Introduction to the special issue on twenty years of GEOTRACES: An international study of the marine biogeochemical cycles of trace elements and isotopes DOI Creative Commons
Tim M. Conway, Jessica N. Fitzsimmons, Rob Middag

и другие.

Oceanography, Год журнала: 2024, Номер 37(2)

Опубликована: Янв. 1, 2024

This special issue of Oceanography celebrates the transformational findings international GEOTRACES program in chemical oceanography, 20 years after drafting Science Plan 2004 (GEOTRACES Planning Group, 2006). With section cruise phase ending soon, and a planned pivot toward smaller-​scale process studies, this is an opportune time to look back at achievements during last two decades highlight some advances our understanding processes that determine oceanic distributions trace elements isotopes (TEIs).

Язык: Английский

GEOTRACES Reflections DOI Creative Commons
Robert L. Anderson

Oceanography, Год журнала: 2024, Номер 37(2)

Опубликована: Янв. 1, 2024

GEOTRACES is an international program that has benefited from contributions by investigators in 35 nations. The mission to identify processes and quantify fluxes control the distributions of key trace elements isotopes ocean establish sensitivity these changing environmental conditions. This perspective first summarizes historical motivation for program, then describes selected research highlights, focusing on recent findings related iron. patchy distribution iron indicates a short residence time, at low end range times estimated models. Iron removal must, therefore, be rapid. Recent results North Atlantic Ocean suggest formation particulate authigenic phases may factor contributing faster than previously thought. article also identifies several areas where advancements are expected through modeling synthesis efforts.

Язык: Английский

Процитировано

5

The “Net” Impact of Hydrothermal Venting on Oceanic Elemental Inventories: Contributions to Plume Geochemistry from the International GEOTRACES Program DOI Creative Commons
Jessica N. Fitzsimmons, Janelle Steffen

Oceanography, Год журнала: 2024, Номер 37(2), С. 102 - 115

Опубликована: Янв. 1, 2024

Hydrothermal vents serve as a primary interface between the cold deep ocean and warm oceanic crust. While early research showed that seawater-​rock interactions add to or remove elements from seawater during generation of hydrothermal fluids, consideration these fluid fluxes alone does not relay total impact systems have on geochemistry. In addition, plumes, areas where fluids mix with waters, are host range particle precipitation scavenging reactions further modify gross define “net” inventories. Here, we review major discoveries made by international GEOTRACES program regarding geochemical transformations occurring within plumes. We classify each element into one five categories based its behavior in spectrum spanning mass balance net source plume sinks. Overall, celebrate role has played defining extent dynamics geochemistry, which is crucial lever for determining global impacts.

Язык: Английский

Процитировано

5

The Influence of Natural, Anthropogenic, and Wildfire Sources on Iron and Zinc Aerosols Delivered to the North Pacific Ocean DOI Creative Commons
Zachary B. Bunnell, Matthias Sieber, Douglas S. Hamilton

и другие.

Geophysical Research Letters, Год журнала: 2025, Номер 52(3)

Опубликована: Янв. 30, 2025

Abstract Atmospheric deposition is an important source of iron (Fe) and perhaps zinc (Zn) to the oceans. We present total water‐soluble aerosol Fe Zn isotopic compositions, size‐fractionated enrichment factors from North Pacific GEOTRACES GP15 section (Alaska‐Tahiti) during low dust season. found distinct bulk provinces along this latitudinal transect: Asian aerosols (especially crustal dust) dominate at higher latitudes (52–32°N) while American heavier‐than‐crustal wildfire in Equatorial deployments (20°N 20°S). Soluble was isotopically lighter‐than‐crustal full transect, strongly indicative a pervasive anthropogenic contribution Pacific. Comparison global model corroborates that heavy endmember required for Fe, attributed pyroconvective entrainment soil particles. For Zn, entire dominated by non‐crustal sources, reflected light compositions (bulk: −0.12 ± 0.08‰ soluble: −0.17 0.14‰).

Язык: Английский

Процитировано

0

Long Distance Transport of Subsurface Sediment‐Derived Iron From Asian to Alaskan Margins in the North Pacific Ocean DOI Creative Commons
Matthias Sieber, Nathan T. Lanning, Janelle Steffen

и другие.

Geophysical Research Letters, Год журнала: 2024, Номер 51(20)

Опубликована: Окт. 14, 2024

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 iron (dFe) from North Pacific GP15 section, which, alongside other sediment‐source tracers (including δ 56 Fe, Mn, 228 Ra, and particulate Fe), allows for identification dFe provenance three distinct depth maxima at Alaskan margin. Two these (shelf abyssal depths) local sedimentary origin. third, mid‐depth maximum with an absence is advected signal that, based on tracer data Western transects circulation models, must be sources Asian margin, ∼5,000 km away. This study illustrates importance measuring diagnostic like radium when assigning margins as trace metal budgets.

Язык: Английский

Процитировано

1

Introduction to the special issue on twenty years of GEOTRACES: An international study of the marine biogeochemical cycles of trace elements and isotopes DOI Creative Commons
Tim M. Conway, Jessica N. Fitzsimmons, Rob Middag

и другие.

Oceanography, Год журнала: 2024, Номер 37(2)

Опубликована: Янв. 1, 2024

This special issue of Oceanography celebrates the transformational findings international GEOTRACES program in chemical oceanography, 20 years after drafting Science Plan 2004 (GEOTRACES Planning Group, 2006). With section cruise phase ending soon, and a planned pivot toward smaller-​scale process studies, this is an opportune time to look back at achievements during last two decades highlight some advances our understanding processes that determine oceanic distributions trace elements isotopes (TEIs).

Язык: Английский

Процитировано

0