Oxygen isotope composition of the surface water (calculated from the oxygen isotope composition of and planktonic foraminifera (Globigerinoides ruber white) and UK'37-based sea surface temperature) and ice volume-corrected oxygen isotope composition of the surface water from marine sediment core SO 188-17286-1 (Bay of Bengal, 19°44.58′N, 89°52.76′E, 1428 m water depth) for the last ~130 kyr
The Mediterranean Sea is characterized by a relatively strong west to east salinity gradient, which ...
We obtained Core KX97322-4 (00°01.73′S, 159°14.66′E, 2362 m) from the Ontong Java Plateau in the cen...
We review the different sources of uncertainty affecting the oxygen isotopic composition of plankton...
Oxygen isotope measurements have been made in foraminifera from over 60 deep-sea sediment cores. Tak...
Paleotemperature curves were drawn from oxygen-isotope ratios in CaCO3 of planktonic foraminiferal t...
Stable oxygen isotopes measured on planktonic foraminifera Neogloboquadrina pachyderma
Stable oxygen isotopes for the cores JC138-27GC, JC138-28GC, JC138-29GC, JC138-38GC, JC138-49GC and ...
Stable oxygen isotopes measured on planktonic foraminifera Neogloboquadrina pachyderma
Oxygen isotopic analysis of planktic foraminifera (Globigerina bulloides) from a total of 23 surface...
We present here, for the first time, comprehensive depth specific (near surface to 1800 m) oxygen is...
This study presents osmium (Os) isotope and elemental data for cleaned planktic foraminifera, authig...
The application of stable oxygen isotopic ratio of surface dwelling Globigerinoides ruber (white var...
Measurement of the triple oxygen isotope (TOI) composition of O₂ is an established method for quant...
Ice volume corrected subsurface water oxygen isotope in the Solomon Sea during the past 568-kyr for ...
Oxygen and hydrogen isotopic ratio samples were collected from sea ice and water samples. Coring and...
The Mediterranean Sea is characterized by a relatively strong west to east salinity gradient, which ...
We obtained Core KX97322-4 (00°01.73′S, 159°14.66′E, 2362 m) from the Ontong Java Plateau in the cen...
We review the different sources of uncertainty affecting the oxygen isotopic composition of plankton...
Oxygen isotope measurements have been made in foraminifera from over 60 deep-sea sediment cores. Tak...
Paleotemperature curves were drawn from oxygen-isotope ratios in CaCO3 of planktonic foraminiferal t...
Stable oxygen isotopes measured on planktonic foraminifera Neogloboquadrina pachyderma
Stable oxygen isotopes for the cores JC138-27GC, JC138-28GC, JC138-29GC, JC138-38GC, JC138-49GC and ...
Stable oxygen isotopes measured on planktonic foraminifera Neogloboquadrina pachyderma
Oxygen isotopic analysis of planktic foraminifera (Globigerina bulloides) from a total of 23 surface...
We present here, for the first time, comprehensive depth specific (near surface to 1800 m) oxygen is...
This study presents osmium (Os) isotope and elemental data for cleaned planktic foraminifera, authig...
The application of stable oxygen isotopic ratio of surface dwelling Globigerinoides ruber (white var...
Measurement of the triple oxygen isotope (TOI) composition of O₂ is an established method for quant...
Ice volume corrected subsurface water oxygen isotope in the Solomon Sea during the past 568-kyr for ...
Oxygen and hydrogen isotopic ratio samples were collected from sea ice and water samples. Coring and...
The Mediterranean Sea is characterized by a relatively strong west to east salinity gradient, which ...
We obtained Core KX97322-4 (00°01.73′S, 159°14.66′E, 2362 m) from the Ontong Java Plateau in the cen...
We review the different sources of uncertainty affecting the oxygen isotopic composition of plankton...