eCite Digital Repository

Hydrothermal contribution to the oceanic dissolved iron inventory

Citation

Tagliabue, A and Boop, L and Dutay, JC and Bowie, AR and Chever, F and Jean-Baptiste, P and Bucciarelli, E and Lannuzel, D and Remenyi, TA and Sarthou, G and Aumont, O and Gehlen, M and Jeandel, C, Hydrothermal contribution to the oceanic dissolved iron inventory, Nature Geoscience, 3, (4) pp. 252-256. ISSN 1752-0894 (2010) [Refereed Article]


Preview
PDF
Restricted - Request a copy
435Kb
  

Copyright Statement

Copyright © 2011 Nature Publishing Group http://www.nature.com/

Official URL: http://www.nature.com/ngeo/journal/v3/n4/full/ngeo...

DOI: doi:10.1038/ngeo818

Abstract

Iron limits phytoplankton growth and hence the biological carbon pump in the Southern Ocean1. Models assessing the impacts of iron on the global carbon cycle generally rely on dust input and sediment resuspension as the predominant sources2,3. Although it was previously thought that most iron from deep-ocean hydrothermal activity was inaccessible to phytoplankton because of the formation of particulates4, it has been suggested that iron from hydrothermal activity5–7 may be an important source of oceanic dissolved iron8–13. Here we use a global ocean model to assess the impacts of an annual dissolved iron flux of approximately 9  108 mol, as estimated from regional observations of hydrothermal activity11,12, on the dissolved iron inventory of the world’s oceans. We find the response to the input of hydrothermal dissolved iron is greatest in the Southern Hemisphere oceans. In particular, observations of the distribution of dissolved iron in the Southern Ocean3 (Chever et al., manuscript in preparation; Bowie et al., manuscript in preparation) can be replicated in our simulations only when our estimated iron flux from hydrothermal sources is included. As the hydrothermal flux of iron is relatively constant over millennial timescales14, we propose that hydrothermal activity can buffer the oceanic dissolved iron inventory against shorter-term fluctuations in dust deposition.

Item Details

Item Type:Refereed Article
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Chemical Oceanography
Objective Division:Environment
Objective Group:Physical and Chemical Conditions of Water
Objective Field:Physical and Chemical Conditions of Water in Marine Environments
Author:Bowie, AR (Associate Professor Andrew Bowie)
Author:Lannuzel, D (Dr Delphine Lannuzel)
Author:Remenyi, TA (Dr Tom Remenyi)
ID Code:67548
Year Published:2010
Web of Science® Times Cited:152
Deposited By:CRC-Antarctic Climate & Ecosystems
Deposited On:2011-03-04
Last Modified:2011-05-09
Downloads:13 View Download Statistics

Repository Staff Only: item control page