Geochemistry of ostracode calcite: Part 1. An experimental determination of oxygen isotope fractionation

1997 ◽  
Vol 61 (2) ◽  
pp. 377-382 ◽  
Author(s):  
J. Xia ◽  
E. Ito ◽  
D.R. Engstrom
Keyword(s):  
Experimental Determination ◽  
Oxygen Isotope ◽  
Isotope Fractionation ◽  
Oxygen Isotope Fractionation

Oxygen isotope fractionation between zircon and water: experimental determination and comparison with quartz-zircon calibrations

2002 ◽  
Vol 14 (4) ◽  
pp. 849-853 ◽  
Author(s):  
Dmitry P. Krylov ◽  
Vasilij N. Zagnitko ◽  
Stephan Hoernes ◽  
Irina P. Lugovaja ◽  
Radegund Hoffbauer
Keyword(s):  
Experimental Determination ◽  
Oxygen Isotope ◽  
Isotope Fractionation ◽  
Oxygen Isotope Fractionation

scholarly journals Experimental determination of the temperature dependence of oxygen-isotope fractionation between water and chitinous head capsules of chironomid larvae

2021 ◽  
Author(s):  
Alex Lombino ◽  
Tim Atkinson ◽  
Stephen J. Brooks ◽  
Darren R. Gröcke ◽  
Jonathan Holmes ◽  
...  
Keyword(s):  
Temperature Dependence ◽  
Oxygen Isotope ◽  
Oxygen Isotopes ◽  
Isotope Fractionation ◽  
Temperature Dependent ◽  
Oxygen Isotope Fractionation ◽  
Chironomid Larvae ◽  
Increasing Temperature ◽  
The Relationship

AbstractOxygen-isotope values of invertebrate cuticle preserved in lake sediments have been used in palaeoenvironmental reconstructions, generally with the assumption that fractionation of oxygen isotopes between cuticle and water ($$\upalpha_{\text{cuticle}-\text{H}_{2}\text{O}}$$ α cuticle - H 2 O ) is independent of temperature. We cultured chironomid larvae in the laboratory with labelled oxygen-isotope water and across a range of closely controlled temperatures from 5 to 25 °C in order to test the hypothesis that fractionation of oxygen isotopes between chironomid head capsules and water ($$\upalpha_{\text{chironomid}-\text{H}_{2}\text{O}}$$ α chironomid - H 2 O ) is independent of temperature. Results indicate that the hypothesis can be rejected, and that $$\upalpha_{\text{chironomid}-\text{H}_{2}\text{O}}$$ α chironomid - H 2 O decreases with increasing temperature. The scatter in the data suggests that further experiments are needed to verify the relationship. However, these results indicate that temperature-dependence of $$\upalpha_{\text{chironomid}-\text{H}_{2}\text{O}}$$ α chironomid - H 2 O should be considered when chironomid δ18O is used as a paleoenvironmental proxy, especially in cases where data from chironomids are combined with oxygen-isotope values from other materials for which fractionation is temperature dependent, such as calcite, in order to derive reconstructions of past water temperature.

An experimental and theoretical determination of oxygen isotope fractionation in the system magnetite-H2O from 300 to 800°C

2004 ◽  
Vol 68 (17) ◽  
pp. 3569-3585 ◽  
Author(s):  
David R. Cole ◽  
Juske Horita ◽  
Veniamin B. Polyakov ◽  
John W. Valley ◽  
Michael J. Spicuzza ◽  
...  
Keyword(s):  
Oxygen Isotope ◽  
Isotope Fractionation ◽  
Theoretical Determination ◽  
Oxygen Isotope Fractionation
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