Origin of δ13C minimum events in thermocline and intermediate waters of the western South Atlantic
RA Nascimento, TP Santos, IM Venancio… - Quaternary Science …, 2021 - Elsevier
Stable carbon isotopic (δ 13 C) minimum events have been widely described in marine
archives recording the properties of thermocline and intermediate waters during glacial …
archives recording the properties of thermocline and intermediate waters during glacial …
ENSO-like evolution of the tropical Pacific climate mean state and its potential causes since 300ka
Abstract The tropical Pacific Ocean plays a significant role in climate change, and the El
Niño-Southern Oscillation (ENSO) is considered to be closely related to extreme climate …
Niño-Southern Oscillation (ENSO) is considered to be closely related to extreme climate …
Thermodynamic air-sea equilibration controls carbon isotopic composition of the South Atlantic thermocline during the last glacial period
Negative stable carbon isotope (δ 13 C) excursions in the marine upper water column have
been related to the release of aged oceanic CO 2 to the atmosphere during millennial-scale …
been related to the release of aged oceanic CO 2 to the atmosphere during millennial-scale …
[HTML][HTML] No detectable influence of the carbonate ion effect on changes in stable carbon isotope ratios (C) of shallow dwelling planktic foraminifera over the past …
P Köhler, S Mulitza - Climate of the Past, 2024 - cp.copernicus.org
Laboratory experiments showed that the isotopic fractionation of δ 13 C and of δ 18 O during
calcite formation of planktic foraminifera are species-specific functions of ambient CO 3 2 …
calcite formation of planktic foraminifera are species-specific functions of ambient CO 3 2 …
No detectable influence of the carbonate ion effect on changes in stable carbon isotope ratios (δ13C) of shallow dwelling planktic foraminifera over the past 160 kyr
P Köhler, S Mulitza - Climate of the Past Discussions, 2023 - cp.copernicus.org
Laboratory experiments showed that the isotopic fractionation of δ 13 C and of δ 18 O during
calcite formation of planktic foraminifera are species-specific functions of oceanic CO 3 2 …
calcite formation of planktic foraminifera are species-specific functions of oceanic CO 3 2 …
Improving Paleoclimate Reconstructions using Models and Observations of Foraminifera
DE Gaskell - 2022 - search.proquest.com
This study investigates the biological and morphological factors controlling carbon and
oxygen stable isotope fractionation in foraminifera (δ 13 C and δ 18 O) and uses these …
oxygen stable isotope fractionation in foraminifera (δ 13 C and δ 18 O) and uses these …