Minor element ratios of Globorotalia tumida and subsurface temperature reconstruction for IODP Site 321-U1338
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| Format: | Dataset Open Access |
| Sprache: | en |
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2018
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| _version_ | 1867169123850518528 |
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| author | Ford, Heather L Ravelo, Ana Christina Ramirez, Briana Akers, Taylor Krzeminski, Olivia |
| author_facet | Ford, Heather L Ravelo, Ana Christina Ramirez, Briana Akers, Taylor Krzeminski, Olivia |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The equatorial Pacific thermocline is a critical component in determining the ocean-atmosphere interactions of the tropics. During the Pliocene warm period, the tropical thermocline was warm and/or deep and shoaled toward present day. Here we use Mg/Ca values of subsurface-dwelling Globorotalia tumida to reconstruct subsurface temperatures at Integrated Ocean Drilling Program, JOIDES Resolution, Expedition 320/321, Pacific Equatorial Age Transect, Site U1338. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_884538 |
| institution | PANGAEA |
| language | en |
| publishDate | 2018 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Minor element ratios of Globorotalia tumida and subsurface temperature reconstruction for IODP Site 321-U1338 Ford, Heather L Ravelo, Ana Christina Ramirez, Briana Akers, Taylor Krzeminski, Olivia 321-U1338; AGE; Calcium; Calculated from Mg/Ca ratios (Mohtadi et al. 2011); COMPCORE; Composite Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DSDP/ODP/IODP sample designation; Exp321; Globorotalia tumida, Magnesium/Calcium ratio; Globorotalia tumida, Manganese/Calcium ratio; Globorotalia tumida, Strontium/Calcium ratio; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Pacific Equatorial Age Transect II / Juan de Fuca; Sample code/label; Sub-surface temperature The equatorial Pacific thermocline is a critical component in determining the ocean-atmosphere interactions of the tropics. During the Pliocene warm period, the tropical thermocline was warm and/or deep and shoaled toward present day. Here we use Mg/Ca values of subsurface-dwelling Globorotalia tumida to reconstruct subsurface temperatures at Integrated Ocean Drilling Program, JOIDES Resolution, Expedition 320/321, Pacific Equatorial Age Transect, Site U1338. |
| title | Minor element ratios of Globorotalia tumida and subsurface temperature reconstruction for IODP Site 321-U1338 |
| topic | 321-U1338; AGE; Calcium; Calculated from Mg/Ca ratios (Mohtadi et al. 2011); COMPCORE; Composite Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DSDP/ODP/IODP sample designation; Exp321; Globorotalia tumida, Magnesium/Calcium ratio; Globorotalia tumida, Manganese/Calcium ratio; Globorotalia tumida, Strontium/Calcium ratio; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Pacific Equatorial Age Transect II / Juan de Fuca; Sample code/label; Sub-surface temperature |
| url | https://doi.org/10.1594/PANGAEA.884538 |