A 1.3 million-year benthic foraminiferal record at IODP Site U1391, Portuguese margin
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| Autori principali: | , , , |
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2020
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| _version_ | 1867170475642191872 |
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| author | Guo, Qimei Li, Baohua Voelker, Antje H L Kim, Jin Kyoung |
| author_facet | Guo, Qimei Li, Baohua Voelker, Antje H L Kim, Jin Kyoung |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Reconstruction of the Mediterranean Outflow Water (MOW) dynamics in the geologic past contributes to exploring its influence on the North Atlantic Ocean circulation and the climate. The middle Pleistocene transition (MPT) is one of the most important characteristics of Quaternary climate change, but until now, research on the MOW variability during this time interval has been limited. This work presents the first continuous and high-resolution (~2 kyr) foraminiferal stable oxygen and carbon isotopes and benthic foraminiferal records from Integrated Ocean Drilling Program (IODP) Site U1391, drilled off the Portuguese margin in the Northeast Atlantic Ocean, to decipher the MOW variability over the last 1.3 myr. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_923308 |
| institution | PANGAEA |
| language | en |
| publishDate | 2020 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | A 1.3 million-year benthic foraminiferal record at IODP Site U1391, Portuguese margin Guo, Qimei Li, Baohua Voelker, Antje H L Kim, Jin Kyoung Benthic foraminifera; IODP Site U1391; mid-Pleistocene transition; Stable isotopes Reconstruction of the Mediterranean Outflow Water (MOW) dynamics in the geologic past contributes to exploring its influence on the North Atlantic Ocean circulation and the climate. The middle Pleistocene transition (MPT) is one of the most important characteristics of Quaternary climate change, but until now, research on the MOW variability during this time interval has been limited. This work presents the first continuous and high-resolution (~2 kyr) foraminiferal stable oxygen and carbon isotopes and benthic foraminiferal records from Integrated Ocean Drilling Program (IODP) Site U1391, drilled off the Portuguese margin in the Northeast Atlantic Ocean, to decipher the MOW variability over the last 1.3 myr. |
| title | A 1.3 million-year benthic foraminiferal record at IODP Site U1391, Portuguese margin |
| topic | Benthic foraminifera; IODP Site U1391; mid-Pleistocene transition; Stable isotopes |
| url | https://doi.org/10.1594/PANGAEA.923308 |