reference on the physical

dynamics of the coastal ocean

“This concise, up-to-date textbook has

virtually everything a student needs for

a course on coastal ocean physics.”

—John Wilkin, Rutgers University

• Covers the physical dynamics and properties

of the coastal ocean, synthesizing theory

and global observations

• Topics include turbulent boundary layers,

wind driving, coastal-trapped waves, the

inner shelf, tides, buoyancy currents,

instabilities, and connections with the

deep open ocean

Oceanography Flipbooks

https://oceanography.publuu.com

Be sure to visit the open access Oceanography flipbook library to

page through the full GEOTRACES special issue. While there, explore

other Oceanography issues back to March 2015.

AUTHORS! Flipbooks are an exciting enhancement to Oceanography.

In these flipbooks, we can embed videos, animations, photo galleries,

and audio files in your article. For details on file sizes and formats, visit

https://tos.org/oceanography/guidelines.

Oceanography | Vol. 37, No. 2

INTRODUCTION TO THE

SPECIAL ISSUE ON

TWENTY YEARS OF GEOTRACES

AN INTERNATIONAL STUDY OF THE MARINE BIOGEOCHEMICAL

CYCLES OF TRACE ELEMENTS AND ISOTOPES

INTRODUCTION

This special issue of Oceanography cele-

brates the transformational findings of

the international GEOTRACES program

in chemical oceanography, 20 years after

drafting of the GEOTRACES Science

Plan in 2004 (GEOTRACES Planning

Group, 2006). With the section cruise

phase of the program ending soon, and a

planned pivot toward smaller- scale pro-

cess studies, this is an opportune time

to look back at the achievements of

GEOTRACES during the last two decades

and to highlight some of the advances in

our understanding of the processes that

determine the oceanic distributions of

trace elements and isotopes (TEIs).

GEOTRACES

GEOTRACES is a cooperative interna-

tional effort comprising scientists from

35 countries, supported by national fund-

ing agencies, and guided by international

steering committees. Since 2008, the pro-

gram has carried out oceanographic,

World Ocean Circulation Experiment

(WOCE)-style “section” cruises through-

out all the ocean basins. Rigorous inter-

calibration efforts stand at the foun-

dation of GEOTRACES to ensure that

basin-scale analyses made by individ-

ual nations can be compared with-

out question. This has been achieved

primarily by occupation of “crossover”

stations between cruises hosted by dif-

ferent countries—perhaps the most

evocative was a meeting of German and

US GEOTRACES Arctic cruises at the

North Pole in 2015. Moreover, the drive

for publicly available synthesized data-

sets has resulted in the production of

an online electronic atlas (https://www.

egeotraces.org/) and the release of three

intermediate data products to date, with

a fourth expected in 2025. These efforts

have led to a sea change in the quantity

of high-quality TEI data available for the

ocean, coupled with many advances in

our understanding of the biogeochemical

processes that determine these distribu-

tions (Anderson et al., 2014).

ARTICLES IN THE

SPECIAL ISSUE

This special issue begins with reflec-

tions from junior and senior scien-

tists on the GEOTRACES program,

the benefit of a multi-tracer approach

for answering biogeochemical ques-

tions, and what life is like aboard a

GEOTRACES section cruise (Anderson,

Halbeisen, and Jeandel). A key suc-

cess of GEOTRACES lies in the rigorous

intercalibration of all data incorporated

into its products, a process overseen

by the Standards and Intercalibration

Committee. This achievement is based

on crucial cooperation among scien-

tists who openly shared protocols, as

discussed in Aguilar-Islas et al., and

allows for both a holistic view of TEI

cycling within a basin (e.g., Arctic

Ocean; Jensen and Colombo) and

synthesized intermediate data prod-

ucts that are valuable for research, edu-

cation, and outreach efforts (as outlined

by Schlitzer and Mieruch-Schnülle).

In addition, from an education and out-

reach perspective, the GEOTRACES

program office has produced a series

of short educational videos, which are

highlighted by Masferrer Dodas et al.

