Paleoclimate records for Marine Isotope Stage 46 to 49 (1407-1476 ka) from IODP Site U1387, southern Portuguese margin

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...

Full description

Bibliographic Details
Main Authors: Voelker, Antje H L, Rodrigues, Teresa, Trotta, Samanta, Marino, Maria, Kuhnert, Henning
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
benthic foraminiferal stable isotopes
Integrated Ocean Drilling Program / International Ocean Discovery Program
IODP
nannofossil
planktic foraminifera assemblage
Portuguese Margin
Sea surface temperature
Planktonic foraminifera
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.951458
https://doi.org/10.1594/PANGAEA.951458
Description
Summary: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.

Similar Items