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(Table 1) Lithology, N isotope ratios and carbonate content of DSDP Hole 93-603B
This dataset has no description
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(Table 1) Lithology, N isotope ratios and carbonate content of DSDP Hole 75-530A
For C-chemistry see Dean et al (1986) dataset: doi:10.1594/PANGAEA.714825 -
(Table 1) Lithology and N isotope ratios of DSDP Hole 41-367
For C-chemistry see Dean et al (1986) dataset: doi:10.1594/PANGAEA.714823 -
Statistical analysis of bulk nitrogen isotopes from IODP Site 323-U1342
Here, we present the results of a statistical analysis published in Knudson et al., (2021, Science Advances), which investigates nitrogen isotopes from Integrated Ocean Drilling... -
Bulk sedimentary nitrogen isotopes and nitrogen content of ODP Site 202-1242
The bulk sedimentary nitrogen isotopic measurements and relative contribution of nitrogen were analysed in ODP Site 202-1242 (7º51.352'N, 83º36.418'W, 1364 meters water depth)... -
Bulk and diatom-bound nitrogen isotope ratios, opal, TOC, and TN from ODP Hol...
Intense seasonal productivity and carbon drawdown on the West Antarctic Peninsula (WAP) is driven by upwelling of nutrient-rich Circumpolar Deep Water (CDW) and subsequent... -
Nitrogen isotope ratio and oxygen isotope ratio from Arabian Sea IODP Site 35...
Denitrification in the Arabian Sea is closely related to the monsoon-induced upwelling and subsequent phytoplankton production in the surface water. The δ15N values of bulk... -
Organic matter derived stable isotopes from ODP Site 177-722
Data included in this entry was sampled from ODP Site 722 (16.6218°N/59.7953°E). Original drilling was carried out by E/V JOIDES Resolution as part of ODP leg 117 between 6th... -
Bulk sediment nitrogen isotopes from IODP Site 323-U1343 Holes A, C, and E
High latitude deep water upwelling has the potential to control global climate over glacial timescales through the biological pump and ocean-atmosphere CO2 exchange. However,... -
(Table 1) Comparison of diatom-bound and bulk sedimentary d15N values of ODP ...
The Matuyama Diatom Maximum (MDM) is a time of peak opal accumulation from 2.6 to ~2.0 Ma within the Benguela Current upwelling system that was initiated by increased influence... -
Ranges and mean values for elemental and isotopic composition in the early Ap...
The occurrence of intervals of enhanced sequestration of organic matter (OM) during the Mid-Cretaceous-collectively termed "Oceanic Anoxic Events" (OAE)-reflect abrupt changes... -
SSGC-ESEP: Surface sediment bulk geochemistry from the equatorial and south e...
In this first volume of SSGC-ESEP, we show bulk sediment geochemistry of surface marine sediments from the continental margin off Chile (Southeast Pacific). The surface sediment... -
δ¹³Corg and d15N of lake Nam Co sediment core NC 08/01
This study is part of DFG Priority Programme (Schwerpunktprogramm) 1372 "Tibetan Plateau: Formation - Climate - Ecosystems (TiP)" -
Bulk sediment δ15N of sediment core M40/4_SL87, Balearic Rise, Western Medite...
The data were raised to compare the history of sea-surface temperature (based on the alkenone unsaturation index UK'37), organic and inorganic carbon accumulation, and the ratio... -
Stable isotope analysis of sediment core CD86_11_BC8
This dataset has no description
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Stable isotope analysis of sediment core CD86_09_BC1
This dataset has no description
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Stable isotope analysis of sediment core CD86_07_BC4
This dataset has no description
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Stable isotope analysis of sediment core CD86_05_BC5
This dataset has no description
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Stable isotope analysis of sediment core CD86_03_BC4
This dataset has no description
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Stable isotope analysis of sediment core CD86_01_BC1
This dataset has no description
