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ON TWENTY YEARS OF GEOTRACES
PERSPECTIVE GEOTRACES: FIFTEEN YEARS OF
PROGRESS IN MARINE AEROSOL RESEARCH

Clifton S Buck, Susanne Fietz, Douglas S Hamilton, Tung-Yuan Ho, Morgane

M G Perron, Rachel U Shelley

► To cite this version:

Clifton S Buck, Susanne Fietz, Douglas S Hamilton, Tung-Yuan Ho, Morgane M G Perron, et al.: ON TWENTY YEARS OF GEOTRACES PERSPECTIVE GEOTRACES: FIFTEEN YEARS OF PROGRESS IN MARINE AEROSOL RESEARCH. Oceanography, 2024, 37 (2), pp.98-101. 10.5670/oceanog.2024.409. hal-04608149

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PERSPECTIVE

GEOTRACES: FIFTEEN YEARS OF PROGRESS IN
MARINE AEROSOL RESEARCH

By Clifton S. Buck, Susanne Fietz, Douglas S. Hamilton, Tung-Yuan Ho, Morgane M.G. Perron, and Rachel U. Shelley

**ABSTRACT.** The international GEOTRACES program has allowed unprecedented access to aerosols in the remote marine environment, moved the community toward standardized methodologies, and contributed to expanding research capabilities around the globe. A key aspect of GEOTRACES aerosol research is the quantification of deposition fluxes of trace elements and isotopes to the surface ocean as a source for biolimiting nutrients and anthropogenic contaminants. New methods for quantifying flux have been developed that leverage radioisotope tracers in the surface ocean to estimate bulk deposition rates on longer and more relevant timescales. The question as to what fraction of aerosols is soluble remains and is a source of continuing uncertainty. To that end, the community has engaged in coordinated study to address questions regarding the fractional solubility of aerosol trace elements and isotopes through the evaluation of widely used dissolution and extraction techniques. Intercalibration efforts, method standardization, and normalization of open-access data archiving will be the legacy of GEOTRACES-era aerosol research.

INTRODUCTION

From the outset, the mission of the inter-
national GEOTRACES program has
included efforts to better understand the
role of micronutrients in marine ecosys-
tems as well as the transport and fate of
contaminants (SCOR Working Group,
2007). One primary research theme has
been to quantify the fluxes that control the
distributions of key trace elements and
isotopes (TEIs) in the marine environ-
ment. In remote regions, far from other
major sources, aerosol deposition can be
the primary source of soluble, and poten-
tially bioavailable, TEIs to surface waters
where their input may impact biological
primary production. For example, TEIs

such as iron, manganese, zinc, copper,
and nickel can influence phytoplank-
ton community structure in the surface
water and material cycling in the water
column. In addition, excess concentra-
tions of anthropogenic contaminant TEIs
like lead and cadmium are used as tracers
of anthropogenic emissions, and metals
that are mainly sourced from Earth's
crust, such as aluminum, titanium, and
thorium, may be used as tracers of litho-
genic material. The study of aerosol TEIs
is therefore essential in order to better
understand specific processes and mech-
anisms in the ocean; hence, their inclu-
sion as "key parameters" to be measured
on all GEOTRACES research cruises.

EXPANSION OF GLOBAL
COVERAGE AND DATA
ARCHIVES

By design, GEOTRACES brought disci-
pline-focused research to central ocean
basins and provided unprecedented
access for coincident sampling of the
water column and atmosphere. Following
predecessors like the US CLIVAR section
cruises (e.g., Buck et al., 2010, 2013) and
the repeat Atlantic Meridional Transects
(e.g., Baker et al., 2006), GEOTRACES
has provided a means to greatly expand
the spatial scale of aerosol sampling.
Since the 2008 aerosol trace element
intercomparison effort (Morton et al.,
2013), 16 GEOTRACES research proj-
ects, including section cruises and some
process studies, have reported aerosol
datasets, and an additional 13 studies col-
lected aerosols but have yet to make the
data available. Combined, these programs
have sampled all the world's ocean basins,
including the understudied regions of the
central Arctic Ocean and South Pacific
Ocean. Most of these individual research
projects have made aerosol data avail-
able through online data repositories. A
smaller subset has provided data for the
open access GEOTRACES Intermediate
Data Products (Figure 1; Schlitzer and
Mieruch-Schnülle, 2024, in this issue)
<figure><img src="image_2.png" /></figure>

**FIGURE 1.** Blue circles indicate aerosol sampling locations whose data are available in version 2 of the GEOTRACES Intermediate Data Product (GEOTRACES Intermediate Data Product Group, 2023).

through the GEOTRACES Data Assembly Center, a process that requires high standards of data quality control and evaluation by the GEOTRACES Committee on Standards & Intercalibration (Aguilar-Islas et al., 2024, in this issue).

