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Biogeographic variability in the physiological response of the cold-water cor...
While ocean acidification is a global issue, the severity of ecosystem effects is likely to vary considerably at regional scales. The lack of understanding of how... -
Seawater carbonate chemistry and reproductive success of giant kelp (Macrocys...
Understanding how climate change may influence ecosystems depends substantially on its effects on foundation species, such as the ecologically important giant kelp (Macrocystis... -
Seawater carbonate chemistry and behaviour of coral reef fishes
The partial pressure of CO2 in the oceans has increased rapidly over the past century, driving ocean acidification and raising concern for the stability of marine ecosystems.... -
Seawater carbonate chemistry and characterising biogeochemical fluctuations i...
Coastal and intertidal habitats are at the forefront of anthropogenic influence and environmental change. The species occupying these habitats are adapted to a world of... -
(Table 2) Daily velocities and travel distances of individual gray whales (Es...
Satellite transmitter information from Table 1 included. Tagging position of Graywhale_37286 was on land (Latitude: 65.604 Longitude: -171.279), so position was slightly adapted... -
Pulse amplitude modulation (PAM) of the benthic foraminiferia Amphistegina lo...
Med: Eastern Mediterranean -
Field soundscape recordings obtained from three geographically separated natu...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2015) was used to compute a complete and consistent set of... -
Fig. 2 - Larval performance of Baltic Sea and North Sea populations exposed t...
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... -
Trace element concentrations of calcite veins pervading the Troodos pillow lavas
<: Below detection limit -
Bulk rock data of serpentinites and ophicalcites from the Northern Apennine o...
Below detection limit (bdl) = <0.01Not determined (n.d.) = empty cell -
Trace element mineral analyses from the Northern Apennine ophiolite sequence
Empty cell = not determined (n.d.)<0.01 = below detection limit (bdl)<0.0001 = below detection limit (bdl) for Tantalum -
Geochronologic and trace element concentrations for zircon from Northern Yeme...
This dataset has no description
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Uranium series ages of cold-water corals from east Equatorial Atlantic and Re...
U-series ages of deep-sea corals from east Equatorial Atlantic and Reykjanes Ridge defined by laser ablation method. Depths of east Equatorial Atlantic corals was retrieved by... -
Detrital rutile trace element from the late Neogene Baode Red Clay sequence, ...
The data consist of detrital rutile trace element geochemistry of the 6.91–2.64 Ma Baode Red Clay (three samples from the Miocene Baode Formation, five samples from the Pliocene... -
Blanks for microplastic analysis in sediment samples
This dataset has no description
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Temperature responses of different functional traits in Arctic phytoplankton
This study was conducted in autumn/winter 2021/2022 at the laboratory of the Alfred-Wegener-Institute Bremerhaven. To assess temperature response patterns of various functional... -
Radiocarbon dates of peat in palsas near Eletsky settlement, north-eastern pa...
Conventional radiocarbon dating was carried out at the Institute for the History of Material Culture, St. Petersburg (lab code Le), at the radiocarbon laboratory of Helsinki... -
Stratigraphy and cryostructure of peat and underlying mineral sediments of pa...
This dataset has no description
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Stable isotope values (δ18О, δ2Н and dexc) for palsa ice cores and surface wa...
Stable isotope ratios in ice were analyzed in the stable isotope laboratory of the Geography Faculty at Lomonosov Moscow State University using a Finnigan Delta-V Plus mass... -
Minimum, mean and maximum values of δ18O, δ2H and dexc for palsa ice cores an...
Stable isotope ratios in ice were analyzed in the stable isotope laboratory of the Geography Faculty at Lomonosov Moscow State University using a Finnigan Delta-V Plus mass...
