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

Conwell, Christopher T. ; Saltzman, Matthew R. ; Lindskog, Anders LU ; Eriksson, Mats E. LU ; Griffith, Elizabeth M. ; Leslie, Stephen A. ; Edwards, Cole T. ; Hints, Olle and Herrmann, Achim D. (2026) In Palaeogeography, Palaeoclimatology, Palaeoecology 685.
Abstract

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... (More)

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.

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Contribution to journal
publication status
published
subject
keywords
Carbonates, Chemostratigraphy, Conodont, Diagenesis, Geochemistry, Sr isotope
in
Palaeogeography, Palaeoclimatology, Palaeoecology
volume
685
article number
113524
publisher
Elsevier
external identifiers
  • scopus:105027073706
ISSN
0031-0182
DOI
10.1016/j.palaeo.2025.113524
language
English
LU publication?
yes
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Publisher Copyright: © 2025 Elsevier B.V.
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22dea282-79a6-4845-8404-18b2b4917bf1
date added to LUP
2026-03-23 16:14:22
date last changed
2026-03-23 17:28:42
@article{22dea282-79a6-4845-8404-18b2b4917bf1,
  abstract     = {{<p>Despite frequent use of conodonts as an archive for seawater <sup>87</sup>Sr/<sup>86</sup>Sr, available diagenetic screening tools are inconsistent predictors of primary seawater <sup>87</sup>Sr/<sup>86</sup>Sr preservation. Here, we attempt to isolate variables affecting the preservation of seawater <sup>87</sup>Sr/<sup>86</sup>Sr in conodonts. We present new Middle–Late Ordovician (∼470–450 Ma) conodont <sup>87</sup>Sr/<sup>86</sup>Sr 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 <sup>87</sup>Sr/<sup>86</sup>Sr measurements from Kårgärde and Estonian sections are offset from global seawater by ∼ +2 × 10<sup>−4</sup> but preserve the overall structure of the seawater curve, suggesting minor diagenetic Sr exchange. <sup>87</sup>Sr/<sup>86</sup>Sr measurements from the more argillaceous Fjäcka section show extensive alteration with highly radiogenic values as much as ∼6 × 10<sup>−4</sup> 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 <sup>87</sup>Sr/<sup>86</sup>Sr 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 (<sup>87</sup>Sr/<sup>86</sup>Sr<sub>conodont</sub> – <sup>87</sup>Sr/<sup>86</sup>Sr<sub>seawater</sub>) reveal that paleolatitude and associated differences in sedimentation rate affect preservation of seawater <sup>87</sup>Sr/<sup>86</sup>Sr 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 <sup>87</sup>Sr/<sup>86</sup>Sr records using conodont apatite target low-latitude settings with high sedimentation rate and CAI ≤ 2.</p>}},
  author       = {{Conwell, Christopher T. and Saltzman, Matthew R. and Lindskog, Anders and Eriksson, Mats E. and Griffith, Elizabeth M. and Leslie, Stephen A. and Edwards, Cole T. and Hints, Olle and Herrmann, Achim D.}},
  issn         = {{0031-0182}},
  keywords     = {{Carbonates; Chemostratigraphy; Conodont; Diagenesis; Geochemistry; Sr isotope}},
  language     = {{eng}},
  month        = {{03}},
  publisher    = {{Elsevier}},
  series       = {{Palaeogeography, Palaeoclimatology, Palaeoecology}},
  title        = {{Factors affecting <sup>87</sup>Sr/<sup>86</sup>Sr preservation in conodont apatite : An example from the Ordovician of Baltoscandia}},
  url          = {{http://dx.doi.org/10.1016/j.palaeo.2025.113524}},
  doi          = {{10.1016/j.palaeo.2025.113524}},
  volume       = {{685}},
  year         = {{2026}},
}