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Sources and distribution of organic matter and polycyclic aromatic hydrocarbons...

Total organic carbon (Corg), total nitrogen (Ntot), Corg/Ntot, δ13Corg, δ15N, calcium carbonate (CaCO3), and grain size were analyzed in 70 surface samples and 19 short cores from the southwestern Portuguese shelf. Perylene and USEPA-16 PAHs were quantified in a subset of these samples. The findings suggest that organic matter derives from a mix of terrestrial and marine sources, outlined by Corg, Ntot, and iso...

Millennial‐Scale Climate Variability Potentially Shaped the Early Interglacial ...

The seasonal and latitudinal distribution of insolation is considered the main factor controlling the magnitude and timing of interglacial periods. However, despite small differences in insolation forcing, vegetation and hydrology in southern Europe during past interglacials are variable and the gradual change in insolation cannot explain the observed short‐lived forest optimum. Here we focus on vegetation and ...

Combination of insolation and ice-sheet forcing drive enhanced humidity in nort...

Marine Isotope Stage (MIS) 13, similar to 533-478 ka, has received particular attention due to the unexpected enhancement of monsoon systems under a cool climate characterized by lower atmospheric CO2 and larger ice volume than many other interglacials. Key questions remain about its regional expression (intensity, climate variability, length), and underlying forcing factors, in particular at the mid-latitudes....

A new perspective of the Alboran Upwelling System reconstruction during the Mar...

A high-resolution study of the MIS 12/MIS 11 transition and the MIS 11 (430-376 kyr) coccolithophore assemblages at Ocean Drilling Program Site 977 was conducted to reconstruct the palaeoceanographic and climatic changes in the Alboran Sea from the variability in surface water conditions. The nannofossil record was integrated with the planktonic oxygen and carbon stable isotopes, as well as the U-37(k') Sea Sur...

Unexpected weak seasonal climate in the western Mediterranean region during MIS...

Marine Isotope Stage 31 (MIS 31) is an important analogue for ongoing and projected global warming, yet key questions remain about the regional signature of its extreme orbital forcing and intra-interglacial variability. Based on a new direct land-sea comparison in SW Iberian margin IODP Site U1385 we examine the climatic variability between 1100 and 1050 ka including the "super interglacial" MIS 31, a period d...

Past climate variability in the Iberian Margin during Marine Isotope Stages 15-...

Extreme glacial conditions in the Iberian Margin during MIS 12 and MIS 14

Climate changes in the Western Iberian Margin during Marine Isotope Stages 15-9...

Climate changes in the Western Iberian Margin during Marine Isotope Stages 15-9...

Sea surface temperature similarities during the present and past interglacials