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(Fig. 21) DYE-3, GRIP, Crete winter season δ¹⁸O average
This is the average of the normalized winter d18O series from the three ice cores. The average time series has been normalized. -
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... -
Organic carbon and δ¹³C of sediment core 108-658B (Table A6)
This dataset has no description
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Organic carbon and δ¹³C of sediment core GIK16772-2 (Table A5)
This dataset has no description
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δ¹³C of plankton from surface water (Table A2)
This dataset has no description
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Organic chemistry analysis on surface sediments from the equatorial east Atla...
This dataset has no description
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Stable isotopes and sedimentation rate from sediment core M31/2_KL23
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,... -
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... -
Geochemical Measurements of Kelp in the Santa Barbara Basin, CA
<0 = concentrations below detection limit. -
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... -
(Table 1) Helium isotope ratios of sediment core TT013_114
We present a helium isotope record for core TT013-114PC from the central equatorial Pacific (140°W, 4°N, 4432 m water depth) spanning a period of 1 million years. We focus on... -
Elemental geochemistry (P, Ca, Al, Fe and Mn) from IODP 306-U1314
Elemental geochemistry (P, Ca, Al, Fe and Mn) from IODP Site 306-U1314, between 84.12-60 mcd, which corresponds to ca. 779-1069 ka. The age model was previously published in... -
Methane ebullition, sedimentation rates, organic matter quality and environme...
To determine spatiotemporal variability of methane (CH4) ebullition and its drivers, we measured CH4 ebullition rates, sedimentation rates and characteristics of the sedimented... -
Carbonate mass accumulation rates from IODP Hole 371-U1506A
This dataset has no description
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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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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...
