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Age chronology (modern) based on U/Th ages, bomb pulse 14C data and year of c...
Stalagmite GL-S3 chronology in Years CE for upper 4 mm based on laminae count and year of collection (2008). -
δ13C and δ18O record of Stalagmite GL-S3 (modern) from the Golgotha Cave in s...
GolgothaCave_GLS3modern_stalagmite_O&C_isotopes: median depth, d18O and d13C values in VPDB for upper 4 mm. Chronology is that used for Treble et al (2022). -
Age chronology based on U/Th ages, bomb pulse 14C data and year of collection...
Stalagmite GL-S2 chronology in Years CE based on U/Th ages, bomb pulse 14C data and year of collection (2005). Treble et al. (2022) used 50th percentile age-depth model. -
δ13C and δ18O record of Stalagmite GL-S4 from the Golgotha Cave in southwest ...
GolgothaCave_GLS4_stalagmite_O&C_isotopes: median depth, d18O and d13C values in VPDB. Chronology is that used for Treble et al (2022). -
δ13C and δ18O record of Stalagmite GL-S1 from the Golgotha Cave in southwest ...
GolgothaCave_GLS1_stalagmite_O&C_isotopes: median depth, d18O and d13C values in VPDB. Chronology is that used for Treble et al (2022). -
Age chronology based on aminae count and year of collection (2012) of Stalagm...
Stalagmite GL-S4 chronology (CE) based on laminae count and year of collection (2012). This laminae count is the chronology used in Treble et al (2022). -
Oxygen and carbon isotope, saturation magnetization and coercivity from a sta...
We present results of oxygen isotope, saturation magnetization (Ms) and coercivity (Bc) data from a speleothem from northern Tasmania, Australia.The depths are relative to the... -
Fluid inclusion hydrogen isotope data from speleothem WB-21-5-A
Deuterium measured from water was converted to temperature using several different transfer functions (parameters 5-7). The error applies to both temperature and temperature... -
Fluid inclusion hydrogen isotope data from speleothem EC-17-7-A
Deuterium measured from water was converted to temperature using several different transfer functions (parameters 4-6). The error applies to both temperature and temperature... -
Stable isotope records of sei whale baleens from Chilean Patagonia
The datafile includes nitrogen and carbon isotope analyses of seven baleen plates from six individuals of sei whales (Balaenoptera borealis) from the Chilean-Patagonian fjord... -
Neodymium and lead isotopes from manganese crust DR01-001a (Vema)
The ages are calculated for the respective mean depths. Depending on the different growth rates of the crusts, samples correspond to different age intervals. -
Calcium carbonate and inorganic carbon in the western Arabian Gulf
This dataset has no description
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Calcium carbonate and inorganic carbon in the Central eastern Red Sea coast
This dataset has no description
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Annual Sr/Ca record from a Diploastrea heliopora coral from Fiji covering 137...
The 627-year record spanning from 1370 to 1997 consists of annual Sr/Ca measurements obtained from a Diploastrea heliopora coral core (F14) extracted from Kanathea Island in the... -
Uranium series isotopes and dating of stalagmite C09-2 from Closani Cave
Ages were calculated using the half-lives of Cheng et al. (2000). Correction for detrital contamination assumes a 232Th/238U weight ratio of 3.8 ± 1.9 and 230Th, 234U and 238U... -
Stable oxygen and carbon isotope record of stalagmite C09-2 from Closani Cave
This dataset has no description
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Table 1. Composition of manganese crusts from the Atlantis Fracture Zone
Summaries of the transition element chemistry of oceanic ferro-manganese deposits report compositional trends related to water depth and to geographic proximity to continental... -
(Table 8.4, Page 220-223) Chemical composition of different growth structures...
In the nodule field of the Peru Basin, situated south of the zone of high bioproductivity, a relatively high flux of biogenic matter explains a distinct redox boundary at about... -
(Table 4+5, Page 290) Distribution of Mn, Fe, Cu. Pb, Zn, Ni and Co in single...
Chemical analyses of manganese nodules from the Central Pacific Basin show that their chemical composition varies regionally, although that of the associated sediments is... -
(Figure 2, page 940) K-T boundary enrichment for cerium and iridium chemical ...
Hydrogenous manganese nodules form on the ocean floor by slow authigenic precipitation (1-6 mm/Ma) of the oxyhydroxides of manganese and iron that continuously scavenge trace...
