Iron isotopes as a tool in oceanography

Jul 31, 2009

New research involving scientists from the National Oceanography Centre, Southampton (NOCS) highlights the potential utility of iron isotopes for addressing important questions in ocean science. The findings are published in the August edition of the journal Geology.

Large regions of the world's oceans have low primary production despite having plenty of macronutrients such as phosphate, nitrate and silicate. This is due a shortage of the essential micro-nutrient iron, which is needed for the growth of phytoplankton. These tiny, plant-like organisms sit at the base of the marine food chain and collectively draw vast amounts of the greenhouse gas carbon dioxide down from the atmosphere through the process of photosynthesis.

A proportion of the carbon is exported to the deep ocean, making the oceans a major carbon dioxide sink, without which global warming would rapidly accelerate. The natural supply of iron to such 'High Nutrient Low Chlorophyll (HNLC) regions is therefore, albeit indirectly, an important determinant of climate.

The importance of dissolved iron in derived from bottom (benthic) sediments is increasingly recognised as being important. Around the continental margins, in particular, iron is released from the sediments during the decomposition of organic carbon by dissimilatory iron-reducing bacteria - micro-organisms that use elemental iron to obtain energy. This leads to the enrichment of iron in pore fluids and bottom waters. However the ubiquity of sedimentary iron inputs to seawater remains unknown.

Different biological and chemical processes can leave behind characteristic isotopic 'fingerprints'. Of specific interest here, iron isotopes in sediment pore fluids may be a unique tracer of sediment respiration by dissimilatory iron-reducing bacteria.

Dissimilatory iron reduction is thought to be one of the earliest metabolic pathways on Earth , thus sedimentary iron isotopes may also be useful in reconstructing past iron cycling in the ancient ocean.

Pore-fluid iron isotope measurements have so far been restricted to the continental shelves where the supply of carbon is typically high and dissimilatory iron reduction is extensive, precluding comparisons with low-carbon, deep-water environments. William Homoky, who is a research student at the University of Southampton's School of Ocean and Earth Sciences based at NOCS, and his colleagues have helped fill this gap be measuring iron isotopes in pore fluids from both the Eel River shelf on the northern California margin (120 m water depth), and deep-sea sediments from the Southern Ocean around the Crozet Island Plateau (3000 m water depth), about 1400 miles southeast of South Africa.

"We are excited by our findings not only because they represent the first measurements of their kind, but because they are telling us something important about iron cycling processes in the deep-sea, which can inform future iron isotope investigations in ancient rocks and the modern oceans," said William Homoky.

They find that the composition of iron isotopes in the pore fluids reflects the different extent of sedimentary iron recycling between the two sites. Specifically, the pore-fluid iron isotope compositions reflect the extent of iron recycling during early diagenesis, which is driven by organic carbon inputs from the overlying water column.

The researchers believe that iron isotope processing in carbon-limited environments, such as the deep-sea, is important and that it should help future interpretations of the rock record. "Additionally," they say, "the unique isotopic fingerprint of pore fluid iron in continental shelf settings is confirmed, highlighting the potential for iron isotopes to trace the inputs of continental shelf-derived iron in seawater."

Current thesis research aims to improve our understanding of iron cycling between sediments and seawater and compares the affects of contrasting sediment geochemistry on iron flux generating processes.

"In the future I would like to examine processes of sedimentary cycling in the high-latitudes, where sediments are subject to enhanced rates of environmental change due to changing climate in these regions," Said Homoky.

More information: Homoky, W., S. Severmann, S., Mills, R., Statham, P. & Fones, G. Pore-fluid Fe isotopes reflect the extent of benthic Fe redox recycling: Evidence from continental shelf and deep-sea sediments. Geology XXX, xxxx-xxxx (2009).

Source: National Oceanography Centre, Southampton

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omatumr
2 / 5 (3) Jul 31, 2009
ISOTOPE FINGERPRINTS

This is an exciting development and I look forward to reading more about the findings. The measurement will be more difficult than measuring the isotope fingerprint of lightweight elements.

Stable isotope studies have provided a great deal of information on the origin of the solar system and the subsequent redistribution by processes that sort isotopes by mass (mass-fractionate the isotopes).

Mass fractionation is most easily observed in lightweight elements, like carbon or oxygen, because fractional differences in isotope masses are greater for the lighter elements.

The stable isotopes of iron are Fe-54 (5.8%), Fe-56 (91.8%), Fe-57 (2.15%) and Fe-58 (0.29%). Relative to the most abundant isotope, the maximum fractional mass difference is only 2/56 = ~3.6 %.

By comparison, the maximum fractional mass differences relative to the most abundant isotope of oxygen (O-16) is 2/16 = ~12.5 %.

With kind regard,
Oliver K. Manuel
http://www.omatumr.com