Several articles in this issue focus

on “key parameters,” tracers that are

deemed essential to the GEOTRACES

program. For example, Anderson and

Conway et al. both focus on dissolved

iron and how GEOTRACES has elegantly

demonstrated the utility of a multi-tracer

approach and the unexpected and per-

sistent nature of iron from deep bound-

ary sources such as marine sediments

and hydrothermal venting. Fitzsimmons

and Steffen take a deeper dive into

how GEOTRACES research on hydro-

thermal plumes have transformed our

understanding of which TEIs are sup-

plied or consumed by hydrothermal

systems before influencing the wider

im M. Conway, Jessica N. Fitzsimmons, Rob Middag, Taryn L. Noble, and Hélène Planquette

FROM THE GUEST EDITORS

June 2024 | Oceanography

ocean. Hayes provides an overview of

the unique value of the thorium radio-

nuclides as timekeepers for rates in the

ocean and how they aid understand-

ing of manifold biogeochemical pro-

cesses, while Casciotti et al. describe

recent advances in our understanding

of the marine nitrogen cycle that have

come from GEOTRACES and other

efforts. Rafter then looks at how linking

together elements such as iron and nitro-

gen can enhance insights into oceanic

nutrient cycling.

The proliferation of GEOTRACES

datasets has sparked renewed appre-

ciation for the role of physical circula-

tion in influencing global TEI distri-

butions. The paper by de Souza and

Morrison takes a close look at our

increasing understanding of the role of

the Southern Ocean “hub” in driving

global nutrient and TEI distributions.

However, it is not just knowledge of oce-

anic “dissolved” TEIs and circulation that

are needed to understand marine bio-

geochemical cycles; GEOTRACES has

also provided numerous advances in

our knowledge of elemental speciation

and organic complexation, marine par-

ticles, and aerosols as featured by sev-

eral articles in this issue (Whitby et al.,

Twining, and Buck et al., respectively).

Tagliabue and Weber provide an over-

view of how a range of different ocean

biogeochemical modeling approaches

have been stimulated by—and become

invaluable in the interpretation of—

GEOTRACES datasets. Lastly, we look to

the future with Saito et al. describing the

nascent BioGeoSCAPES program, which

aims to build on advances from pro-

grams such as GEOTRACES and stim-

ulate a research program designed to

enhance understanding of the linkages

between microbes, climate change, and

biogeochemical cycles. We eagerly antic-

ipate the development of this new pro-

gram and the continuing discoveries to

come from GEOTRACES.

REFERENCES

Aguilar-Islas, A., H. Planquette, M.C. Lohan, W. Geibert,

and G. Cutter. 2024. Intercalibration: A corner-

stone of the success of the GEOTRACES program.

Oceanography 37(2):21–24, https://doi.org/10.5670/

oceanog.2024.404.

Anderson, R.F. 2024. GEOTRACES reflections.

Oceanography 37(2):8–12, https://doi.org/10.5670/

oceanog.2024.405.

Anderson, R., E. Mawji, G.A. Cutter, C.I. Measures,

and C. Jeandel. 2014. GEOTRACES: Changing

the way we explore ocean chemistry.

Oceanography 27(1):50–61, https://doi.org/

10.5670/oceanog.2014.07.

Buck, C.S., S. Fietz, D.S. Hamilton, T.-Y. Ho,

M.M.G. Perron, and R.U. Shelley. 2024.

GEOTRACES: Fifteen years of progress in marine

aerosol research. Oceanography 37(2):116–119,

https://doi.org/10.5670/oceanog.2024.409.

Casciotti, K.L., T.A. Marshall, S.E. Fawcett,

and A.N. Knapp. 2024. Advances in under-

standing the marine nitrogen cycle in the

GEOTRACES era. Oceanography 37(2):85–101,

https://doi.org/10.5670/oceanog.2024.406.

Conway, T.M., R. Middag, and R. Schlitzer. 2024.

GEOTRACES: Ironing out the details of the oce-

anic iron sources? Oceanography 37(2):35–45,

https://doi.org/10.5670/oceanog.2024.416.

de Souza, G.F., and A.K. Morrison. 2024. The

Southern Ocean hub for nutrients, micronutrients,

and their isotopes in the global ocean.

Oceanography 37(2):46–59, https://doi.org/

10.5670/oceanog.2024.414.

Fitzsimmons, J.N., and J.M. Steffen. 2024. The “net”

impact of hydrothermal venting on oceanic ele-

mental inventories: Contributions to plume geo-

chemistry from the international GEOTRACES pro-

gram. Oceanography 37(2):102–115, https://doi.org/

10.5670/oceanog.2024.421.

GEOTRACES Planning Group. 2006. GEOTRACES

Science Plan. Scientific Committee on Oceanic

Research, Baltimore, MD, https://geotracesold.

sedoo.fr/libraries/documents/Science_plan.pdf.

