David Zakharov

Assistant Professor

Western Michigan University

United States

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David Zakharov is an Assistant Professor at Western Michigan University in the United States. His research interests focus on isotope geochemistry, particularly in the context of paleoproterozoic and Archean geological processes. Recent publications include studies on oxygen and silicon isotopic compositions in relation to seafloor hydrothermalism and the analysis of magmatic-hydrothermal systems. His work contributes valuable insights into the geochemical evolution of early Earth environments.

Articles (10)

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2025

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2025

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2024

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2024

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2023

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2023

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2023

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2022

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2021

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2021

Collaborators (4)

Torsten Vennemann

SWITZERLAND

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Kristoffer Szilas

Københavns Universitet

DENMARK

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Lingyu Zhang

University of Copenhagen

DENMARK

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Andreas Pack

Georg-August-Universität

GERMANY

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David Zakharov

Research Interests

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About

Articles (10)

Low-δ18O (−8 ‰, VSMOW) Paleoproterozoic and discordant zircon: Lessons learned from using a combination of traditional bulk and in situ approaches

Reaction-controlled triple O-isotope exchange trajectories during experimental alteration of olivine

Selective metasomatism of ultramafic cumulates within Archean supracrustal sequences

Oxygen and silicon isotopic compositions of Archean silicified lava and cherts of the Onverwacht Group: Implication for seafloor hydrothermalism and the nature of recycled components in the source of granitoids

In‐Situ and Triple Oxygen Isotope Characterization of Seafloor Drilled Cherts: Marine Diagenesis and Its Bearing on Seawater Reconstructions

In‐Situ and Triple Oxygen Isotope Characterization of Seafloor Drilled Cherts: Marine Diagenesis and Its Bearing on Seawater Reconstructions

Quantitative record of the Neoarchean water cycle from a 2.67 Ga magmatic-hydrothermal system, Fennoscandian Shield

Low-δ<sup>18</sup>O Neoarchean precipitation recorded in a 2.67 Ga magmatic-hydrothermal system of the Keivy granitic complex, Russia

A New Insight Into Seawater-Basalt Exchange Reactions Based on Combined δ<sup>18</sup>O—Δ′<sup>17</sup>O—<sup>87</sup>Sr/<sup>86</sup>Sr Values of Hydrothermal Fluids From the Axial Seamount Volcano, Pacific Ocean

Influence of high marine Ca/SO<sub>4</sub> ratio on alteration of submarine basalts at 2.41 Ga documented by triple O and Sr isotopes of epidote

Collaborators (4)

Torsten Vennemann

Kristoffer Szilas

Lingyu Zhang

Andreas Pack

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