Skip to main content

Research Repository

Advanced Search

The biogeochemical impact of glacial meltwater from Southwest Greenland

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

Authors

Katharine R. Hendry

Veerle A.I. Huvenne

Laura F. Robinson

Amber Annett

Marcus Badger

Allison W. Jacobel

Hong Chin Ng

Jacob Opher

Rebecca A. Pickering

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

Tao Li

Jerry F. McManus

Michael P. Meredith

Rupert Perkins

E. Malcolm S. Woodward



Abstract

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.

Citation

Hendry, K. R., Huvenne, V. A., Robinson, L. F., Annett, A., Badger, M., Jacobel, A. W., …Woodward, E. M. S. (2019). The biogeochemical impact of glacial meltwater from Southwest Greenland. Progress in Oceanography, 176, Article 102126. https://doi.org/10.1016/j.pocean.2019.102126

Journal Article Type Article
Acceptance Date Jun 15, 2019
Online Publication Date Jun 17, 2019
Publication Date Sep 30, 2019
Deposit Date Jun 26, 2019
Publicly Available Date Jun 18, 2020
Journal Progress in Oceanography
Print ISSN 0079-6611
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 176
Article Number 102126
DOI https://doi.org/10.1016/j.pocean.2019.102126
Keywords Aquatic Science; Geology
Public URL https://nottingham-repository.worktribe.com/output/2230769
Publisher URL https://www.sciencedirect.com/science/article/pii/S0079661118302817

Files




You might also like



Downloadable Citations