Abstract
This dataset includes baseline stable carbon and oxygen isotope measurements from benthic foraminifera throughout the Gulf of Mexico. Stable isotope measurements were performed on Cibicidoides spp. The dataset contains the sediment core information such as location, date, and depth; and benthic foraminiferal stable carbon and oxygen isotopes. Sediment cores were collected on multiple cruises from 2010-06-13 to 2017-07-19.
Purpose
The purpose of this dataset was to provide Gulf of Mexico-wide baseline measurements of benthic foraminifera stable isotope in advance of future oil spills. These baseline measurements can be used in the event of future oil spills as a reference to quantitatively assess impact and recovery. They also have implications for the calibration and development of paleoceanographic proxies.
Keywords
stable isotopes, C13, O18, baseline, benthic foraminifera, sediment cores
UDI
R6.x805.000:0006
Date
10-26-2018
Point of Contact
Schwing, Patrick
University of South Florida
College of Marine Science
140 7th Ave South
St. Petersburg , FL 33701
USA
pschwing@mail.usf.edu
Funding Source
RFP-VI
Start of Data Collection
June 2010
End of Data Collection
July 2017
DOI
https://doi.org/10.7266/n7-repn-q515
Rights Information
This work is licensed under a
Creative Commons Public Domain Dedication 1.0 License.
Scholar Commons Citation
Schwing, Patrick and Hollander, David J., "Gulf-wide seafloor surface benthic foraminifera stable isotopes from sediment cores collected on multiple cruises from 2010-06-13 to 2017-07-19" (2018). C-IMAGE data. 66.
https://digitalcommons.usf.edu/cimage_data/66
Comments
Data and metadata is made available by the Gulf of Mexico Research Initiative Information and Data Cooperative (GRIIDC) through a CC0 license in compliance with the Gulf of Mexico Research Initiative (GoMRI). The original dataset landing pages may be accessed at GRIIDC’s dataset monitoring webpage.
Data users are encouraged to contact the originating investigator prior to data use and provide appropriate credit.