-
Air-sea gas transfer velocities in the Baltic Sea measured with the Active Co...
Heat transfer velocities measured during three different campaigns in the Baltic Sea using the Active Controlled Flux Technique (ACFT) with wind speeds ranging from 5.3 to 14.8... -
(Table 4) Polarity magnetozones and correlative chrons of DSDP Hole 43-384
Below 161.25 mbsf magnetostratigraphy from Larson and Opdyke (1979, doi:10.2973/dsdp.proc.43.139.1979) -
Short gravity surface sediment cores from SE Skagerrak: core S57b/129 m/ wate...
Water: weight loss by dryingPb210: conc. HNO3/HCl digestion, Po210 deposition , Po210 alpha counting, surf. barrier detector (Erlenkeuser and Pederstad, 1984)Pb(Po)210 age: CIC... -
Short gravity surface sediment cores from SE Skagerrak: core POS35_S11b water...
Water: weight loss by dryingPb210: conc. HNO3/HCl digestion, Po210 deposition , Po210 alpha counting, surf. barrier detector (Erlenkeuser and Pederstad, 1984)Pb(Po)210 age: CIC... -
(Table 3) Morphometric measurements of Neogloboquadrina pachyderma sin. from ...
sampling size fraction 125-500 µm -
(Table 3) Morphometric measurements of Neogloboquadrina pachyderma sin. from ...
sampling size fraction 125-500 µm -
(Table 3) Morphometric measurements of Neogloboquadrina pachyderma sin. from ...
sampling size fraction 125-500 µm -
(Table 3) Morphometric measurements of Neogloboquadrina pachyderma sin. from ...
sampling size fraction 125-500 µm -
(Table 3) Morphometric measurements of Neogloboquadrina pachyderma sin. from ...
sampling size fraction 125-500 µm -
(Table 3) Morphometric measurements of Neogloboquadrina pachyderma sin. from ...
sampling size fraction 125-500 µm. Furthe test size measurements of N. pachyderma sin. see Huber et al. (2000b) data set: doi:10.1594/PANGAEA.81110 -
(Figure 2) C31 δ¹³C, %C3 vegetation, wet season length and mean annual rainfa...
calc. % C3: Estimates are based on d13C values for C4 plants of -21.7 per mil and for C3 plants of -35.2 per mil.calc. Wet season length: Estimates are based on WSL = 0.077(%C3)... -
(Supplementary Table 1) Overview of clumped isotope measurements from IODP Si...
Depth is m CCSF-A (core composite depth below sea floor) from Wilkens et al., 2013.Age from Drury et al., 2016. -
(Supplementary Table 2) Overview of clumped isotope derived temperatures and ...
Depth is m CCSF-A (core composite depth below sea floor) from Wilkens et al., 2013.Age from Drury et al., 2016.Sample ID and depth information as reported by Rousselle et al.,... -
Measurements of microbial processes, dissolution, water and porewater chemist...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of... -
Measurements of microbial processes, dissolution, water and porewater chemist...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of... -
Measurements of microbial processes, dissolution, water and porewater chemist...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of... -
The size-frequency distribution of TEP(2-16µm) in Aelotron experiment 2014
This dataset has no description
-
The size-frequency distribution of CSP(2-16µm) in Aelotron experiment 2014
This dataset has no description
-
Measurements of microbial processes, dissolution, water and porewater chemist...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of... -
Measurements of microbial processes, dissolution, water and porewater chemist...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of...