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Protracted oxygenation across the Cambrian–Ordovician transition : A key initiator of the Great Ordovician Biodiversification Event?

Kozik, Nevin P. (författare)
Florida State University
Young, Seth A. (författare)
Florida State University
Lindskog, Anders (författare)
Lund University,Lunds universitet,Berggrundsgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Lithosphere and Biosphere Science,Department of Geology,Faculty of Science,Florida State University
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Ahlberg, Per (författare)
Lund University,Lunds universitet,Berggrundsgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Lithosphere and Biosphere Science,Department of Geology,Faculty of Science
Owens, Jeremy D. (författare)
Florida State University
visa färre...
 (creator_code:org_t)
2023-01-26
2023
Engelska.
Ingår i: Geobiology. - : Wiley. - 1472-4677 .- 1472-4669. ; 21:3, s. 323-340
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • Fluctuations in marine oxygen concentrations have been invoked as a primary driver for changes in biodiversity throughout Earth history. Expansions in reducing marine conditions are commonly invoked as key causal mechanisms for mass extinctions, while increases in marine oxygenation are becoming an increasingly common causal mechanism invoked for biodiversification events. Here we utilize a multiproxy approach to constrain local and global marine paleoredox conditions throughout the late Cambrian–Early Ordovician from two drill core successions in Baltoscandia. Local paleoredox proxies such as manganese concentrations and iron speciation reveal that both sites in the Baltic paleobasin had persistently anoxic and predominantly euxinic (anoxic and sulfidic) bottom water conditions throughout the study interval. Corresponding trace metal datasets indicate nuanced contraction and expansion of global anoxic and euxinic conditions along continental margins during the late Cambrian–Early Ordovician. Lastly, thallium isotope data from these locally reducing sections suggest a global expansion of oxygenated shelf and deeper marine environments from the late Cambrian into the Early Ordovician. This evidence for increasingly oxic marine environments coincides with increases in burrowing depth and tiering in marine animals, as well as diversification of body fossils throughout this ~8-million-year interval. The collective geochemical datasets provide some of the first direct paleoredox evidence for an increase in marine oxygen concentrations as a key mechanism for the Ordovician radiation of marine life.

Ämnesord

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

Nyckelord

anoxia
biodiversity
Cambrian
molybdenum
Ordovician
thallium isotopes
vanadium

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Av författaren/redakt...
Kozik, Nevin P.
Young, Seth A.
Lindskog, Anders
Ahlberg, Per
Owens, Jeremy D.
Om ämnet
NATURVETENSKAP
NATURVETENSKAP
och Geovetenskap och ...
och Geologi
Artiklar i publikationen
Geobiology
Av lärosätet
Lunds universitet

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