Carbon and oxygen isotope fractionation in scleractinian corals: a review

1983 ◽  
Vol 19 (1) ◽  
pp. 51-80 ◽  
Author(s):  
Peter K. Swart
2008 ◽  
Vol 72 (19) ◽  
pp. 4687-4698 ◽  
Author(s):  
Erin F. Owen ◽  
Alan D. Wanamaker ◽  
Scott C. Feindel ◽  
Bernd R. Schöne ◽  
Paul D. Rawson

2013 ◽  
Vol 103 ◽  
pp. 232-244 ◽  
Author(s):  
Dana F.C. Riechelmann ◽  
Michael Deininger ◽  
Denis Scholz ◽  
Sylvia Riechelmann ◽  
Andrea Schröder-Ritzrau ◽  
...  

2021 ◽  
Author(s):  
Yuan jie

Abstract Based on thermodynamic equilibrium isotope fractionation theory, this letter reasonably understands the clumping 13C-18O (Δ47 ), as well as carbon and oxygen isotope fractionation in calcites with extremely slow-growing rates from Devils Hole and Laghetto Basso (Corchia Cave) at atomic level with solid physical precipitation models and quantum-mechanical backgrounds. It is found that most calcites in nature precipitate in at equilibrium.


1984 ◽  
Vol 277 ◽  
pp. 581 ◽  
Author(s):  
W. D. Langer ◽  
T. E. Graedel ◽  
M. A. Frerking ◽  
P. B. Armentrout

2018 ◽  
Vol 235 ◽  
pp. 127-139 ◽  
Author(s):  
Jens Fohlmeister ◽  
Jennifer Arps ◽  
Christoph Spötl ◽  
Andrea Schröder-Ritzrau ◽  
Birgit Plessen ◽  
...  

2013 ◽  
Vol 40 (2) ◽  
pp. 145-152 ◽  
Author(s):  
Barbara Sensuła ◽  
Anna Pazdur

Abstract We present the first analysis of the influence of climate change on carbon and oxygen isotope fractionation factors for two saccharides (glucose and α-cellulose) of pine wood. The conifers grew in the Niepołomice Forest in Poland and the annual rings covered a time span from 1935 to 2000 AD. Glucose samples from acid hydrolysis of α-cellulose were extracted from annual tree rings. The carbon and oxygen isotope fractionation factors between glucose and α-cellulose were not stable over time. The mean value for the carbon isotope fractionation factors between glucose and α-cellulose was greater than unity. The mean value for the oxygen isotope fractionation factors between glucose and α-cellulose was lower than unity. We established, with respect to climate change, the significance of the interannual and intraannual variation in the carbon and oxygen isotope fractionation factors between both saccharides. We used moving interval correlation results for May of the previous year through September of the current year using a base length of 48 years. The relationship with summer temperature is the main climate signal in the carbon isotope fractionation factor between glucose and α-cellulose. The relationship with autumn sunshine is the main climate signal in the oxygen isotope fractionation factor between glucose and α-cellulose for the tree ring chronology.


Sign in / Sign up

Export Citation Format

Share Document