Cardiff University | Prifysgol Caerdydd ORCA
Online Research @ Cardiff 
WelshClear Cookie - decide language by browser settings

The effect of seawater carbonate chemistry on the stable isotope composition of Cibicidoides wuellerstorfi and other Cibicidoides species

Nederbragt, Alexandra J. 2023. The effect of seawater carbonate chemistry on the stable isotope composition of Cibicidoides wuellerstorfi and other Cibicidoides species. Paleoceanography and Paleoclimatology 38 (9) , e2023PA004667. 10.1029/2023PA004667

[thumbnail of Nederbragt_Cibicidoides_isotopes accepted manuscript.pdf]
Preview
PDF - Accepted Post-Print Version
Download (1MB) | Preview

Abstract

The δ13C composition of Cibicidoides wuellerstorfi and other Cibicidoides spp is an important tool to reconstruct past changes in the deep ocean carbon cycle. The species are expected to match the δ13C of ambient dissolved inorganic carbon (DIC), although it has been recognized that substantial offsets can occur. Here, I present a compilation of modern δ13C and δ18O data for named Cibicidoides species in combination with fully resolved carbonate chemistry at each core location. The data show for C. wuellerstorfi that the offset from the expected value in both carbon (∆13C) and oxygen (∆18O) is correlated with seawater carbonate chemistry. The result is comparable to, but not identical with, published culture experiments in which marine organisms were grown under variable pH-conditions. Overall, ∆13C in C. wuellerstorfi correlates positively with carbonate saturation, [DIC], and temperature. The three variables together explain 47.1% of the variation in ∆13C. The trend for ∆18O is similar, except that the effect of temperature has been removed through correction with a published δ18O-temperature equation. Up to 35% of the remaining variation in ∆18O can be explained by ambient carbonate chemistry. Data for other named Cibicidoides species are broadly similar, but are too sparse for a detailed analysis. The results indicate that strongly negative ∆13C occurs predominantly in the deep Atlantic in response to a combination of low [DIC], low temperature, and undersaturation within the lysocline. Implications for paleoceanographic reconstructions are discussed.

Item Type: Article
Date Type: Publication
Status: Published
Schools: Earth and Environmental Sciences
Publisher: American Geophysical Union
ISSN: 2572-4517
Date of First Compliant Deposit: 25 September 2023
Date of Acceptance: 7 September 2023
Last Modified: 02 Dec 2024 04:00
URI: https://orca.cardiff.ac.uk/id/eprint/162715

Actions (repository staff only)

Edit Item Edit Item

Downloads

Downloads per month over past year

View more statistics