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Grunert P, Tzanova A, Harzhauser M, et al. Mid-Burdigalian Paratethyan alkenone record reveals link between orbital forcing, Antarctic ice-sheet dynamics and European climate at the verge to Miocene Climate Optimum. Glob Planet Change. 2014;123:36-43doi: 10.1016/j.gloplacha.2014.10.011.
Grunert, P., Tzanova, A., Harzhauser, M., & Piller, W. E. (2014). Mid-Burdigalian Paratethyan alkenone record reveals link between orbital forcing, Antarctic ice-sheet dynamics and European climate at the verge to Miocene Climate Optimum. Global and planetary change, 12336-43. https://doi.org/10.1016/j.gloplacha.2014.10.011
Grunert, Patrick, et al. "Mid-Burdigalian Paratethyan alkenone record reveals link between orbital forcing, Antarctic ice-sheet dynamics and European climate at the verge to Miocene Climate Optimum." Global and planetary change vol. 123 (2014): 36-43. doi: https://doi.org/10.1016/j.gloplacha.2014.10.011
Grunert P, Tzanova A, Harzhauser M, Piller WE. Mid-Burdigalian Paratethyan alkenone record reveals link between orbital forcing, Antarctic ice-sheet dynamics and European climate at the verge to Miocene Climate Optimum. Glob Planet Change. 2014 Dec;123:36-43. doi: 10.1016/j.gloplacha.2014.10.011. PMID: 25844022; PMCID: PMC4375607.
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Glob Planet Change. 2014 Dec;123:36-43. doi: 10.1016/j.gloplacha.2014.10.011.

Mid-Burdigalian Paratethyan alkenone record reveals link between orbital forcing, Antarctic ice-sheet dynamics and European climate at the verge to Miocene Climate Optimum.

Global and planetary change

Patrick Grunert, Alexandrina Tzanova, Mathias Harzhauser, Werner E Piller

Affiliations

  1. Institute for Earth Sciences, University of Graz, NAWI Graz, Heinrichstraße 26, 8010 Graz, Austria.
  2. Department of Geological Sciences, Brown University, 324 Brook Street, Box 1846, Providence, RI 02912, USA.
  3. Geological-Paleontological Department, Natural History Museum Vienna, Burgring 7, 1030 Vienna, Austria.

PMID: 25844022 PMCID: PMC4375607 DOI: 10.1016/j.gloplacha.2014.10.011

Abstract

The Early Ottnangian Cooling (EOC), a distinct cold-spell in European climate at ~ 18 Ma preceding the Miocene Climate Optimum, is frequently reported in Paratethys records; however, the duration, magnitude, and underlying causes are poorly understood. A new palaeoclimatic data-set provides unexpected insights into this event. U

Keywords: Burdigalian; Early Ottnangian Cooling; Paratethys; alkenones; orbital forcing; palaeoclimate

References

  1. Science. 2001 Apr 13;292(5515):274-8 - PubMed
  2. Nature. 2006 Oct 12;443(7112):687-91 - PubMed
  3. Nat Commun. 2014;5:2999 - PubMed
  4. Science. 2001 Apr 27;292(5517):686-93 - PubMed
  5. Science. 2006 Dec 22;314(5807):1894-8 - PubMed
  6. Nature. 2008 Jan 17;451(7176):279-83 - PubMed

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Grant support