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Palynological characteristic of the ice deposit at the left bank of the Erkut...
Palynological characteristic of the ice deposit at the left bank of the Erkutayaha River (southern part of Yamal) in % (point 10–YuV–Yerk). -
(Table 8a) Presence of light minerals (<2.9) in bottom sediments of the South...
Data include total presence of minerals in whole sections of sediment cores in grain size fractions: >2.0; 2.0-1.0; 1.0-0.5; 0.25-0.1; 0.1-0.01 mm. + = present, - = absent. -
(Table T5) Distribution of accessory assemblages and other fragments in ODP H...
Sediment depth is given in mbsf. Abundance as follows: C = common, F = few, R = rare, B = barren. Tr = trace, X = present above trace quantities, N = noteworthy, - = not found. -
Microplastic in snow from European and Arctic sites
We analysed microplastic and fibers in snow samples from ice floes in the Fram Strait (2016/17) and from Spitsbergen, Helgoland, Bremen, Bavaria and the Swiss Alps (2018) to... -
Ice rafted debris content of sediment core MD99-2303
For method on "AGE" see Risebrobakken et al., 2005. For method on "Age model" see Risebrobakken et al., 2006 -
Smear slide investigation on ODP Hole 188-1166A
This dataset has no description
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A Synthetic Control Assessment of the Green Paradox The Role of Climate Actio...
This paper extends the green paradox literature by providing empirical insights into its existence. To check the green paradox theory, I analyse the production of coal in four...