## STANDARDIZATION OF SAMPLING EQUIPMENT AND ANALYTICAL TECHNIQUES

GEOTRACES is a coordinated study that involves research groups in different parts of the world, and many of the target parameters are assessed by new and developing analytical techniques. Thus, community agreement on best practices and standard procedures for sampling, sample processing, and analysis is necessary to reduce introduced variability and ensure the highest quality data.

Aerosol loading and composition can vary according to characteristics of the sampling site (e.g., distance to and type of local and surrounding sources, altitude if a land-based site, meteorological conditions) as well as processes occurring during particle transport. Additional variability comes from the various collection and sample processing techniques in use. As with water-column parameters, GEOTRACES has spurred the aerosol community to critically assess sampling

and analytical protocols. Prior to this effort, aerosol collections were made with a variety of equipment, including both low-volume and high-volume active samplers, passive collectors, and total suspended or size-fractionated particle samplers. The choice of collection substrate, often a membrane filter, is yet another variable. A wide range of laboratory and sampling protocols in use resulted in datasets that are not readily intercomparable. Recognizing the importance of intercomparable data in global efforts, the community set out best practices for aerosol TEI sampling and sample handling in the “GEOTRACES Cookbook.” This resource is freely available online (https://www.geotracess.org/methods-cookbook/) and is regularly revised to reflect methodological advances in the field. Descriptions of aerosol extraction methods widely used in the community are also included.

By its nature, GEOTRACES ensured that ships from many nations and with different configurations would serve as observational platforms during program-endorsed research expeditions. Therefore, researchers sought a common sampling system that would be adaptable. The ideal system would be commercially available and not require extensive modification so that a broad swath of the

research community could acquire the necessary equipment. Total suspended particle collectors were recommended because they met the desired criteria and have been used in both land-based and ship-based atmospheric sampling programs. These high-volume samplers feature a relatively small footprint, brushless motors, and are self-contained. The sampling interface and vacuum pump are co-located within an aluminum housing that can be mounted to the forward railings of ships (Figure 2). The collector is designed for bulk collections or can accommodate a cascade impactor for particle size fractionation. In addition to agreements on sampling practices, guidance on analysis of total TEI content in aerosols was provided following the aforementioned GEOTRACES-led intercomparison study effort (Morton et al., 2013). For example, similar total aeolian TEI determination protocols are now typically applied worldwide using nitric and hydrofluoric acids and heat to digest aerosol-laden filters.

Not all aerosol metals reaching surface waters are assimilable by marine phytoplankton. Assessment of the soluble content in aerosols is therefore crucial for GEOTRACES water-column studies, as it is a proxy for the readily bioavailable
<figure><img src="image_3.png" /><figcaption>FIGURE 2. Total suspended particle samplers are shown mounted on the forward railing next to the sector-control anemometer aboard R/V *Roger Revelle* during US GEOTRACES section cruise GP15.</figcaption></figure>

fraction of aerosol TEIs. Constraining the soluble aerosol fraction remains a major challenge hindering our understanding of air-sea biogeochemical interactions. Laboratory methods used to assess the soluble aerosols typically consist of conducting leaching experiments on aerosol-loaded filters. Currently, many leaching protocols, using various solutions and extraction techniques, are employed to represent different atmospheric processes or types of deposition (Perron et al., 2020). However, data resulting from the different techniques are used as analogs in modeling studies. Hence, intercalibration is necessary to reduce the associated uncertainty. The Scientific Committee on Oceanic Research Working Group 167 (Reducing Uncertainty in Soluble aerosol Trace Element Deposition) is leading the synthesis effort and promoting best practices for intercomparable data on TEI bioavailability, including recommending broad use of community consensus reference materials that are appropriate for aerosols in the marine environment.

