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(Tabls S1) Bulk geochemistry for sediment samples collected from the Cenomani...
Oceanic Anoxic Event 2 (OAE2), spanning the Cenomanian-Turonian boundary (CTB), represents one of the largest perturbations in the global carbon cycle in the last 100 Myr. The... -
(Table 1) Geochemistry of the ETM-2 section from IODP Hole 302-M0004A
During the early Eocene, a series of short-term global warming events ("hyperthermals”) occurred in response to the rapid release of carbon into the oceans and atmosphere. In... -
(Table 1) Carbon and isotopic composition of organic carbon in sediments from...
We have analyzed inorganic and organic carbons and determined the isotopic composition of both sedimentary organic carbon and inorganic carbon in carbonates contained in... -
(Table 2) δ¹³C from the Lusklint section
The carbon isotope composition (d13C) of bulk organic matter and two palynomorph groups (scolecodonts and chitinozoans) from the Llandovery-Wenlock strata of Gotland (E Sweden)... -
(Table 1) Isotopic composition of organic compinents of DSDP Hole 24-231
Plant leaf wax hydrogen isotope (dDwax) reconstructions are increasingly being used to reconstruct hydrological change. This approach is based upon the assumption that... -
(Table 1) Organic carbon isotopic composition in Cretaceous sediments at DSDP...
Cretaceous sediments from DSDP Site 530 have been analyzed for organic carbon isotopic composition. The d13C values in the sediments decrease from -22.7 per mil to -27.5 per mil... -
Hydrochemistry measured on water bottle samples during POLARFRONT cruise PF94
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Hydrochemistry measured on water bottle samples during POLARFRONT cruise PF93
This dataset has no description
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Hydrochemistry measured on water bottle samples during POLARFRONT cruise PF92
This dataset has no description
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Hydrochemistry measured on water bottle samples during POLARFRONT cruise PF91
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Hydrochemistry measured on water bottle samples during Johan Hjort cruise JH9...
This dataset has no description
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Hydrochemistry measured on water bottle samples during G. O. Sars cruise GS90
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(Table 1) Organic carbon, nitrogen and sulphur concentrations and δ¹³C of TOC...
A high-resolution analysis of Hole 1017E revealed that total organic carbon (TOC) concentrations (24.8 ± 2.9 mg/g) and d13C of TOC (-21.3 ± 0.2 per mil) in Holocene sections are... -
(Appendix) Carbon and nitrogen isotope ratios of ODP Site 160-964
Nitrogen isotopes of chlorins, degradation products of chlorophyll, reflect the isotopic composition of nutrient N utilized by marine phytoplankton communities. Here we show... -
delta13Corg of Paleozoic land plants
Based on the evaluation of 1323 carbon isotope values for Silurian to Permian terrestrial organic carbon, measured on plant fossils, cuticules, humic coals and bulk terrestrial... -
Concentration and stable carbon isotopic composition of organic carbon of DSD...
The 7% carbon-13 depletion in cold water phytoplankton provides a striking signal that is traceable in deep-sea cores taken in high latitude regions of the Southern hemisphere.... -
Stable carbon and oxygen isotope ratios of foraminifera and organic carbon of...
Ocean Drilling Program Leg 188, Prydz Bay, East Antarctica is part of a larger initiative to explore the Cenozoic history of the Antarctic Ice Sheet through direct drilling and... -
Age determination of sediment core HZM, lake Holzmar (Tables 1, 2)
AMS radiocarbon ages have been determined on terrestrial macrofossils selected from the annually laminated sediments of lake Holzmaar (Germany). The radiocarbon chronology of... -
Concentrations of organic carbon and organic matter isotopic compositions of ...
Multiple layers of sapropels occur widely in the sedimentary record of the Mediterranean Sea and record repetitions of paleoclimatic conditions that favored increased production... -
(Table 1) Age determination on sediment core Glen_Torridon
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