This dataset contains stable isotope (carbon, oxygen) as well as Radiocarbon ages from North Atlantic sediment core SU90-08. The radiocarbon ages were measured on benthic (mixed species) as well as on planktonic (single species) using both classical graphite targets and MICADAS coupled with a gas introdcution system. Radiocarbon measurements were performed at ETH Zürich and Chrono center Belfast. The stable carbon and oxygen isotope measurements were performed on benthic foraminifera C. Wuellestorfi at LSCE, Gif sur Yvette. The radiocarbon measurements cover the last 25 ka (cal BP) and the stable isotopes measurements cover the last 40 ka. Please refer to the article "Radiocarbon dating of small sized foraminifer samples: insights into mar...
foraminifera and corals, requires the extraction of about 1 mg C (10 mg CaCO3). Most laboratories pr...
In recent years, the most common technique for radiocarbon dating of deep-ocean sediments has been a...
Radiocarbon ages measured on different sample types from the marine sediment core OR1-1218-C2-BC whi...
Radiocarbon (14C) can be used to build absolute chronologies and reconstruct ocean ventilation over ...
Sediment depth age-models, stable carbon isotope data, and radiocarbon data are reported for a suite...
Radiocarbon (14C) measurements of foraminifera often provide the only absolute age constraints in ma...
Radiocarbon was measured on small mono-specific samples of between 3 and 30 individual foraminiferal...
We present radiocarbon results from a geographically constrained depth transect of sediment cores fr...
International audienceFor 14C measurements of ultra-small samples we use the gas ion source of the A...
The 51.58 m long marine sediment core MD99-2220 was raised from the Laurentian Channel in the St. La...
Radiocarbon (14C) measurements of foraminifera are often challenging as their reliability and accura...
In recent years, the most common technique for radiocarbon dating of deep-ocean sediments has been a...
International audienceRadiocarbon dating of small foraminifera samples with a gas ion source Contenu...
From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000.In re...
From the 12th International Radiocarbon Conference held in Trondheim, June 24-28, 1985.14C ages were...
foraminifera and corals, requires the extraction of about 1 mg C (10 mg CaCO3). Most laboratories pr...
In recent years, the most common technique for radiocarbon dating of deep-ocean sediments has been a...
Radiocarbon ages measured on different sample types from the marine sediment core OR1-1218-C2-BC whi...
Radiocarbon (14C) can be used to build absolute chronologies and reconstruct ocean ventilation over ...
Sediment depth age-models, stable carbon isotope data, and radiocarbon data are reported for a suite...
Radiocarbon (14C) measurements of foraminifera often provide the only absolute age constraints in ma...
Radiocarbon was measured on small mono-specific samples of between 3 and 30 individual foraminiferal...
We present radiocarbon results from a geographically constrained depth transect of sediment cores fr...
International audienceFor 14C measurements of ultra-small samples we use the gas ion source of the A...
The 51.58 m long marine sediment core MD99-2220 was raised from the Laurentian Channel in the St. La...
Radiocarbon (14C) measurements of foraminifera are often challenging as their reliability and accura...
In recent years, the most common technique for radiocarbon dating of deep-ocean sediments has been a...
International audienceRadiocarbon dating of small foraminifera samples with a gas ion source Contenu...
From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000.In re...
From the 12th International Radiocarbon Conference held in Trondheim, June 24-28, 1985.14C ages were...
foraminifera and corals, requires the extraction of about 1 mg C (10 mg CaCO3). Most laboratories pr...
In recent years, the most common technique for radiocarbon dating of deep-ocean sediments has been a...
Radiocarbon ages measured on different sample types from the marine sediment core OR1-1218-C2-BC whi...