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Sediment depth age-models, stable carbon isotope data, and radiocarbon data o...
Sediment depth age-models, stable carbon isotope data, and radiocarbon data are reported for a suite of sediment cores from Iberian- and Brazil Margins, in the Atlantic basin.... -
Climate variability in the northern Mediterranean across the onset of the Mes...
This data set was used to trace the climate and hydrologic variability in the northern Mediterranean in the late Miocene, from about 6.07 to 5.92 Ma. This time interval... -
The middle to late Miocene "Carbonate Crash" in the equatorial Indian Ocean
We integrate benthic foraminiferal stable isotopes, X-ray fluorescence elemental ratios, and carbonate accumulation estimates in a continuous sedimentary archive recovered at... -
Carbon stable isotopes of coral colony 13SS-1 from the Tropical South Atlantic
This dataset has no description
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Composite carbon stable isotopes of regional coral colonies from the Tropical...
This dataset has no description
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Carbon stable isotopes of coral colony 18ACS2 from the Tropical South Atlantic
This dataset has no description
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Carbon stable isotopes of coral colony 18ACS1 from the Tropical South Atlantic
This dataset has no description
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Carbon stable isotopes of coral colony 18SM-C2 from the Tropical South Atlantic
This dataset has no description
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Organic geochemical proxies of the Govone section
0.0001 = traces. -
Stable isotope ratios of Planulina wuellerstorfi of IODP Site 353-U1443
Isotope values were first specified with one decimal place, corrected to 3 decimal places (2020-01-21). -
Stable isotopes data from marine sediment core CAGE19-3-KH14, the eastern Fra...
We present stable oxygen and carbon isotopes data from marine sediment core CAGE19-3-KH14. Core CAGE19-3-KH14 was retrieved from the eastern Fram Strait (77°31'22.8" N,... -
Dissolved Methane release from the western margin of the Greenland Ice Sheet ...
A field sampling campaign spanning the entire western margin of the Greenland Ice Sheet was conducted in the summer melt seasons of 2021, 2022, and 2023, to measure release of... -
Calcium concentration in sediment cores from the Arctic Ocean
Cores analyzed in this dataset were retrieved from three Swedish expeditions: Arctic Ocean Expedition 1996 (AO96), Lomonosov Ridge off Greenland (LOMROG) 2007 and 2012. The four... -
Mg/Ca ratios and stable isotopes of Neogloboquadrina pachyderma in the Arctic...
Cores analyzed in this dataset were retrieved from three Swedish expeditions: Arctic Ocean Expedition 1996 (AO96), Lomonosov Ridge off Greenland (LOMROG) 2007 and 2012. The four... -
Mean ages calculated by the bayesian age-depth model of sediment core JPC42 f...
Age-depth model of the JPC42 sediment core. The core chronology is based on the radiocarbon ages published in Caniupán et al. (2014, doi:10.1016/j.yqres.2014.07.009). All... -
Predicted mean grain size of the JPC42 sediment core from Wide Channel (Chile...
Mean grain size predicted at a 2 mm resolution using the XRF intensities of Fe, K, Ti, Rb, Zr and Mn following Liu et al. (2019, doi:10.1029/2018GC008154). A set of 112 samples... -
Geochemical and sedimentological data of the JPC42 sediment core from Wide Ch...
Organic geochemical and sedimentological data analyzed at a 10 to 20 cm interval on the JPC42 and KC41 cores including total organic carbon content, stable carbon isotopes,... -
Mean ages calculated by the bayesian age-depth model
The age model of the LAR sediment core was produced with the BACON 2.4.3 software, using 11 radiocarbon ages. The table contains the mean age of the sediment at a 1mm resolution. -
Fractions of lithogenic particles >63 µm and >150 µm of the LAR sediment core
The lithogenic fractions >63 µm and >150 µm were separated through wet-sieving. Five (30.5 – 680.5 cm) or 10 g (680.5 – 910.5 cm) of freeze-dried sediment was used for... -
Magnetic susceptibility of the LAR sediment core
Continuous high-resolution logging of magnetic susceptibility was accomplished using a Bartington MS2E spot sensor integrated into an automatic logging system. Measurements were...
