Calibration and application of the ‘clumped isotope’ thermometer to foraminifera for high-resolution climate reconstructions

Grauel, A. L. and Schmid, Thomas W. and Hu, Bin and Bergami, Caterina and Capotondi, Lucilla and Zhou, Liping and Bernasconi, Stefano M. (2013) Calibration and application of the ‘clumped isotope’ thermometer to foraminifera for high-resolution climate reconstructions. Geochimica et Cosmochimica Acta, 108. pp. 125-140. DOI https://doi.org/10.1016/j.gca.2012.12.049

	PDF Grauel_et_al._-_2013_-_Calibration_and_application_of_the_‘clumped_isotop.pdf Restricted to Registered users only Download (1MB)
Preview	Image (JPEG) A_G_1-s2.0-S0016703713000380-gr1.jpg Download (77kB) | Preview

Abstract

The reconstruction of past ocean temperatures is fundamental to the study of past climate changes, therefore considerable effort has been invested in developing proxies for seawater temperatures. One of the most recent and promising new proxy is carbonate ‘clumped isotope’ thermometry, in particular because it is based on thermodynamic equilibrium and not on biogeochemical proxies. Here, we present a new calibration of the ‘clumped isotope’ thermometer to foraminifera based on seven species of planktic and benthic foraminifera spanning a growth temperature range of ∼2–28 °C. We used a newly developed technique for the measurements of small samples to improve the applicability of this method to paleoceanography. Our data have a comparable precision (∼0.005–0.013‰) and confirm previous calibration studies based on biogenic and inorganic calcite. We discuss possible sources of uncertainty such as over-/underestimation of the calcification temperatures, species-specific vital effects, pH variations between the seawater and the vacuole water of the species and possible kinetic effects on the ‘clumped isotope’ calibration. To validate our calibration study and test the applicability of our measuring technique to paleoclimate and paleoceanographic studies we measured the isotope composition of Globigerinoides ruber (white) at high-resolution in a sediment core covering the last 700 years in the Gulf of Taranto (Mediterranean Sea). The results show that it is necessary to average a relatively large number of analyses to achieve a consistent temperature signal for the detection of small sea surface temperature changes. Although with the current analytical system, ‘clumped isotope’ thermometry is only applicable to the analysis of relatively large SST changes in marine sediments, further technical improvements may make this a very powerful technique for paleoceanographic studies.

Item Type:	Article
Uncontrolled Keywords:	2013AREP; IA65;
Subjects:	01 - Climate Change and Earth-Ocean Atmosphere Systems
Divisions:	01 - Climate Change and Earth-Ocean Atmosphere Systems
Journal or Publication Title:	Geochimica et Cosmochimica Acta
Volume:	108
Page Range:	pp. 125-140
Identification Number:	https://doi.org/10.1016/j.gca.2012.12.049
Depositing User:	Sarah Humbert
Date Deposited:	25 May 2013 13:20
Last Modified:	23 Jul 2013 10:06
URI:	http://eprints.esc.cam.ac.uk/id/eprint/2790

Actions (login required)

View Item