Journal
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
Volume 11, Issue -, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2010GC003190
Keywords
Brachiopoda; carbon and oxygen isotopes; isotopic equilibrium; paleoenvironmental proxy; northwest subtropical Pacific
Categories
Funding
- Japan Society for the Promotion of Science [21340152]
- Tohoku University
- University of the Ryukyus
- Grants-in-Aid for Scientific Research [21340152] Funding Source: KAKEN
Ask authors/readers for more resources
This study examines the fidelity of carbon (delta C-13) and oxygen (delta O-18) isotope compositions of two modern brachiopod species (Kikaithyris hanzawai and Basiliola lucida) to use as proxies of delta C-13 values of total dissolved inorganic carbon and temperature and/or delta O-18 values of seawater, respectively. Well-preserved shells of K. hanzawai and living individuals of B. lucida were collected from a subtropical shelf environment off Amami-o-shima, southwestern Japan. Some portions of the shells are in isotopic equilibrium with the ambient seawater, while other portions are not. The degree of disequilibrium differs between the two species and between different portions of each shell. Statistically significant positive correlations are recognized between the delta C-13 and delta O-18 values of these samples, which can be ascribed to a kinetic fractionation effect. Far from the posterior shell edge and along the axis of shell growth, the delta O-18 values of the secondary shell layer of K. hanzawai mostly fall within the expected range of equilibrium calcite. The delta C-13 values from the inner surface of the secondary shell layer in both species are relatively constant and are equivalent to or very close to equilibrium calcite. Therefore, these portions of the shells are most suitable for collecting reliable environmental proxy data. Although the delta C-13 and delta O-18 values of modern brachiopod shells are predominantly controlled by a kinetic fractionation effect, the appropriate selection of species and shell portions that reflect the isotopic composition of ambient seawater can facilitate the reconstruction of secular variations in oceanic delta C-13 or delta O-18 values.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available