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Holocene evolution of sea-surface temperature and salinity in the Gulf of Mexico

Stable oxygen and carbon isotope composition (δ18O and δ13C) and magnesium-to-calcium (Mg/Ca) ratios were measured in the tests of planktic foraminiferal species, Globigerinoides ruber (white variety), in a northwestern Gulf of Mexico (GoM) sediment core 2010-GB2-GC1 collected from the Garrison Basin (26.67°N, 93.92°W) at a water depth of 1776 meters (m), aboard the R/V Cape Hatteras in April 2010. These measurements are used to generate sub-centennial-scale reconstructions of sea surface temperature (SST) and the stable oxygen isotope composition of seawater (δ18Osw; a proxy for changes in salinity) over the past 11,700 years. For further information regarding data collection and/or processing methods, refer to the associated journal article (Thirumalai and others, 2021).

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Author(s) Kaustubh Thirumalai, Julie N Richey orcid, Terrence M. Quinn, Caitlin E Reynolds
Publication Date 2021-05-07
Beginning Date of Data 2010-04-11
Ending Date of Data 2010-04-20
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DOI https://doi.org/10.5066/P9Q5L9VU
Citation Thirumalai, K., Richey, J.N., Quinn, T.M., and Reynolds, C.E., 2021, Holocene evolution of sea-surface temperature and salinity in the Gulf of Mexico: U.S. Geological Survey data release, https://doi.org/10.5066/P9Q5L9VU.
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Metadata Date 2021-09-22
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Loading https://doi.org/10.1029/2021PA004221

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License http://www.usa.gov/publicdomain/label/1.0/
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Harvest Source: Coastal and Marine Geoscience Data System
Harvest Date: 2025-01-07T07:20:07.907Z