-
(Table 3) Relative depth and age, CaCO3, δ¹⁸O, δ¹³C and Sr/Ca analysis from O...
Interpretations of calcite strontium/calcium records in terms of ocean history and calcite diagenesis require distinguishing the effects on deep-sea calcite sediments of changes... -
Benthic foraminifera stable isotope data for the Mossy Grove sediment core
Sample preparation for benthic foraminiferal stable-isotope analyses: Sediment amples were prepared and analyzed at Kochi University. Samples were washed through a 63 μm screen... -
Gas properties in ice core #23 from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Gas properties at core depth 1.95 m in ice cores from Larsen blue ice area, E...
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Ice properties at core depth 1.95 m in ice cores from Larsen blue ice area, E...
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Properties of ice core #23 from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Ice surface measurements from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
CO2 in ice cores at core depth 1.95 m from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
CO2 in ice core #23 from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
South Pacific Convergence Zone (SPCZ) d2Hdinosterol and calculated precipitat...
South Pacific Convergence Zone (SPCZ) d2Hdinosterol and calculated precipitation values (where appropriate) from Lac Lanutavake (duplicate cores UC1 and UC4), Lac Lalolalo... -
Size-fraction-specific stable oxygen isotope variations in ODP Site 198-1209
This dataset has no description
-
Size-fraction-specific stable carbon isotope variations in ODP Site 198-1209
This dataset has no description
-
Stable isotope record of benthic foraminifera of sediment core M125-73-3
This dataset has no description
-
Stable carbon and oxygen isotope measurements of Cibicidoides wuellerstorfi a...
This dataset has no description
-
Oxygen isotopic composition (δ18O) of planktonic foraminifera Globorotalia tr...
This dataset has no description
-
Oxygen isotopic composition (δ18O) of planktonic foraminifera Globigerinoides...
This dataset has no description
-
Oxygen isotopic composition (δ18O) of benthic foraminifera Cibicides sp. from...
This dataset has no description
-
Globorotalia inflata oxygen isotopic composition (δ18O) from subtropical west...
This dataset has no description
-
AMS radiocarbon ages of organic microinclusions extracted from the ice-wedge ...
In 1985, samples were taken from the exposure located at +48 m a.s.l. (44 m above the river water level). In 1999, samples were taken in the upper part of the Duvanny Yar... -
δ¹⁸O values in the ice wedge from the Adventdalen valley, Svalbard
The oxygen stable isotope analysis was carried out in the Stable Isotope Laboratory of the Geography Department at Lomonosov Moscow State University, using a Delta-V mass...
