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Article Dans Une Revue Nature Communications Année : 2023

Transient fertilization of a post-Sturtian Snowball ocean margin with dissolved phosphate by clay minerals

Jalila Al Bahri
  • Fonction : Auteur
Christophe Brosson
  • Fonction : Auteur
Jérémie Aubineau
Alexandra Nederbragt
  • Fonction : Auteur
Anthony Oldroyd
  • Fonction : Auteur
Alasdair Skelton
Linda Lowhagen
  • Fonction : Auteur
David Webster
  • Fonction : Auteur
Wilson Fantong
  • Fonction : Auteur
Benjamin Mills
Kurt Konhauser

Résumé

Abstract Marine sedimentary rocks deposited across the Neoproterozoic Cryogenian Snowball interval, ~720-635 million years ago, suggest that post-Snowball fertilization of shallow continental margin seawater with phosphorus accelerated marine primary productivity, ocean-atmosphere oxygenation, and ultimately the rise of animals. However, the mechanisms that sourced and delivered bioavailable phosphate from land to the ocean are not fully understood. Here we demonstrate a causal relationship between clay mineral production by the melting Sturtian Snowball ice sheets and a short-lived increase in seawater phosphate bioavailability by at least 20-fold and oxygenation of an immediate post-Sturtian Snowball ocean margin. Bulk primary sediment inputs and inferred dissolved seawater phosphate dynamics point to a relatively low marine phosphate inventory that limited marine primary productivity and seawater oxygenation before the Sturtian glaciation, and again in the later stages of the succeeding interglacial greenhouse interval.
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hal-04520815 , version 1 (26-03-2024)

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Ernest Chi Fru, Jalila Al Bahri, Christophe Brosson, Olabode Bankole, Jérémie Aubineau, et al.. Transient fertilization of a post-Sturtian Snowball ocean margin with dissolved phosphate by clay minerals. Nature Communications, 2023, 14 (1), pp.8418. ⟨10.1038/s41467-023-44240-9⟩. ⟨hal-04520815⟩
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