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(Table 2) Strontium isotope ratios and age estimations of ODP Hole 120-748B o...
Original 87Sr/86Sr data are from Zachos et al. (1999) data set: doi:10.1594/PANGAEA.695370. The 87Sr/86Sr ratios were normalized to NIST-987= 0.710248 (McArthur et al., 2001) by... -
(Table 2) Strontium isotope ratios and age estimations of ODP Hole 119-744A o...
Original 87Sr/86Sr data are from Barrera et al. (1991) data set doi:10.1594/PANGAEA.695371. The 87Sr/86Sr ratios were normalized to NIST-987= 0.710248 (McArthur et al., 2001) by... -
(Appendix 8) Barium excess calculations in sediment core LV28-42-4
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(Table 2) SPECMAP stack of stable oxygen isotopes covering the last 300 000 y...
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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... -
Particulate organic carbon composition, granulometric and geochemical data fo...
To study the transformation of organic carbon through long distance transport in rivers, we measured the composition of bulk organic carbon in river suspended sediment of the... -
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... -
Tab. 1: Sampling date, location, ice thickness, salinity, Nd isotope composit...
Freshwater and sea ice in the Arctic Ocean (AO) both respond to climate forcing but changes in their distribution may in turn also significantly affect Northern Hemisphere... -
(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... -
(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... -
Near-UV observation of exoplanet HAT-P-16b
please provide abstract This is the transit of the hot Jupiter, HAT-P-16b taken with Mont4k CCD on the 1.55 m Steward Observatory Kuiper Telescope on Mt. Bigelow. We used the... -
(Appendix 1) Coral analysis and isostatic rebound effects from different Hole...
Past sea-level records provide invaluable information about the response of ice sheets to climate forcing. Some such records suggest that the last deglaciation was punctuated by... -
Tab. I: Alkenon analyses on sample material of cores Krummland KR-1 und Dageb...
Geochemical studies of organic "biomarker" compounds were applied to Eemian sediments cored at Dagebuell (DA-1) on the west coast, and at Krummland (KR-1) in the east of the... -
Total organic carbon, bitumen ratio, hopane and sterane parameters of ODP Sit...
Notable compositional changes of organic matter are observed below the silica transition zone in thermally immature sediments. The increase of bitumen ratio, and hopane and... -
Organic carbon and δ¹³C of sediment core 108-658B (Table A6)
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Organic carbon and δ¹³C of sediment core GIK16772-2 (Table A5)
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δ¹³C of plankton from surface water (Table A2)
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Organic chemistry analysis on surface sediments from the equatorial east Atla...
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Stable isotopes and sedimentation rate from sediment core M31/2_KL23
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