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Journal Of Inorganic Biochemistry • September 2003<br />

A biogeochemical cycle for aluminium?<br />

Author information<br />

Exley C1.<br />

Birchall Centre for Inorganic Chemistry and Materials Science<br />

Keele University, Staffordshire ST5 5BG, UK<br />

c.exley@chem.keele.ac.uk<br />

Abstract<br />

The elaboration of biogeochemical cycles for elements which are known<br />

to be essential for life has enabled a broad appreciation of the homeostatic<br />

mechanisms which underlie element essentiality. In particular<br />

they can be used effectively to identify any part played by human activities<br />

in element cycling and to predict how such activities might impact<br />

upon the lithospheric and biospheric availability of an element in the<br />

future. The same criteria were the driving force behind the construction<br />

of a biogeochemical cycle for aluminium, a non-essential element<br />

which is a known ecotoxicant and a suspected health risk in humans.<br />

The purpose of this exercise was to examine the concept of a biogeochemical<br />

cycle for aluminium and not to review the biogeochemistry<br />

of this element. The cycle as presented is rudimentary and qualitative<br />

though, even in this nascent form, it is informative and predictive and,<br />

for these reasons alone, it is deserving of future quantification. A fully<br />

fledged biogeochemical cycle for aluminium should explain the biospheric<br />

abundance of this element and whether we should expect its<br />

(continued) active involvement in biochemical evolution.<br />

“a non-essential element<br />

which is a known ecotoxicant and a<br />

suspected health risk in humans.”<br />

http://www.ncbi.nlm.nih.gov/pubmed/14507454

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