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Mats Eriksson

Mats Eriksson

Professor

Mats Eriksson

Factors affecting 87Sr/86Sr preservation in conodont apatite : An example from the Ordovician of Baltoscandia

Author

  • Christopher T. Conwell
  • Matthew R. Saltzman
  • Anders Lindskog
  • Mats E. Eriksson
  • Elizabeth M. Griffith
  • Stephen A. Leslie
  • Cole T. Edwards
  • Olle Hints
  • Achim D. Herrmann

Summary, in English

Despite frequent use of conodonts as an archive for seawater 87Sr/86Sr, available diagenetic screening tools are inconsistent predictors of primary seawater 87Sr/86Sr preservation. Here, we attempt to isolate variables affecting the preservation of seawater 87Sr/86Sr in conodonts. We present new Middle–Late Ordovician (∼470–450 Ma) conodont 87Sr/86Sr from mid-paleolatitude (30–45°S) carbonate successions from central Sweden (Fjäcka, Kårgärde) and Estonia (Uuga Cliff, Viki borehole) which have low Conodont Alteration Index (CAI) values of 1–1.5. Coeval 87Sr/86Sr measurements from Kårgärde and Estonian sections are offset from global seawater by ∼ +2 × 10−4 but preserve the overall structure of the seawater curve, suggesting minor diagenetic Sr exchange. 87Sr/86Sr measurements from the more argillaceous Fjäcka section show extensive alteration with highly radiogenic values as much as ∼6 × 10−4 greater than global seawater and a stratigraphic trend that diverges from the seawater curve. This may be explained by highly radiogenic Sr contribution from the Kinnekulle K-bentonite and Fjäcka shale units that occur at Fjäcka section. We compiled 1164 conodont 87Sr/86Sr measurements spanning ∼485–250 Ma and categorized measurements by host rock, sample preparation, paleolatitude, and CAI. Boxplots and Mann-Whitney U testing of residual values relative to the seawater curve (87Sr/86Srconodont87Sr/86Srseawater) reveal that paleolatitude and associated differences in sedimentation rate affect preservation of seawater 87Sr/86Sr values in conodonts. The relative abundance of clay minerals did not significantly correlate with residual values for conodonts from mid- or low-latitude deposits. We recommend that future investigations of seawater 87Sr/86Sr records using conodont apatite target low-latitude settings with high sedimentation rate and CAI ≤ 2.

Department/s

  • Department of Earth and Environmental Sciences (MGeo)
  • Department of Geology

Publishing year

2026-03-01

Language

English

Publication/Series

Palaeogeography, Palaeoclimatology, Palaeoecology

Volume

685

Document type

Journal article

Publisher

Elsevier

Topic

  • Geology

Keywords

  • Carbonates
  • Chemostratigraphy
  • Conodont
  • Diagenesis
  • Geochemistry
  • Sr isotope

Status

Published

ISBN/ISSN/Other

  • ISSN: 0031-0182