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Table 1. Concentration of rare earth elements in ferromanganese nodule (crust...
Based on the X-ray fluorescence spectrum analysis of 15 rare earth elements in 6 ferromanganese nodu1es and 5 ferro mangane se crusts from the South China Sea, their abundances,... -
Carbon and oxygen isotopic compositions of Permian and Carboniferous brachiop...
This dataset has no description
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Carbon and oxygen isotopic compositions of Permian and Carboniferous brachiop...
Depositional Environment (Bruckschen et al., 2001), relative depth from shallow to deeper: 7 isolated shelf sea lagoon; 6 semiisolated sea shallow bank; 5 shallow part of open... -
Global soil and peat branched GDGT compilation dataset
Accurate temperature records for the deep geological past are a vital component of paleoclimate research. Distributional changes of branched glycerol dialkyl glycerol tetraether... -
Stable isotopes and Mg/Ca ratios of Globorotalia truncatulinoides from sedime...
Stable carbon (δ13C) and oxygen isotope (δ18O) and Mg/Ca-measurements were performed on the planktonic subsurface-dwelling foraminiferal species Globorotalia truncatulinoides.... -
(Table S2) Stable isotope record and Mg/Ca ratios of benthic foraminifera fro...
Mg/Ca ratios at 22.26 m depth are measured on 16 Cibicidoides spp. and 17 C. pippeni. For dataset of Miller et al. (2008) see: doi:10.1594/PANGAEA.769592 -
Standard data for major and trace element analyses of whole rocks using XRF a...
This dataset has no description
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Animal sightings during Filchner Expedition 1912
Digitized from text by Maximiliane Heidecke, Larissa Brockmann, Agata Zielnica, Marten Tönjes. See further details for a Google Earth layer. -
Holocene precipitation change in different monsoon sub-regions (time-slices a...
The recently proposed global monsoon hypothesis interprets monsoon systems as part of one global-scale atmospheric overturning circulation, implying a connection between the... -
Beryllium-10 concentration in the EPICA Dome C core between 2384.36 and 2626....
Ice cores are exceptional archives which allow us to reconstruct a wealth of climatic parameters as well as past atmospheric composition over the last 800 kyr in Antarctica.... -
(Table 1) Diatom bioevents used for the Middle Miocene age model of ODP Hole ...
This dataset has no description
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Chronostratigraphic summary for Middle Miocene through Pliocene dinoflagellat...
This dataset has no description
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(Table S4) Tie points between the Vostok and EDC99 ice cores
This dataset has no description
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(Table S3) Tie points between the DF and EDC99 ice cores
This dataset has no description
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(Table S1) Stable carbon and oxygen isotope ratios of Nuttallides truempyi of...
An exceptional analogue for the study of the causes and consequences of global warming occurs at the Palaeocene/Eocene Thermal Maximum, 55 million years ago. A rapid rise of... -
Ship-based biogeochemical bottle data from the CVOO time series (2006-2019) i...
This dataset compiles all available ship-based biogeochemical measurements at the Cape Verde Ocean Observatory (CVOO) into one merged dataset. The irregular measurements at CVOO... -
(Table 2) U and Th concentrations, isotopic activity ratios, and ages of cora...
This dataset has no description
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Respiration rate of pelagic copepods determined experimentally
This dataset has no description
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Amino acids and hexosamines in water and pore water samples from different oc...
These water and pore water samples were collected in different oceanic areas between 2013 and 2016. The samples were compiled from previous studies and used for statistical... -
Dissolved and soluble pore water trace metals (Cd, U, V, Cu, As, Mo) from sed...
Physical and chemical trace metal speciation are important for our understanding of metal cycling and potential toxicity to marine life. Trace metals can have different...
