Post-depositional processes: What really happens to new atmospheric iron in the ocean's surface?

Matthieu Bressac, Cecile Guieu

Research output: Contribution to journalArticle

Abstract

Abiotic iron removal processes such as scavenging can significantly and rapidly modify iron distribution in the dissolved-colloidal-particulate continuum. Therefore, these processes could be considered, in addition to ligand complexation, as a major control on atmospheric iron dissolution in seawater. In this work, we investigated the seasonal abiotic processes occurring once dust deposited on surface seawater using a series of artificial seeding experiments (allowing us to take into consideration the settling of particles on a 1 m depth layer). Here, we demonstrate that atmospheric dissolved iron concentration ([DFe]) is driven by the processes governed by the dissolved organic matter (DOM) pool. Following artificial dust seeding, an order magnitude range increase in the [DFe] (12 - 181 nmol L-1) was observed depending on the season. Under high and fresh DOM conditions (spring and summer), the rapid formation of aggregates induced a negative feedback on the [DFe] through scavenging, while a fraction of the DFe was likely organically complexed. In contrast, in low-DOM surface waters (winter), aggregation was not observed, allowing a very large transient increase in [DFe] (181 nmol L-1) before being removed by adsorption onto settling particles. A key result of the findings is that depending on the age and quantity of DOM, the "lithogenic carbon pump" is likely a major pathway for organic carbon export. Modeling studies should therefore relate both atmospheric iron dissolution in seawater and the intensity of the subsequent biological response, to the age and quantity of DOM. Key Points Atmospheric iron dissolution is driven by the dissolved organic matter poolSeawater biogeochemical conditions are a key determinant of iron solubilityLithogenic carbon pump is likely a major pathway for organic carbon export.

Original languageEnglish (US)
Pages (from-to)859-870
Number of pages12
JournalGlobal Biogeochemical Cycles
Volume27
Issue number3
DOIs
StatePublished - Sep 4 2013

Fingerprint

Biological materials
sea surface
dissolved organic matter
Iron
iron
Seawater
Dissolution
Scavenging
Organic carbon
dissolution
Dust
seawater
seeding
Carbon
Pumps
pump
organic carbon
dust
particle settling
Complexation

Keywords

  • adsorption
  • aggregation
  • atmospheric dissolved iron
  • dissolved organic matter
  • scavenging

ASJC Scopus subject areas

  • Global and Planetary Change
  • Atmospheric Science
  • Environmental Science(all)
  • Environmental Chemistry

Cite this

Post-depositional processes : What really happens to new atmospheric iron in the ocean's surface? / Bressac, Matthieu; Guieu, Cecile.

In: Global Biogeochemical Cycles, Vol. 27, No. 3, 04.09.2013, p. 859-870.

Research output: Contribution to journalArticle

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