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

Journal article
(Original article)


Publication Details

Author(s): Zigaite Z, Joachimski M, Lehnert O, Brazauskas A
Journal: Palaeogeography, Palaeoclimatology, Palaeoecology
Publisher: Elsevier
Publication year: 2010
Volume: 294
Pages range: 242-247
ISSN: 0031-0182


FAU Authors / FAU Editors

Joachimski, Michael Prof. Dr.
Lehrstuhl für Geologie (Exogene Dynamik)
Lehnert, Oliver PD Dr.
Lehrstuhl für Geologie (Exogene Dynamik)


External institutions
LILLE 1 University - Science and Technology
Vilnius University / Vilniaus universitetas


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://dx.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.

BibTeX: 

Last updated on 2018-09-08 at 15:08