d18O compostion from conodont apatite indicates climate cooling during the Middle Pridoli

Zigaite Z, Joachimski M, Lehnert O, Brazauskas A (2010)

Publication Type: Journal article, Original article

Publication year: 2010

Journal

Palaeogeography, Palaeoclimatology, Palaeoecology Elsevier

Publisher: Elsevier

Book Volume: 294

Pages Range: 242-247

DOI: 10.1016/j.palaeo.2010.03.033

Authors with CRIS profile

Michael Joachimski Lehrstuhl für Geologie (Exogene Dynamik) Oliver Lehnert Lehrstuhl für Geologie (Exogene Dynamik)

Involved external institutions

LILLE 1 University - Science and Technology FR France (FR) Vilnius University / Vilniaus universitetas LT Lithuania (LT)

How to cite

APA:

Zigaite, Z., Joachimski, M., Lehnert, O., & Brazauskas, A. (2010). d18O compostion from conodont apatite indicates climate cooling during the Middle Pridoli. Palaeogeography, Palaeoclimatology, Palaeoecology, 294, 242-247. https://doi.org/10.1016/j.palaeo.2010.03.033

MLA:

Zigaite, Zivile, et al. "d18O compostion from conodont apatite indicates climate cooling during the Middle Pridoli." Palaeogeography, Palaeoclimatology, Palaeoecology 294 (2010): 242-247.

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