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Rebecca Pickering

Rebecca Pickering

Postdoctoral fellow

Rebecca Pickering

The biogeochemical impact of glacial meltwater from Southwest Greenland

Author

  • Katharine R. Hendry
  • Rebecca Pickering
  • Veerle A.I. Huvenneb
  • Laura F. Robinson
  • Amber Annett
  • Marcus Badger
  • Allison W. Jacobel
  • Hong Chin Ng
  • Jacob Opher
  • Michelle L. Taylor
  • Stephanie L. Bates
  • Adam Cooper
  • Grace G. Cushman
  • Claire Goodwin
  • Shannon Hoy
  • George Rowland
  • Ana Samperiz
  • James A. Williams
  • Eric P. Achterberg
  • Carol Arrowsmith
  • J. Alexander Brearley
  • Sian F. Henley
  • Jeffrey W. Krause
  • Melanie J. Leng
  • Tao Li
  • Jerry F. McManus
  • Michael P. Meredith
  • Rupert Perkins
  • E. Malcolm S. Woodward

Summary, in English

Biogeochemical cycling in high-latitude regions has a disproportionate impact on global nutrient budgets. Here, we introduce a holistic, multi-disciplinary framework for elucidating the influence of glacial meltwaters, shelf currents, and biological production on biogeochemical cycling in high-latitude continental margins, with a focus on the silica cycle. Our findings highlight the impact of significant glacial discharge on nutrient supply to shelf and slope waters, as well as surface and benthic production in these regions, over a range of timescales from days to thousands of years. Whilst biological uptake in fjords and strong diatom activity in coastal waters maintains low dissolved silicon concentrations in surface waters, we find important but spatially heterogeneous additions of particulates into the system, which are transported rapidly away from the shore. We expect the glacially-derived particles – together with biogenic silica tests – to be cycled rapidly through shallow sediments, resulting in a strong benthic flux of dissolved silicon. Entrainment of this benthic silicon into boundary currents may supply an important source of this key nutrient into the Labrador Sea, and is also likely to recirculate back into the deep fjords inshore. This study illustrates how geochemical and oceanographic analyses can be used together to probe further into modern nutrient cycling in this region, as well as the palaeoclimatological approaches to investigating changes in glacial meltwater discharge through time, especially during periods of rapid climatic change in the Late Quaternary.

Publishing year

2019-09

Language

English

Publication/Series

Progress in Oceanography

Volume

176

Document type

Journal article

Publisher

Elsevier

Topic

  • Geochemistry
  • Oceanography, Hydrology, Water Resources

Keywords

  • Biogeochemistry
  • Silica cycling
  • Nutrients
  • Primary production
  • Glaciers

Status

Published

ISBN/ISSN/Other

  • ISSN: 0079-6611