Heavy metal, sex and granites: Crustal differentiation and bioavailability in the mid-Proterozoic

John Parnell, Malcolm Hole, Adrian J. Boyce, Samuel Spinks, Stephen Bowden

Research output: Contribution to journalArticle

19 Citations (Scopus)

Abstract

Biogeochemical and genomic studies have suggested that the availability of trace metals has been essential to the progressive evolution of life on Earth. In particular, the evolution of eukaryotes to diverse complex multicellular life has been related to the availability of trace metals. The radiation of eukaryotes, and the evolution of sex, is timed at Mesoproterozoic, but at this time the metals may have been preferentially sequestered in a sulfidic deep ocean. However, the addition of a huge volume of new crust to form a supercontinent at c. 1.9 Ga, including an unprecedented episode of within-plate anorogenic magmatism, led to an extraordinary new flux of metals to the upper crust in the mid-Proterozoic. The appearance of sulfate evaporites from ~1.7–1.6 Ga indicates extensive weathering of metallic sulfides. Erosion of the supercontinent into Mesoproterozoic sediments thence introduced key metals to near surface reservoirs, providing an enhanced biogeochemical environment conducive to the expansion of an evolving biota.
Original languageEnglish
Pages (from-to)751-754
Number of pages4
JournalGeology
Volume40
Issue number8
Early online date8 Jun 2012
DOIs
Publication statusPublished - Aug 2012

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bioavailability
Proterozoic
supercontinent
eukaryote
heavy metal
trace metal
metal
evaporite
upper crust
biota
magmatism
genomics
weathering
sulfide
crust
sulfate
erosion
ocean
sediment
radiation

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Heavy metal, sex and granites : Crustal differentiation and bioavailability in the mid-Proterozoic. / Parnell, John; Hole, Malcolm; Boyce, Adrian J.; Spinks, Samuel; Bowden, Stephen.

In: Geology, Vol. 40, No. 8, 08.2012, p. 751-754.

Research output: Contribution to journalArticle

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