## ESTIMATES OF AEROSOL PROPERTIES AND DEPOSITION FLUX

A key aspect of aerosol research within the GEOTRACES framework is the quantification of TEI deposition fluxes to the surface ocean as a source of biolimiting nutrients. Understanding why, where, and when aerosol TEI concentrations are changing, due to climate change and other anthropogenic activities, is crucial for assessing the impact of atmospheric deposition on society through consequences on ecosystem health, primary productivity, and global climate feedbacks, among other effects. Such understanding requires quantifying the properties of aerosols across different ocean basins and timescales. To fill this knowledge gap, GEOTRACES data, and data from other field programs, have been used to trace and constrain anthropogenic and natural sources of iron and other TEIs, and there have been important advances since the last progress report on TEI deposition research (Baker et al., 2016).

For example, in recent years, a growing avenue of study has been the use of GEOTRACES data to identify variations in isotope fractionation of specific TEIs to differentiate aerosol sources of metals (e.g., Conway et al., 2019; Kurisu et al., 2021; Sieber et al., 2023). GEOTRACES data can then constrain atmospheric and oceanic modeling, thus improving projections of future patterns in aerosol nutrient and contaminant distributions.

Modeling studies have shown that uncertainty in the input fluxes of iron hampers efforts to build agreement on its residence time in ocean waters and thus the ability of models to accurately reproduce observations within the water column (Tagliabue et al., 2016). Long-used techniques, which apply a bulk deposition velocity estimate to convert observed atmospheric loading into a flux term, poorly constrain the magnitude of atmospheric deposition (Duce et al., 1991). Recent GEOTRACES efforts further indicated that deposition velocity estimates should also be region, particle size, and element specific. For example, aerosol iron concentrations and solubilities in size-fractionated aerosols collected in the North Pacific region originating from East Asia are significantly different from those collected in the North Atlantic region where aerosols mainly originate from North Africa, including the Saharan desert. Recent work shows that Atlantic aerosol iron on particles <1.0 µm (the fine fraction) has a fractional solubility less than about 5%, while the fractional solubility of iron on Pacific particles may be greater than 30% in the same size fraction (Baker et al., 2020; Hsieh et al., 2022). These studies use different methods to estimate fractional solubility, which complicates comparisons of the results (Perron et al., 2020). As summarized by Chance et al. (2015), non-lithogenic elements are often associated with smaller aerosol particles and are subject to lower deposition velocity estimates than are elements more associated with lithogenic material. Because aerosol deposition velocity and solubility are
both highly dependent on particle size, deficient size-fractionated data and the corresponding metal solubilities could introduce significant bias in estimates of soluble aerosol deposition fluxes.

These estimates are also dependent on temporal snapshots of aerosol loading, which may miss seasonality in atmospheric deposition. GEOTRACES studies by their nature are short relative to seasonal and episodic aerosol transport and deposition events. To address this issue, GEOTRACES affiliated researchers have developed methods that leverage chemical tracers in the water column—in particular, radioisotopes like thorium-230, thorium-232, and beryllium-7—to produce flux estimates that are less reliant on snapshot observations of loading in the atmosphere (Anderson et al., 2016; Hayes et al., 2018; Kadko et al., 2015). Time-series atmospheric sampling stations located on coasts or islands are also powerful tools that can complement GEOTRACES work and provide information on longer-term variability in atmospheric emissions/deposition.

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## ACKNOWLEDGMENTS

MMGP was supported by the Interdisciplinary graduate school for the blue planet (ISBlue, ANR-17-EURE-0015) in a project co-funded by the French government under the program "Investissements d'Avenir" embedded in France 2030. DSH gratefully acknowledges support from NASA (grant 80NSSC24K0446). The GEOTRACES 2021 Intermediate Data Product (IDP2021) represents an international collaboration and is endorsed by the Scientific Committee on Oceanic Research (SCOR). The many researchers and funding agencies responsible for the collection of data and quality control are thanked for their contributions to IDP2021. 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

Clifton S. Buck (csbuck@uga.edu) is Associate Professor, Skidaway Institute of Oceanography, Savannah, GA, USA. Susanne Fietz is Associate Professor, Stellenbosch University, Stellenbosch, South Africa. Douglas S. Hamilton is Assistant Professor, North Carolina State University, Raleigh, NC, USA. Tung-Yuan Ho is Research Fellow, Academia Sinica, Taipei, Taiwan. Morgane G.M. Perron is Postdoctoral Fellow, Université de Brest - UMR 6539 CNRS/UBO/IRD/Ifremer, Laboratoire des sciences de l'environnement marin (LEMAR) - Institut Universitaire Européen de la Mer, Plouzané, France. Rachel U. Shelley is Senior Researcher, University of East Anglia, Norwich, UK.

## ARTICLE CITATION

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.

## COPYRIGHT & USAGE

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