Halbeisen, D.J. 2024. A young scientist’s perspec-

tive on GEOTRACES. Oceanography 37(2):13–16,

https://doi.org/10.5670/oceanog.2024.403.

Hayes, C.T. 2024. Timekeepers for trace elements

in the global ocean: The thorium stopwatches.

Oceanography 37(2):156–161, https://doi.org/

10.5670/oceanog.2024.412.

Jeandel, C. 2024. The value of going to sea

on big ships and the advantage of multi-

ple tracers for GEOTRACES style programs.

Oceanography 37(2):17–20, https://doi.org/

10.5670/oceanog.2024.408.

Jensen, L., and M. Colombo. 2024. Shelf-basin

connectivity drives dissolved Fe and Mn dis-

tributions in the western Arctic Ocean: A syn-

optic view into polar trace metal cycling.

Oceanography 37(2):60–71, https://doi.org/

10.5670/oceanog.2024.410.

Masferrer Dodas, E., C. Jeandel, and A. Artis. 2024.

Three-minute videos to learn about marine geo-

chemistry. Oceanography 37(2):34, https://doi.org/

10.5670/oceanog.2024.401.

Rafter, P.A. 2024. On the variability of equa-

torial Pacific nitrate and iron utilization.

Oceanography 37(2):72–84, https://doi.org/

10.5670/oceanog.2024.411.

Saito, M.A., H. Alexander, H.M. Benway, P.W. Boyd,

M. Gledhill, E.B. Kujawinski, N.M. Levine,

M. Maheigan, A. Marchetti, I. Obernosterer, and

others. 2024. The dawn of the BioGeoSCAPES pro-

gram: Ocean metabolism and nutrient cycles on

a changing planet. Oceanography 37(2):162–166,

https://doi.org/10.5670/oceanog.2024.417.

Schlitzer, R., and S. Mieruch-Schnülle. 2024. The

GEOTRACES intermediate data products: Rich

resources for research, education, and out-

reach. Oceanography 37(2):25–33, https://doi.org/

10.5670/oceanog.2024.402.

Tagliabue, A., and T. Weber. 2024. Novel insights

into ocean trace element cycling from biogeo-

chemical models. Oceanography 37(2):131–141,

https://doi.org/ 10.5670/oceanog.2024.418.

Twining, B.S. 2024. An ocean of particles:

Characterization of particulate trace ele-

ments by the GEOTRACES program.

Oceanography 37(2):120–130, https://doi.org/

10.5670/oceanog.2024.407.

Whitby, H., J. Park, Y. Shaked, R.M. Boiteau, K.N. Buck,

and R.M. Bundy. 2024. New insights into the

organic complexation of bioactive trace met-

als in the global ocean from the GEOTRACES era.

Oceanography 37(2):142–155, https://doi.org/

10.5670/ oceanog.2024.419.

ACKNOWLEDGMENTS

We thank Robert Anderson, the US GEOTRACES

Program Office, and the US National Science

Foundation for supporting this Special Issue through

NSF award OCE-2219888. We also thank each of

the authors of the original GEOTRACES Science Plan

(GEOTRACES Planning Group, 2006), whose vision

brought us to the outstanding discoveries described

in this special issue. The international GEOTRACES

program is possible in part thanks to the support from

the US National Science Foundation (Grant OCE-

2140395) to the Scientific Committee on Oceanic

Research (SCOR).

AUTHORS

Tim M. Conway (tmconway@usf.edu) is Associate

Professor, College of Marine Sciences, University

of South Florida, St. Petersburg, FL, USA.

Jessica N. Fitzsimmons is Associate Professor,

Department of Oceanography, Texas A&M University,

College Station, TX, USA. Rob Middag is Research

Leader, Royal Netherlands Institute for Sea Research

(NIOZ), Den Burg, the Netherlands, and Honorary

Professor, Centre for Isotope Research - Oceans,

University of Groningen, Groningen, the Netherlands.

Taryn L. Noble is Senior Lecturer, Institute for Marine

and Antarctic Studies, University of Tasmania,

Hobart, Tasmania, Australia. Hélène Planquette is

Senior Researcher, CNRS, Université de Bretagne

Occidentale, IRD, Ifremer, LEMAR, Plouzané, France.

