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Redox dynamics of later Cambrian oceans

Gill, Benjamin C. (författare)
Virginia Polytechnic Institute and State University
Dahl, Tais W. (författare)
University of Copenhagen
Hammarlund, Emma U. (författare)
Lund University,Lunds universitet,Berggrundsgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Molekylär evolution,Forskargrupper vid Lunds universitet,Lithosphere and Biosphere Science,Department of Geology,Faculty of Science,Molecular Evolution,Lund University Research Groups
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LeRoy, Matthew A. (författare)
Virginia Polytechnic Institute and State University
Gordon, Gwyneth W. (författare)
Arizona State University
Canfield, Donald E. (författare)
University of Southern Denmark
Anbar, Ariel D. (författare)
Lund University
Lyons, Timothy W. (författare)
University of California, Riverside
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 (creator_code:org_t)
Elsevier BV, 2021
2021
Engelska.
Ingår i: Palaeogeography, Palaeoclimatology, Palaeoecology. - : Elsevier BV. - 0031-0182. ; 581
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • A growing body of evidence suggests that the deep oceans during the early Paleozoic Era were widely oxygen deficient, despite evidence for increased marine oxygenation during the Neoproterozoic. However, the temporal and geographic extents and dynamics of reducing marine conditions within these oceans are not well understood. Here, we investigate marine redox history during the Drumian through the earliest Jiangshanian International Stages of the Cambrian Period, using concentrations of redox-sensitive metals (vanadium, uranium, and molybdenum), iron speciation, and Mo isotope stratigraphy of the Alum Shale Formation of Scandinavia. These data suggest a major perturbation occurred in trace metal cycling during the later Cambrian Period that was linked to a transient change in marine redox conditions coincident with the well-known Steptoean Positive Isotope Excursion or SPICE. The δ98Mo measurements of the Alum shale show systematic variations during the interval that contains the SPICE which are broadly consistent with a transient expansion of sulfidic, reducing marine environments — indicating a significant exacerbation of an already-common condition during the Cambrian Period. Additionally, iron speciation data record a local transition from predominantly anoxic, ferruginous (Fe+2 containing) to anoxic, euxinic (sulfide containing) water column conditions near the initiation of the SPICE. Trace metal abundances, however, appear to decline well before the start of the SPICE, suggesting an earlier initiation of the global expansion of reducing environments. More broadly, our data and modeling support the notion that significant portions of the oceans remained oxygen deficient throughout the later portion of the Cambrian, and that these oceans were also prone to transient intervals of more reducing conditions similar to the Oceanic Anoxic Events of the Mesozoic.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)

Nyckelord

Cambrian
Iron Speciation
Marine redox
Molybdenum isotopes
SPICE
Trace metals

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art (ämneskategori)
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