Abstract The Medieval Climate Anomaly (MCA) is a climatic perturbation with a core period
of 1000-1200 AD that is well-recognized in the Northern Hemisphere (NH). Its existence in …

Lipid-biomarkers have been used to reconstruct environmental changes in lacustrine
systems on a range of time scales. Lake sediments are excellent archives to apply these …

Brazilian shellmounds are archaeological sites with a high concentration of marine faunal
remains. There are more than 2000 sites along the coast of Brazil that range in age from …

The Brazil Current (BC) is a relevant feature in the Atlantic Meridional Overturning
Circulation (AMOC). Its behavior during slowdown or intense AMOC remains poorly known …

Marine productivity largely controls the oceanic uptake of atmospheric carbon dioxide and
contributed to the global climate changes that led to the termination of the last glacial cycle …

The last glacial inception was characterised by rapid changes in temperature, atmospheric
pCO2, and changes in the water mass geometry of the major ocean basins. Although …

Western boundary upwelling systems such as those found in the southeastern Brazilian
margin (SBM) are promoted by special atmospheric and oceanographic interactions with …

The Paraiba do Sul River delta, a South America east coast system, presents deposits
recording complex sedimentary dynamics in the deltaic plain during the Little Ice Age (LIA) …

The distribution of planktonic foraminifera in box-core tops under the influence of a western
boundary upwelling system along the southeastern Brazilian continental margin was …

We present a multi-year record of shell fluxes and δ 18 O of six planktonic foraminifera
species (Globigerinoides ruber pink, Globigerinoides ruber white, Trilobatus sacculifer …