ARTICLE CITATION

Conway, T.M., J.N. Fitzsimmons, R. Middag,

T.L. Noble, and H. Planquette. 2024. Introduction to

the special issue on twenty years of GEOTRACES:

An international study of the marine biogeo-

chemical cycles of trace elements and isotopes.

Oceanography 37(2):6–7, https://doi.org/10.5670/

oceanog.2024.415.

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Oceanography | Vol. 37, No. 2

PERSPECTIVE

GEOTRACES REFLECTIONS

By Robert F. Anderson

SPECIAL ISSUE ON TWENTY YEARS OF GEOTRACES

Though geochemists have long sought to

understand biogeochemical cycles, initial

attempts to measure the extremely low

concentrations of trace elements in sea-

water were frustrated by contamination

problems. It was not until the 1970s that

contamination-free methods were devel-

oped, launching a new era of research to

characterize the biogeochemical cycles of

trace elements in the ocean.

Nevertheless, by the beginning of the

new millennium, after two decades of

improved and, generally, contamination-

free sample collection, work was pro-

ceeding so slowly that description of

the marine biogeochemical cycles of

most trace elements was beyond reach.

For example, by 2003, dissolved iron

(dFe) profiles from the surface ocean

to >2,000 m had been reported for no

more than two dozen locations world-

wide (Anderson et al., 2014). Despite reli-

able data, for the most part, they were

grossly inadequate to define biogeochem-

ical cycling of Fe.

Efforts would have to be coordinated

to characterize the global biogeochem-

ical cycle of any trace element: no sin-

gle nation, let alone an individual inves-

tigator, could hope to compile sufficient

information. This recognition led to the

creation of the GEOTRACES program

(https://www.geotraces.org/), an inter-

national study of the marine biogeo-

chemistry of trace elements and their

isotope (TEIs).

The objectives of the program were

straightforward: to determine ocean dis-

tributions of TEIs globally and to under-

stand the processes that control them

well enough to code the defining param-

eters into models. Achieving the neces-

sary global coverage required contribu-

tions from many investigators in many

nations, which, in turn, led to two further

prerequisites: intercalibration, to ensure

internal consistency of data generated by

different labs (Aguilar-Islas et al., 2024, in

this issue) and a data management sys-

tem that combined the international suite

of intercalibrated data into a single data-

base that was available in multiple for-

mats, including graphical illustration of

the results in an electronic atlas (Schlitzer

and Mieruch-Schnülle, 2024, in this

issue). These prerequisites were put into

place in advance of the global study.

International workshops held in 2007,

focusing on the Pacific, Atlantic, and

Indian Oceans, enabled investigators to

identify target locations, either where

strong sources or sinks of TEIs were

thought to exist, or where internal cycling

processes (biological uptake, regener-

ation, abiotic scavenging, transport by

ocean circulation) have a strong influ-

ence over TEI distributions. Investigation

of the Arctic and Southern Oceans began

in 2007 under the International Polar

Year (IPY). Although GEOTRACES

was not ready at that time to under-

take a full study of all TEIs of interest,

the development of new technologies

for the collection of contamination-free

samples (de Baar et al., 2008) in prepa-

ration for GEOTRACES allowed some

GEOTRACES investigators to partic-

ipate in the IPY. More complete plan-

ning for Arctic Ocean work (Jensen and

Colombo, 2024, in this issue) was orga-

nized during an international workshop

in 2009. Workshop reports, containing

recommendations for a global survey, are

available at https://www.geotraces.org/

planning-documents/.

A global survey of TEI distributions

(Figure 1) was designed using the targeted

locations noted above, enabling investi-

gators to develop, and in some cases test,

ABSTRACT. GEOTRACES is an international program that has benefited from con-

tributions by investigators in 35 nations. The program mission is to identify processes

and quantify fluxes that control the distributions of key trace elements and isotopes

in the ocean and to establish the sensitivity of these distributions to changing envi-

ronmental conditions. This perspective first summarizes the historical motivation

for the program, and then describes selected research highlights, focusing on recent

findings related to iron. The patchy distribution of iron in the ocean indicates a short

residence time, at the low end of the range of residence times estimated in models.

Iron removal from the ocean must, therefore, be rapid. Recent results from the North

Atlantic Ocean suggest that the formation of particulate authigenic iron phases may be

a factor contributing to iron removal that is faster than previously thought. This arti-

cle also identifies several areas where advancements are expected through modeling

and synthesis efforts.

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