Circumpolar Deep Water upwelling is a primary source of 10Be in Antarctic continental shelf sediments

  • Matt Jeromson
  • , Toshiyuki Fujioka
  • , David Fink
  • , Krista Simon
  • , James Smith
  • , Claus Dieter Hillenbrand
  • , Gerhard Kuhn
  • , Alexandra L. Post
  • , Jose Tonatiuh SANCHEZ-PALACIOS
  • , Marcello Blaxell
  • , T. Gabriel Enge
  • , Duanne White

    Research output: Contribution to journalArticlepeer-review

    Abstract

    Beryllium-10 (10Be) has been proposed as a potential proxy for investigating ice shelf presence and absence, or meltwater discharge in coastal polar environments. However, the sources and distribution of atmospherically produced meteoric-10Be in the Antarctic marine realm are yet to be fully characterized, making any inferences about its concentration in sediments challenging. We present a dataset of 9Be and 10Be concentrations, and 10Be/9Be ratios in seafloor surface sediments from the Antarctic continental shelf - including from sub ice shelf cores - to assess the sources and processes contributing Be-isotopes to ice-sheet proximal marine settings. We show that upwelling waters (e.g. Circumpolar Deep Water) are a significant source of 10Be to continental shelf sediments. This limits the use of 10Be/9Be as a proxy for ice shelf environment or meltwater discharge, but instead provides a potential proxy for reconstructing Circumpolar Deep Water incursions onto Antarctic continental shelves.
    Original languageEnglish
    Article number104424
    Pages (from-to)1-11
    Number of pages11
    JournalGlobal and Planetary Change
    Volume236
    DOIs
    Publication statusPublished - May 2024

    UN SDGs

    This output contributes to the following UN Sustainable Development Goals (SDGs)

    1. SDG 14 - Life Below Water
      SDG 14 Life Below Water

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