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Dissolved and soluble pore water trace metals (Mn, Fe, Co, Ni) from sediment ...
Physical and chemical trace metal speciation are important for our understanding of metal cycling and potential toxicity to marine life. Trace metals can have different... -
Dissolved and soluble pore water trace metals (Mn, Fe, Co, Ni) from sediment ...
Physical and chemical trace metal speciation are important for our understanding of metal cycling and potential toxicity to marine life. Trace metals can have different... -
Dissolved and soluble pore water trace metals (Mn, Fe, Co, Ni) from sediment ...
Physical and chemical trace metal speciation are important for our understanding of metal cycling and potential toxicity to marine life. Trace metals can have different... -
Solid-phase manganese concentrations of surface sediments from sediment core ...
Surface sediments from the Clarion Clipperton Zone, central Pacific were analyzed for solid-phase Mn to assess potential Mn mobilization into the pore water from the solid phase... -
Diatom isotopes of ODP Site 145-887 (Table S2)
This dataset has no description
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Oxygen and carbon stable isotopes of Globobulimina spp. and Cibicidoides wuel...
This dataset has no description
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Oxygen and carbon stable isotopes of Globobulimina spp. and Cibicidoides wuel...
This dataset has no description
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Tropical Pacific late Cenozoic Iodine/Calcium from planktic foraminifera spec...
We apply the Iodine to Calcium (I/Ca) ratio in planktic foraminifera to reconstruct oceanic oxygen across the late Cenozoic. The data includes I/Ca ratios from planktic... -
Tropical Pacific late Cenozoic Iodine/Calcium from planktic foraminifera spec...
We apply the Iodine to Calcium (I/Ca) ratio in planktic foraminifera to reconstruct oceanic oxygen across the late Cenozoic. The data includes I/Ca ratios from planktic... -
Tropical Pacific late Cenozoic Iodine/Calcium from planktic foraminifera spec...
We apply the Iodine to Calcium (I/Ca) ratio in planktic foraminifera to reconstruct oceanic oxygen across the late Cenozoic. The data includes I/Ca ratios from planktic... -
Tropical Pacific late Cenozoic Iodine/Calcium from planktic foraminifera spec...
We apply the Iodine to Calcium (I/Ca) ratio in planktic foraminifera to reconstruct oceanic oxygen across the late Cenozoic. The data includes I/Ca ratios from planktic... -
High-resolution stable oxygen, carbon isotope and Magnesium/Calcium ratio dat...
This dataset lists the results of stable oxygen and carbon isotope measurements (in ‰ VPDB), and trace element analysis (Mg/Ca ratios in mmol mol-1) from Ocean Drilling Program... -
Biogeochemical and phospholipid-derived fatty acid (PLFA) composition of shal...
During R/V Sonne cruise SO254, we conducted ex-situ experiments with shallow- and deep-water demo- and hexactinellid sponges from New Zealand. Over a period of 5 hours, the... -
Carbon and nitrogen fluxes of shallow-water and deep-water demo- and hexactin...
During R/V Sonne cruise SO254, we conducted ex-situ experiments with shallow- and deep-water demo- and hexactinellid sponges from New Zealand. Over a period of 5 hours, the... -
Bacterial composition of shallow-water and deep-water demo- and hexactinellid...
During R/V Sonne cruise SO254, we conducted ex-situ experiments with shallow- and deep-water demo- and hexactinellid sponges from New Zealand. Over a period of 5 hours, the... -
A new helium isotope recored of the Paleocene-Eocene Thermal Maximum from ODP...
The Paleocene-Eocene Thermal Maximum (PETM; around 56 Ma ago) is arguably the most intensively studied event of rapid greenhouse warming of the geological past. The duration and... -
A new helium isotope recored of the Paleocene-Eocene Thermal Maximum from ODP...
The Paleocene-Eocene Thermal Maximum (PETM; around 56 Ma ago) is arguably the most intensively studied event of rapid greenhouse warming of the geological past. The duration and... -
A new helium isotope recored of the Paleocene-Eocene Thermal Maximum from ODP...
The Paleocene-Eocene Thermal Maximum (PETM; around 56 Ma ago) is arguably the most intensively studied event of rapid greenhouse warming of the geological past. The duration and... -
δ18O and δ13C of Cibicidoides wuellerstorfi and related species and carbonate...
The δ13C composition of Cibicidoides wuellerstorfi and other Cibicidoides spp is an important tool to reconstruct past changes in the deep ocean carbon cycle. The species are... -
Physical oceanography during RV SONNE cruise SO290 (PaläoTaNZ)
Data presented here were collected during the cruise SO290 (PaläoTaNZ) with RV Sonne from Nouméa, New Caledonia to Nouméa, New Caledonia (April, 11th, 2022 to May 12th, 2022)....
