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Geochemical Measurements of Kelp in the Santa Barbara Basin, CA
<0 = concentrations below detection limit. -
Revised magnetic susceptibility analysis for the late Pliocene composite sect...
Magnetic susceptibility obtained for the mid to late Pliocene composite section at ODP Site 138-850, determined by shipboard measurements. Values are reported as magnetic... -
Revised color reflectance analysis for the late Pliocene composite section fr...
Color reflectance data obtained for the mid to late Pliocene composite section at ODP Site 138-850, determined by shipboard measurements using Channel 1 data from a visible... -
Bulk mineral composition on cores C00018, C0002D, C0002B and C0006E
This dataset has no description
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(Supplementary Table 2) Estimates of bottom-water oxygenation at site GeoB111...
HO = High Oxygen Indicators (Miliolids, except Articulina tubulosa + Cibicides spp. + Cibicidoides spp. + Gyroidinoides orbicularis + Planulina ariminensis); LO = Low Oxygen... -
Elemental geochemistry (Mn, P and Al) from IODP Site 306-U1314
Elemental geochemistry (Mn, P and Al) from IODP Site 306-U1314, between 84.12-60 mcd, which corresponds to ca. 779-1069 ka. The age model was previously published in... -
Geochemical composition of volcanic glass shards from the sediment core POS51...
To investigate the sedimentary record of the Mid Adriatic Deep (Adriatic sea) and its response to climate/oceanographic changes building a satisfactory depth-age model is... -
Middle Miocene stable carbon and oxygen isotopes of coexisting planktic foram...
Tests of planktic foraminifera are important tracers for reconstructing past oceanic environments. It is essential to have accurate information of the habitat depth of the... -
δ13C and δ18O isotopes of Globigerina bulloides from ODP Site 177-1090
Over the last deglaciation there were two transient intervals of pronounced atmospheric CO2 rise; Heinrich Stadial 1 (17.5-15 kyr) and the Younger Dryas (12.9-11.5 kyr). Leading... -
Microbial diversity and physicochemistry of an estuarine phototrophic bloom i...
Organic-rich, brackish water bodies are common along coastlines and important for the biogeochemical cycling of carbon, nitrogen, sulfur, and phosphorus. These ecosystems are... -
(Table S1) N15 isotope ratios, age determination and accumulation rates of se...
In a piston core from the central Bering Sea, diatom microfossil-bound N isotopes and the concentrations of opal, biogenic barium, calcium carbonate, and organic N are measured... -
Organic carbon and δ¹³C of sediment core GIK16772-2 (Table A5)
This dataset has no description
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Stable isotopes from ODP Hole 130-806B (Fig. 1)
The age of the Brunhes-Matuyama boundary, until recently taken as 730 k.y. in standard time scales for the Quaternary (e.g., Imbrie et al., 1984; Prell et al., 1986,... -
Interpolated and normalized Mg/Ca ratios for ODP Site 181-1123
AGE [ka BP] is interpolated age. -
Measured and normalized Mg/Ca ratios of ODP Site 181-1123 samples
This dataset has no description
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Neodymium (Nd) isotope composition of fossil fish debris and mixed planktic f...
This dataset presents neodymium (Nd) isotope ratios derived from fossil fish teeth/-bones (hereafter fish debris) and Fe-Mn coatings from mixed planktic foraminifera covering... -
Astrochronological age model (silicon) from the Contessa Road (Italy)
Ages are presented in kyr relative to the PETM onset (0 kyr). -
Astrochronological age model (calcium) from the Contessa Road (Italy)
Ages are presented in kyr relative to the PETM onset (0 kyr). -
Astrochronological age model (iron) from the Contessa Road (Italy)
Ages are presented in kyr relative to the PETM onset (0 kyr).
