Cardiff University | Prifysgol Caerdydd ORCA
Online Research @ Cardiff 
WelshClear Cookie - decide language by browser settings

Enhanced trace element mobilization by Earth’s ice sheets

Hawkings, Jon R., Skidmore, Mark L., Wadham, Jemma L., Priscu, John C., Morton, Peter L., Hatton, Jade E., Gardner, Christopher B., Kohler, Tyler J., Stibal, Marek, Bagshaw, Elizabeth A., Steigmeyer, August, Barker, Joel, Dore, John E., Lyons, W. Berry, Tyanter, Martyn, Spencer, Robert G. M. and SALSA Science Team, . 2020. Enhanced trace element mobilization by Earth’s ice sheets. Proceedings of the National Academy of Sciences 117 (50) , pp. 31648-31659. 10.1073/pnas.2014378117

[img] PDF - Accepted Post-Print Version
Download (2MB)

Abstract

Trace elements sustain biological productivity, yet the significance of trace element mobilization and export in subglacial runoff from ice sheets is poorly constrained at present. Here, we present size-fractionated (0.02, 0.22, and 0.45 µm) concentrations of trace elements in subglacial waters from the Greenland Ice Sheet (GrIS) and the Antarctic Ice Sheet (AIS). Concentrations of immobile trace elements (e.g., Al, Fe, Ti) far exceed global riverine and open ocean mean values and highlight the importance of subglacial aluminosilicate mineral weathering and lack of retention of these species in sediments. Concentrations are higher from the AIS than the GrIS, highlighting the geochemical consequences of prolonged water residence times and hydrological isolation that characterize the former. The enrichment of trace elements (e.g., Co, Fe, Mn, and Zn) in subglacial meltwaters compared with seawater and typical riverine systems, together with the likely sensitivity to future ice sheet melting, suggests that their export in glacial runoff is likely to be important for biological productivity. For example, our dissolved Fe concentration (20,900 nM) and associated flux values (1.4 Gmol y−1) from AIS to the Fe-deplete Southern Ocean exceed most previous estimates by an order of magnitude. The ultimate fate of these micronutrients will depend on the reactivity of the dominant colloidal size fraction (likely controlled by nanoparticulate Al and Fe oxyhydroxide minerals) and estuarine processing. We contend that ice sheets create highly geochemically reactive particulates in subglacial environments, which play a key role in trace elemental cycles, with potentially important consequences for global carbon cycling.

Item Type: Article
Date Type: Publication
Status: Published
Schools: Earth and Ocean Sciences
Publisher: National Academy of Sciences
ISSN: 0027-8424
Date of First Compliant Deposit: 27 October 2020
Date of Acceptance: 13 October 2020
Last Modified: 23 May 2021 02:05
URI: http://orca.cardiff.ac.uk/id/eprint/135976

Actions (repository staff only)

Edit Item Edit Item