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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2022
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| Accesso online: | https://doi.org/10.1594/PANGAEA.951458 |
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| _version_ | 1867167681108508672 |
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| author | Voelker, Antje H L Rodrigues, Teresa Trotta, Samanta Marino, Maria Kuhnert, Henning |
| author_facet | Voelker, Antje H L Rodrigues, Teresa Trotta, Samanta Marino, Maria Kuhnert, Henning |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | To better understand interglacial climate variability within the 41 kyr world, we produced centennial-scale climate records for the interval from Marine Isotope Stage (MIS) 46 to MIS 49, with particular focus on interglacial MIS 47 (1424-1452 ka) at IODP Site U1387 (36°48'N, 7°43'W) on the southern Portuguese margin. The reconstructions are based on benthic foraminifera (Cibicidoides pachyderma, Planulina ariminensis) and planktonic foraminifera (G. bulloides, G. ruber white) stable isotope records, Uk'37 sea-surface temperatures (SST), plankton foraminifera assemblage data, and the nannofossil warm water taxa percentage. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_951458 |
| institution | PANGAEA |
| language | en |
| publishDate | 2022 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Paleoclimate records for Marine Isotope Stage 46 to 49 (1407-1476 ka) from IODP Site U1387, southern Portuguese margin Voelker, Antje H L Rodrigues, Teresa Trotta, Samanta Marino, Maria Kuhnert, Henning Benthic foraminiferal stable isotopes; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; nannofossil; Planktic foraminifera assemblage; Portuguese Margin; Sea surface temperature To better understand interglacial climate variability within the 41 kyr world, we produced centennial-scale climate records for the interval from Marine Isotope Stage (MIS) 46 to MIS 49, with particular focus on interglacial MIS 47 (1424-1452 ka) at IODP Site U1387 (36°48'N, 7°43'W) on the southern Portuguese margin. The reconstructions are based on benthic foraminifera (Cibicidoides pachyderma, Planulina ariminensis) and planktonic foraminifera (G. bulloides, G. ruber white) stable isotope records, Uk'37 sea-surface temperatures (SST), plankton foraminifera assemblage data, and the nannofossil warm water taxa percentage. |
| title | Paleoclimate records for Marine Isotope Stage 46 to 49 (1407-1476 ka) from IODP Site U1387, southern Portuguese margin |
| topic | Benthic foraminiferal stable isotopes; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; nannofossil; Planktic foraminifera assemblage; Portuguese Margin; Sea surface temperature |
| url | https://doi.org/10.1594/PANGAEA.951458 |