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Particulate REE and Hf concentrations in surface sediment from RV Meteor crui...
All samples were obtained during RV Meteor cruise M147 (April–May 2018), conducted as the official process study GAPR11 within the framework of the international GEOTRACES program. -
Particulate Nd and Hf isotope compositions in surface sediment samples from R...
All samples were obtained during RV Meteor cruise M147 (April–May 2018), conducted as the official process study GAPR11 within the framework of the international GEOTRACES program. -
(Table 40-7) Speciations of chemical elements in bottom sediments from Core A...
Fractions of element occurrences: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 40-5) Speciations of chemical elements in bottom sediments from Core A...
Fractions of element occurrences: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 40-4) Speciations of chemical elements in bottom sediments from Core A...
Fractions of element occurrences: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 40-3) Speciations of chemical elements in bottom sediments from Core A...
Fractions of element occurrences: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 40-2) Speciations of chemical elements in bottom sediments from Core A...
Fractions of element occurrences: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 40-1) Speciations of chemical elements in bottom sediments from Core A...
Fractions of element occurrences: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 3a) Forms of chemical elements in bottom sediments from Core AMK7-756,...
Fractions (forms) of elements: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 3b) Forms of chemical elements in bottom sediments from Core AMK7-710
Fractions (forms) of elements: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 17) Composition of bitumen A in Black Sea sediments from DSDP Hole 42-379
This dataset has no description
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Seawater carbonate chemistry and Hydrozoa, Copepoda abundances and biomasses,...
Anthropogenic CO2 emissions cause a drop in seawater pH and shift the inorganic carbon speciation. Collectively, the term ocean acidification (OA) summarizes these changes. Few... -
(Table 2) Abundance of ostracods in surface sediment samples from the Admiral...
Sampling depth 0-15 cm. Each separate valve was counted as one specimen. Fragmented valves were not counted. -
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... -
Vertical day-night distribution of the salp Soestia zonaria in the temperate ...
Although the oceanic widespread pelagic tunicate Soestia zonaria has been studied for more than a century, little ecological information exists. Soestia primarily occurs in... -
Radium isotopes and 228Th in water column samples collected on POLARSTERN exp...
Radium isotopes are produced by decay of an isotope of thorium, a highly particle reactive element. Radium is relatively soluble in seawater such that once a thorium isotope in... -
Radium isotopes and 228Th in surface water samples collected on POLARSTERN ex...
228Ra is strongly enriched in shelf waters and its half-life (5.8 years) is well suited to study the fate of shelf-derived water in the central Arctic. During PS78 (TRANSARC I)... -
Pollen, spores and dinoflagellates of sediment core DP30PC from the Gulf of T...
This dataset has no description
