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Compilation of stable nitrogen and carbon isotope ratios of marine biota from...
Bulk stable isotope ratios, primarily of carbon (δ13C) and nitrogen (δ15N), are increasingly used to examine predator-prey interactions and food web structure. We compiled δ13C... -
Element contents and n-alkane pattern of Late Quaternary sediments from the V...
This dataset has no description
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Carbon-chemistry of Tangra Yumco lake sediment record
This dataset has no description
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Seawater carbonate chemistry and changes in isotope fractionation during nitr...
We measured N and O isotope effects during nitrate assimilation and physiological states of the marine diatom Thalassiosira weissflogii and Synechococcus under different pH (8.1... -
Bulk stable isotope analysis (SIA) of historical and contemporary squid beaks
Raw data obtained from stable isotope analysis of δ13C and δ15N in beaks of the squids Gonatus fabricii (Lichtenstein, 1818) and Todarodes sagittatus (Lamarck, 1798)... -
Geochemical data for SOB14-A-21, a Lena Delta 1st terrace exposure
The Holocene delta deposit (1st terrace) exposure SOB14-A-21 (72.53671°N, 127.98945°E) was sampled on 17 August 2014 North of Sobo-Sise Island in the Lena Delta during the... -
Sediment properties of gravity core DG12-GC05 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Sediment properties of gravity core DG12-GC04 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Sediment properties of gravity core DG12-GC02 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Sediment properties of gravity core DG12-GC01 obtained on the Drygalski Basin...
The MS was measured at 1 cm interval using Bartington MS-2B susceptibility meter. The WC was also measured at 1 cm interval using 1 cm thick subsamples by calculating the... -
Biological carbon pump efficiency in the Humboldt current system off Peru: fl...
Potential drivers of export flux attenuation: relationship between carbon export flux and satellite-derived primary production28 (PP, during period of deployment), export flux... -
Geochemistry and biomarker of sediment core PS97/068-2
Calendar Years AD 1780-1875 are extrapolated based on the prior sedimentation rate. -
Geochemistry and biomarker of sediment core PS97/056-1
Calendar Years AD 1830-1880; 1780-1875 and 1823-1876 are extrapolated based on the prior sedimentation rate. -
Adaptation of a globally important coccolithophore to ocean warming and acidi...
This dataset has no description
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Sedimentological bulk parameter in surface sediments from the Ob and Yenisei ...
This dataset has no description
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Seawater carbonate chemistry and growth and carbon fixation of Antarctic cryp...
We conducted a multiple-stressor experiment to evaluate the response of the still poorly studied key Antarctic cryptophyte species Geminigera cryophila (CCMP 2564, isolated from... -
Seawater carbonate chemistry and growth, elemental composition,biomass produc...
Sea ice retreat, changing stratification, and ocean acidification are fundamentally changing the light availability and physico-chemical conditions for primary producers in the... -
Seawater carbonate chemistry and physiological parameters of Thalassiosira sp...
Marine diatoms are one of the marine phytoplankton functional groups, with high species diversity, playing important roles in the marine food web and carbon sequestration. In... -
Seawater carbonate chemistry and growth,cellular composition and photophysiol...
Compared to the rest of the globe, the Arctic Ocean is affected disproportionately by climate change. Despite these fast environmental changes, we currently know little about... -
Seawater carbonate chemistry and growth and particulate organic nitrogen prod...
Phytoplankton in the upper oceans are exposed to changing light levels due to mixing, diurnal solar cycles and weather conditions. Consequently, effects of ocean acidification...