Determining the past record of temperature and salinity of ocean surface waters is essential for understanding past changes in climate, such as those which occur across glacial-interglacial transitions. As a useful proxy, the oxygen isotope composition (
Reconstructing past ocean salinity is important for assessing paleoceanographic change and therefore...
International audienceOver the last decades, sea surface temperature (SST) reconstructions based on ...
A combination of stable isotope records and Mg/Ca temperature estimates of four different planktonic...
Determining the past record of temperature and salinity of ocean surface waters is essential for und...
Seasonal changes in surface ocean temperature are increasingly recognized as an important parameter ...
Paleotemperature curves were drawn from oxygen-isotope ratios in CaCO3 of planktonic foraminiferal t...
Mg/Ca and stable oxygen isotope compositions (d18O) of planktic foraminifera tests are commonly used...
Abstract. Reconstruction of past salinities in surface oceans (SSS) can be done by measuring the iso...
Paleotemperature curves were drawn from oxygen-isotope ratios in CaCO3 of planktonic foraminiferal t...
International audienceTo overcome the lack of long-term instrumental records, paleo-reconstructions ...
International audienceTo overcome the lack of long-term instrumental records, paleo-reconstructions ...
This dataset contains surface (Globigerninodes ruber) and subsurface (Pulleniatina obliquiloculata) ...
Reconstructing past ocean salinity is important for assessing paleoceanographic change and therefore...
International audienceOver the last decades, sea surface temperature (SST) reconstructions based on ...
A combination of stable isotope records and Mg/Ca temperature estimates of four different planktonic...
Determining the past record of temperature and salinity of ocean surface waters is essential for und...
Seasonal changes in surface ocean temperature are increasingly recognized as an important parameter ...
Paleotemperature curves were drawn from oxygen-isotope ratios in CaCO3 of planktonic foraminiferal t...
Mg/Ca and stable oxygen isotope compositions (d18O) of planktic foraminifera tests are commonly used...
Abstract. Reconstruction of past salinities in surface oceans (SSS) can be done by measuring the iso...
Paleotemperature curves were drawn from oxygen-isotope ratios in CaCO3 of planktonic foraminiferal t...
International audienceTo overcome the lack of long-term instrumental records, paleo-reconstructions ...
International audienceTo overcome the lack of long-term instrumental records, paleo-reconstructions ...
This dataset contains surface (Globigerninodes ruber) and subsurface (Pulleniatina obliquiloculata) ...
Reconstructing past ocean salinity is important for assessing paleoceanographic change and therefore...
International audienceOver the last decades, sea surface temperature (SST) reconstructions based on ...
A combination of stable isotope records and Mg/Ca temperature estimates of four different planktonic...