-
CO2 data including revised ODP 122-761B ages
Data are from Rea et al. 2021 -
Revised splice record of ODP Site 184-1146
This dataset has no description
-
Elemental data of IODP Site 363-U1490
This dataset has no description
-
Stable isotope record of IODP Site 353-U1443
This dataset has no description
-
Stable isotope record on revised age model, ODP Hole 189-1171C
This dataset has no description
-
Stable isotope record on revised age model, ODP Site 202-1237
This dataset has no description
-
Stable isotope record on revised age model, ODP Site 202-1236
This dataset has no description
-
Stable isotope record on revised age model, ODP Hole 120-751A
This dataset has no description
-
Stable isotope record on revised age model ODP Hole 122-761B
This dataset has no description
-
Stable isotope record of ODP Site 184-1146
This dataset has no description
-
Age model of ODP Site 184-1146
This dataset has no description
-
Stable isotope record on revised age model, IODP Site U1338-U1337
This dataset has no description
-
Stable isotope offset C. mundulus - O. umbonatus, IODP Site 363-U1490
This dataset has no description
-
Stable isotope offset C. mundulus - Recuvigerina, IODP Site 363-U1490
This dataset has no description
-
Stable isotope record and coarse fraction content of IODP Site 363-U1490
This dataset has no description
-
Carbonate concent of IODP Site 363-U1490
This dataset has no description
-
Discrete bulk Spectro Xepos XRF data of Holocene lake sediments from Lake Sid...
The North African desert margin is considered one of the areas most sensitive to future climate changes. Improved knowledge about Holocene climatic variability and environmental... -
Calibrated high-resolution XRF core-scanning data of Holocene lake sediments ...
The North African desert margin is considered one of the areas most sensitive to future climate changes. Improved knowledge about Holocene climatic variability and environmental... -
Re-organization of Pacific overturning circulation across the Miocene Climate...
We reconstruct the evolution of deep-water chemistry across the Miocene Climate Optimum (16.9 to 14.7 Ma) and Middle Miocene Climate Transition (14.7-13.8 Ma), using... -
Pollen and non-pollen palynomorphs of the sediment core EN20001 from Lake Khamra
48 pollen samples from Lake Khamra were prepared using the established protocol with added Lycopodium marker spore tablets. To store samples and prepare microscopic slides,...
