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(Table T3) Ar40/Ar39 incremental heating ages of ODP Leg 180 dolerites
Ages are reported relative to biotite monitor FCT-3 (27.84 ± 0.12 Ma), which in turn is calibrated against hornblende Mmhb-1 (520.4, Samson and Alexander, 1987). Calculations... -
(Table T4) Argon 40 - Argon 39 incremental heating ages from Neogene ash laye...
Sediment depth is given in mbsf. All ages calculated relative to neutron fluence monitor FCT-2 biotite (28.04 ± 0.12 Ma), decay and abundance constants le = 0.581 x 10-10/yr; lb... -
Biometry of Siphonodictyon infestum (Johnson, 1899); sample no. ZMA POR 19927
See also doi:10.1594/PANGAEA.658984 for primary data -
Biometry of Siphonodictyon infestum (Johnson, 1899); sample no. ZMA POR 19927
See also doi:10.1594/PANGAEA.658942 for primary data -
Collection of X-ray micro computed tomography images of shells of planktic fo...
Calcite shells of planktic foraminifera (Protista, Rhizaria) constitute a large portion of deep-sea sediments. The shells are constructed by sequential addition of partly... -
Hydrothermal cleft monazite SIMS Th-Pb age data, central Alps
Ion probe (SIMS) Th-Pb age measurements of hydrothermal fissure/cleft monazite from the central Alps. The sample area encompasses most of the Lepontine metamorphic dome, the... -
40Ar-39Ar plateau and isochron ages from the Ninetyeast and Broken Ridges (Ta...
Concordant plateau and isochron ages are obtained from 40Ar-39Ar incremental heating experiments on volcanic rocks recovered by drilling at three Leg 121 sites along the... -
IMON_METH_PAR
Ontology of Methodes and Parameters of Integrated Monitoring -
T-MOSAiC 2022 myThaw data set
The Terrestrial Multidisciplinary distributed Observatories for the Study of the Arctic Connections (T-MOSAiC) 2022 myThaw data set provides standardized measurements for... -
Salinity tolerance study details with means and variances of parameters compi...
All studies included in the meta-analysis are listed with study details such as experimental design, species studied, number of replicates, salinity levels and mean values and... -
T-MOSAiC 2021 myThaw data set
The Terrestrial Multidisciplinary distributed Observatories for the Study of the Arctic Connections (T-MOSAiC) 2021 permafrost thaw data set provides standardized measurements... -
Single dataset information and storage location of the extension of the datas...
This dataset has no description
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Morphological data of experimental animals of wild and selected Saccostrea gl...
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... -
Carbon uptake rate calculated for CTD water samples during POLARSTERN cruise ...
Net Primary Production was measured using the 14C uptake method with minor modifications. Seawater samples were spiked with 0.1µCi ml-1 of 14C labelled sodium bicarbonate... -
Carbon uptake rate calculated for melt pond water samples during POLARSTERN c...
Net Primary Production was measured using the 14C uptake method with minor modifications. Melt pond samples were spiked with 0.1µCi ml-1 of 14C labelled sodium bicarbonate... -
Carbon uptake rate calculated for sea-ice core samples during POLARSTERN crui...
Net Primary Production was measured using the 14C uptake method with minor modifications. Melted sea ice samples were spiked with 0.1µCi ml-1 of 14C labelled sodium bicarbonate... -
(Table 6) Gas hydrate-related details of unit I and unit II deposits at the H...
a = The extent of analytical uncertainties is discussed in section 3.4.2; pv, pore volume. b = Assuming identical hydrate fractions in shallow and in deeper sediments. c =... -
Morphometric parameters of the Coral Belt Mounds (CBM), Namibian coral mound ...
Quantitative morphometric analyses were carried out for each mound following the workflows presented by Purkis et al. (2007) The coral mound base was defined following the... -
Phosphorus content and elemental ratios of gelatinous and soft-bodied zooplan...
Climate change and anthropogenic disturbances, among other factors, can change the seawater stoichiometry (C/N/P) and consequently elemental ratios of phytoplankton. This change... -
Results of modelled Arctic river discharge trends since 7 ka BP
The Arctic hydrological cycle throughout the Holocene is analyzed based on the results of transient simulations with the coupled atmosphere-ocean circulation model ECHO-G. The...
