Dataset: Magnesium isotopic ratios from ocean acidification experiments
View Data: Data not available yet
Data Citation:
Eagle, R., Ries, J. B., Lotterhos, K., Alvarez Caraveo, B., Guillermic, M., Downey-Wall, A. (2025) Magnesium isotopic compositions of seawater, extrapallial fluid, and Crassostrea virginica shell material from ocean acidification experiments. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2025-03-01 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/955164 [access date]
Terms of Use
This dataset is licensed under Creative Commons Attribution 4.0.
If you wish to use this dataset, it is highly recommended that you contact the original principal investigators (PI). Should the relevant PI be unavailable, please contact BCO-DMO (info@bco-dmo.org) for additional guidance. For general guidance please see the BCO-DMO Terms of Use document.
Principal Investigator:
Dr Robert Eagle (University of California-Los Angeles, UCLA)
Co-Principal Investigator:
Katie Lotterhos (Northeastern University)
Justin B. Ries (Northeastern University)
Scientist:
Blanca Alvarez Caraveo (University of California-Los Angeles, UCLA)
Alan Downey-Wall (Northeastern University)
Maxence Guillermic (University of California-Los Angeles, UCLA)
Student:
Jill Sutton (Universite de Brest)
BCO-DMO Data Manager:
Dana Stuart Gerlach (Woods Hole Oceanographic Institution, WHOI BCO-DMO)
Version:
1
Version Date:
2025-03-01
Restricted:
No
Validated:
No
Current State:
Preliminary and in progress
Magnesium isotopic compositions of seawater, extrapallial fluid, and Crassostrea virginica shell material from ocean acidification experiments
Abstract:
The geochemistry of biogenic carbonates is an established proxy to record changing seawater parameters. However, the effect of ocean acidification on seawater chemistry and organism physiology may impact isotopic signatures and how elements are incorporated into carbonate shells. In this study, we investigated the geochemistry of three reservoirs important for biomineralization--seawater, the extrapallial fluid (EPF), and the shell. Ocean acidification laboratory experiments were conducted at [____place___] during [____time range___] to examine the effects of ambient, moderate, and high ocean acidification conditions on the geochemistry of the biomineralization reservoirs. Here we present magnesium isotope data for seawater, EPF, and Crassostrea virginica shells.