Jane E. Macdonald

ORCID: 0009-0008-7644-4173
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About
Contact & Profiles
Research Areas
  • Geochemistry and Elemental Analysis
  • Geological and Geochemical Analysis
  • Silicon Effects in Agriculture
  • Astro and Planetary Science
  • Paleontology and Stratigraphy of Fossils
  • Planetary Science and Exploration

University of St Andrews
2023-2024

University of Cambridge
2024

Unraveling ancient melting processes is key to understanding how the earliest, tonalite-trondhjemite-granodiorite (TTG)-dominated continental crust formed from partial of amphibolite. Application silicon isotope analysis reveals that Archaean TTGs exhibit consistently high Si values (δ30Si) compared modern granitoids, attributed seawater-derived silica introduced by either (a) variably silicified basalts or (b) assimilation authigenic silica-rich marine lithologies in melt source. However,...

10.1016/j.gca.2024.01.018 article EN cc-by Geochimica et Cosmochimica Acta 2024-01-24

On the anoxic Archean Earth, prior to onset of oxidative weathering, electron acceptors were relatively scarce, perhaps limiting microbial productivity. An important metabolite may have been sulfate produced during photolysis volcanogenic SO

10.1111/gbi.12595 article EN cc-by Geobiology 2024-03-01
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