A high-resolution nonmarine record of an early Danian hyperthermal event, Boltysh crater, Ukraine

Iain Gilmour*, Mabs Gilmour, David Jolley, Simon Kelley, David Kemp, Robert Daly, Jonathan Watson

*Corresponding author for this work

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

Carbon isotope and palynological analysis of the fine-grained organic carbon-rich lacustrine sediments that filled the Cretaceous-Paleogene (K-Pg) boundary-age Boltysh impact crater (Ukraine) preserve a uniquely complete and detailed record of a negative carbon isotope excursion in an expanded section of the early Danian that we estimate lasted as long as similar to 340 k.y. Palynological assemblages recovered through the excursion reflect the increasing dominance of thermophylic Normapolles species, indicating an increasingly warm and dry climate, while those recovered below and above the excursion reflect a cooler and wetter climate. The record of a transient warming event (hyperthermal) in the early Danian at Boltysh has strong similarities with the Dan-C2 hyperthermal event recorded in marine sediments in Tethys and the Atlantic Ocean, and suggests that there were profound environmental changes occurring on a global scale shortly after the K-Pg boundary.

Original languageEnglish
Pages (from-to)783-786
Number of pages4
JournalGeology
Volume41
Issue number7
Early online date16 May 2013
DOIs
Publication statusPublished - Jul 2013

Keywords

  • cretaceous-paleogene boundary
  • paleocene-eocene boundary
  • carbon reservoirs
  • thermal maximum
  • organic-matter
  • time scales
  • isotope
  • impact
  • basin
  • end

Cite this

Gilmour, I., Gilmour, M., Jolley, D., Kelley, S., Kemp, D., Daly, R., & Watson, J. (2013). A high-resolution nonmarine record of an early Danian hyperthermal event, Boltysh crater, Ukraine. Geology, 41(7), 783-786. https://doi.org/10.1130/G34292.1

A high-resolution nonmarine record of an early Danian hyperthermal event, Boltysh crater, Ukraine. / Gilmour, Iain; Gilmour, Mabs; Jolley, David; Kelley, Simon; Kemp, David; Daly, Robert; Watson, Jonathan.

In: Geology, Vol. 41, No. 7, 07.2013, p. 783-786.

Research output: Contribution to journalArticle

Gilmour, I, Gilmour, M, Jolley, D, Kelley, S, Kemp, D, Daly, R & Watson, J 2013, 'A high-resolution nonmarine record of an early Danian hyperthermal event, Boltysh crater, Ukraine', Geology, vol. 41, no. 7, pp. 783-786. https://doi.org/10.1130/G34292.1
Gilmour, Iain ; Gilmour, Mabs ; Jolley, David ; Kelley, Simon ; Kemp, David ; Daly, Robert ; Watson, Jonathan. / A high-resolution nonmarine record of an early Danian hyperthermal event, Boltysh crater, Ukraine. In: Geology. 2013 ; Vol. 41, No. 7. pp. 783-786.
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N2 - Carbon isotope and palynological analysis of the fine-grained organic carbon-rich lacustrine sediments that filled the Cretaceous-Paleogene (K-Pg) boundary-age Boltysh impact crater (Ukraine) preserve a uniquely complete and detailed record of a negative carbon isotope excursion in an expanded section of the early Danian that we estimate lasted as long as similar to 340 k.y. Palynological assemblages recovered through the excursion reflect the increasing dominance of thermophylic Normapolles species, indicating an increasingly warm and dry climate, while those recovered below and above the excursion reflect a cooler and wetter climate. The record of a transient warming event (hyperthermal) in the early Danian at Boltysh has strong similarities with the Dan-C2 hyperthermal event recorded in marine sediments in Tethys and the Atlantic Ocean, and suggests that there were profound environmental changes occurring on a global scale shortly after the K-Pg boundary.

AB - Carbon isotope and palynological analysis of the fine-grained organic carbon-rich lacustrine sediments that filled the Cretaceous-Paleogene (K-Pg) boundary-age Boltysh impact crater (Ukraine) preserve a uniquely complete and detailed record of a negative carbon isotope excursion in an expanded section of the early Danian that we estimate lasted as long as similar to 340 k.y. Palynological assemblages recovered through the excursion reflect the increasing dominance of thermophylic Normapolles species, indicating an increasingly warm and dry climate, while those recovered below and above the excursion reflect a cooler and wetter climate. The record of a transient warming event (hyperthermal) in the early Danian at Boltysh has strong similarities with the Dan-C2 hyperthermal event recorded in marine sediments in Tethys and the Atlantic Ocean, and suggests that there were profound environmental changes occurring on a global scale shortly after the K-Pg boundary.

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