Arsenic stress after the Proterozoic glaciations

Fru, EC; Arvestål, E; Callac, N; El Albani, A; Kilias, S; Argyraki, A; Jakobsson, M

HERO ID

3379040

Reference Type

Journal Article

Year

2015

Language

English

PMID

26635187

HERO ID 3379040
In Press No
Year 2015
Title Arsenic stress after the Proterozoic glaciations
Authors Fru, EC; Arvestål, E; Callac, N; El Albani, A; Kilias, S; Argyraki, A; Jakobsson, M
Journal Scientific Reports
Volume 5
Page Numbers 17789
Abstract Protection against arsenic damage in organisms positioned deep in the tree of life points to early evolutionary sensitization. Here, marine sedimentary records reveal a Proterozoic arsenic concentration patterned to glacial-interglacial ages. The low glacial and high interglacial sedimentary arsenic concentrations, suggest deteriorating habitable marine conditions may have coincided with atmospheric oxygen decline after ~2.1 billion years ago. A similar intensification of near continental margin sedimentary arsenic levels after the Cryogenian glaciations is also associated with amplified continental weathering. However, interpreted atmospheric oxygen increase at this time, suggests that the marine biosphere had widely adapted to the reorganization of global marine elemental cycles by glaciations. Such a glacially induced biogeochemical bridge would have produced physiologically robust communities that enabled increased oxygenation of the ocean-atmosphere system and the radiation of the complex Ediacaran-Cambrian life.
Doi 10.1038/srep17789
Pmid 26635187
Wosid WOS:000365882300002
Is Certified Translation No
Dupe Override No
Is Public Yes
Language Text English