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Organic geochemistry of ODP Site 128-799 (Table 1)
Samples of Quaternary through Miocene diatomaceous sediment and siliceous sedimentary rock from the Japan Sea (ODP Leg 128, Site 799) were examined to determine the origin of... -
Element concentrations of amphiboles in ODP Hole 147-894G (Table 1)
Metamorphosed oceanic gabbros provide a record of the cooling history of the lower crust near mid-ocean ridges, but the temperature range, rate, and location of subsolidus... -
(Table 1) Abundance of shocked quartz in K/T boundary sediments from DSDP Sit...
Sediments from the Cretaceous/Tertiary (K/T) boundary at Deep Sea Drilling Project Site 596 record accumulation of pelagic clays at about lat 45°S,in the center of the ancestral... -
Seagrass blue carbon stocks in the German Baltic Sea
A total of 169 sediment cores (30 cm length; 5.5 cm inner diameter) were sampled in seagrass meadows (n = 110 cores) and nearby unvegetated sediments (n = 59 cores). Nine cores... -
KOSMOS Bergen 2015 mesocosm study: C. harengus survival
To evaluate the influence of ocean acidification on predatory plankton, e.g. Hydrozoa and fish larvae as well as their interaction in complex natural communities, we deployed... -
(Table 2) Monte Carlo end-member simulation results for the dual carbon isoto...
This dataset has no description
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(Table 4) Geochemical results for central basin sediment core PG2303: TOC and...
This dataset has no description
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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
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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... -
(Table 40-6) 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... -
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...
