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Postimpact earliest Paleogene warming shown by fish debris oxygen isotopes (El Kef, Tunisia)

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Science  29 Jun 2018:
Vol. 360, Issue 6396, pp. 1467-1469
DOI: 10.1126/science.aap8525

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vol. 360 no. 6396 1467-1469

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History: 
  • Received for publication September 1, 2017
  • Accepted for publication May 10, 2018

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  1. K. G. MacLeod1,*,
  2. P. C. Quinton2,
  3. J. Sepúlveda3,
  4. M. H. Negra4
  1. 1Department of Geological Sciences, University of Missouri, Columbia, MO, USA.
  2. 2Department of Geology, SUNY Potsdam, Potsdam, NY, USA.
  3. 3Department of Geological Sciences and Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO, USA.
  4. 4Department of Geology, Faculty of Sciences of Tunis, University of Tunis El Manar, 2092 Manar II, Tunis, Tunisia.
  1. *Corresponding author. Email: macleodk{at}missouri.edu

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