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(Table 3) Nd isotopic ratios of fossil fish teeth and HH extractions of Creta...
Sediment depth is given in mcd. JNdi-1 was run several times during each day of analyses for standardization on the Nu MC-ICPMS. The offset between the daily average JNdi-1... -
(Table 5) Inter and intra laboratory Pb isotope duplicates of authigenic Fe-M...
Sediment depth is given in mbsf. All inter and intra laboratory comparison data are normalized to NIST SRM 981 values reported in Galer and Abouchami (1998) for comparison to... -
(Table 1) Trace element and Tl isotope composition of Late Neogene pyrites
This dataset has no description
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(Table 1) Nd, Sr and Pb isotope records of sediment cores from the Gulf of Ca...
The age model for core M39008 was published by Cacho et al. (2001, doi:10.1029/2000PA000502) and Löwemark et al. (2004, doi:10.1016/S0025-3227(03)00351-7). The age models for... -
(Table 3) Nd and Pb isotope records of sediment cores from the Gulf of Cadiz ...
The age model for core M39008 was published by Cacho et al. (2001, doi:10.1029/2000PA000502) and Löwemark et al. (2004, doi:10.1016/S0025-3227(03)00351-7). The age models for... -
Late Pleistocene δ¹¹B based carbon dioxide levels from ODP Site 154-926
Earth's climate cooled markedly during the Late Miocene from 12 to 5 million years ago, with far-reaching consequences for global ecosystems. However, the driving forces of... -
(Table 2) Arctic Ocean down core leachate and bulk digest radiogenic isotope ...
DEPTH, sediment/rock [m] is given in mcd. -
(Table DR2) Nd isotopic composition of fossil fish teeth and debris from ODP ...
Fraction >0.125 mm was analysed. -
(Table 1) B/Ca and d11B ratios of foraminifera from marine surface sediments
All environmental parameters taken from nearby GLODAP site -
Delta 66Zn ratios and age of carbonates from ODP Site 138-849 (Table 1)
The carbonate fraction of sediment core ODP 849, leg 138, located in the eastern equatorial Pacific, mostly consisting of coccoliths, was separated and analyzed for its Zn... -
Isotope record of Nd-Sr-Pb in deep sea sediments from the Pacific (Table 2)
Pelagic clay of the east-central Pacific province is shown to be a mixture of three primary detrital components, reflecting continental source areas in Asia, North America, and... -
Whole rock major element, trace element and Sr-, Nd- Pb-isotope data of pluto...
This dataset has no description
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(Table 6) Liconcentrations and isotope compositions of various sediment sampl...
This dataset has no description
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Boron and Lithium isotopes of Kumano mud volcanoes' pore waters extracted fro...
B and Li Isotopes data of Kumano mud volcanoes' (Offshore SE Japan) pore waters extracted from cores taken during the SO222 expedition in 2012. Aliquots of 14 untreated fluids... -
Endmember B and Li concentration and isotope ratios of high temperature black...
Calculated pure hydrothermal end-member Li and B isotope compositions in high-temperature fluids from Brothers volcano, Kermadec Arc, Western Pacific collected during SO-253... -
Boron, lithium and isotope compositions in acid-sulfate and black smoker flui...
Lithium, boron and magnesium isotope compositions in high-temperature and acid-sulfate fluids from Brothers and Macauley volcano, Kermadec Arc, Western Pacific collected during... -
Geochemical data from the Cenomanian-Turonian interval of ODP Hole183-1138A
Geochemical data from Ocean Drilling Program Site 1138A, core 69, spanning the Cenomanian–Turonian boundary interval (~94 Ma). The data were generated from marine sediment in... -
(Table S2) Neodymium isotopes of detrital and hydroxylamine hydrochlorite fra...
Sediment depth is given in mcd. -
(Table S1) Neodymium isotopes of fish teeth and hydroxylamine hydrochlorite e...
Sediment depth is given in mcd. For further Nd values see MacLeod et al. (2011) datasets doi:10.1594/PANGAEA.792572. -
(Table S1) Neodymium isotopes of fish teeth and hydroxylamine hydrochlorite e...
Sediment depth is given in mcd. For further Nd values see MacLeod et al. (2008) datasets doi:10.1594/PANGAEA.722613; MacLeod et al. (2011) datasets doi:10.1594/PANGAEA.792572...
