Add to ORKGChanges in the oxygen isotopic composition of the planktonic foraminifer Globigerinoides ruber and in the foraminifera faunal composition in a core retrieved from the southeastern Brazilian continental margin were used to infer past changes in the hydrological balance and monsoon precipitation in the western South Atlantic since the Last Glacial Maximum (LGM). The results suggest a first-order orbital (precessional) control on the South American Monsoon precipitation. This agrees with previous studies based on continental proxies except for LGM estimates provided by pollen records. The causes for this disagreement are discussed
Changes in the Brazilian continental margin`s oceanic productivity and circulation over the last 27,...
The western South Atlantic boundary currents represent a sensitive system within the global thermoha...
O objetivo da presente tese é o de documentar, em escala milenar, as variações paleoclimáticas e pal...
Changes in the oxygen isotopic composition of the planktonic foraminifer Globigerinoides ruber and i...
This study explores the mechanisms behind the high glacial productivity in the southern Brazilian ma...
Marine productivity largely controls the oceanic uptake of atmospheric carbon dioxide and contribute...
Reconstructions of surface paleoceanographic conditions of the western tropical Atlantic and past cl...
In this paper we present a paleoceanographic reconstruction of the southwestern South Atlantic for t...
The stable isotope composition of planktonic foraminifera correlates with evidence for pulses of ter...
Today the western tropical Atlantic is the most important passage for cross-equatorial transfer of h...
This work reconstructs Late Quaternary paleoceanographic changes in the western South Atlantic Ocean...
The central problem of late Quaternary circulation in the South Atlantic is its role in transfer of ...
Detailed 14C AMS data and isotope based stratigraphies from high-resolution paleoceanographic record...
Few studies have focused on past hydroclimatic changes in the tropical coastal regions of eastern So...
The North Brazil Current in the western equatorial Atlantic is the main route for poleward heat tran...
Changes in the Brazilian continental margin`s oceanic productivity and circulation over the last 27,...
The western South Atlantic boundary currents represent a sensitive system within the global thermoha...
O objetivo da presente tese é o de documentar, em escala milenar, as variações paleoclimáticas e pal...
Changes in the oxygen isotopic composition of the planktonic foraminifer Globigerinoides ruber and i...
This study explores the mechanisms behind the high glacial productivity in the southern Brazilian ma...
Marine productivity largely controls the oceanic uptake of atmospheric carbon dioxide and contribute...
Reconstructions of surface paleoceanographic conditions of the western tropical Atlantic and past cl...
In this paper we present a paleoceanographic reconstruction of the southwestern South Atlantic for t...
The stable isotope composition of planktonic foraminifera correlates with evidence for pulses of ter...
Today the western tropical Atlantic is the most important passage for cross-equatorial transfer of h...
This work reconstructs Late Quaternary paleoceanographic changes in the western South Atlantic Ocean...
The central problem of late Quaternary circulation in the South Atlantic is its role in transfer of ...
Detailed 14C AMS data and isotope based stratigraphies from high-resolution paleoceanographic record...
Few studies have focused on past hydroclimatic changes in the tropical coastal regions of eastern So...
The North Brazil Current in the western equatorial Atlantic is the main route for poleward heat tran...
Changes in the Brazilian continental margin`s oceanic productivity and circulation over the last 27,...
The western South Atlantic boundary currents represent a sensitive system within the global thermoha...
O objetivo da presente tese é o de documentar, em escala milenar, as variações paleoclimáticas e pal...