scholarly journals Contrasting shell growth strategies in two Mediterranean bivalves revealed by oxygen-isotope ratio geochemistry: The case of Pecten jacobaeus and Glycymeris pilosa

2019 ◽  
Vol 526 ◽  
pp. 23-35 ◽  
Author(s):  
Melita Peharda ◽  
Julien Thébault ◽  
Krešimir Markulin ◽  
Bernd R. Schöne ◽  
Ivica Janeković ◽  
...  
2018 ◽  
Vol 32 (9) ◽  
pp. 703-710 ◽  
Author(s):  
Steven J. Granger ◽  
Yuguo Yang ◽  
Verena Pfahler ◽  
Chris Hodgson ◽  
Andrew C. Smith ◽  
...  

1971 ◽  
Vol 26 (9) ◽  
pp. 1485-1490 ◽  
Author(s):  
K. Heinzinger ◽  
C. Iunge ◽  
M. Schidlowski

Abstract The separation factor, aM-0= (18O/16O) magnetite/' (18O/16O) atmospheric oxygen, between the magnetite crust of iron meteorites and atmospheric oxygen has been determined to be 0.9946 ± 0.0005. It is concluded that this fractionation of the oxygen isotopes is the consequence of an equilibrium isotope effect at high temperatures. It can be assumed that this is also valid for cosmic spherules, which are mainly ablation products of iron meteorites. As these spherules are found in sediments of different geological ages, their oxygen isotope ratio can give information on the development of atmospheric oxygen. The difference of the oxygen isotope ratios between magnetite from the lithosphere and airborne magnetite can be used to distinguish between terrestrial and extraterrestrial material.


2017 ◽  
Vol 217 (1) ◽  
pp. 105-116 ◽  
Author(s):  
Marco M. Lehmann ◽  
Gregory R. Goldsmith ◽  
Lola Schmid ◽  
Arthur Gessler ◽  
Matthias Saurer ◽  
...  

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