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Benthic Chamber Lander stable isotope tracer experiments in the Cabo Verde Ab...
A total of five deployments of a Benthic Chamber Lander were conducted at the Cabo Verde Abyssal Plain (tropical East Atlantic) at about 4200 m water depth. The deployments took... -
Seawater carbonate chemistry and biomass, calcification and respiration rates...
The stratified Chilean Comau Fjord sustains a dense population of the cold-water coral (CWC) Desmophyllum dianthus in aragonite supersaturated shallow and aragonite... -
Seawater carbonate chemistry and growth, net calcification, respiration and g...
Understanding species' responses to upwelling may be especially important in light of ongoing environmental change. Upwelling frequency and intensity are expected to increase in... -
KOSMOS Bergen 2015 mesocosm study: C. harengus condition
To evaluate the influence of ocean acidification on predatory plankton, e.g. Hydrozoa and fish larvae as well as their interaction in complex natural communities, we deployed... -
Seawater carbonate chemistry and Hydrozoa, Copepoda abundances and biomasses,...
Anthropogenic CO2 emissions cause a drop in seawater pH and shift the inorganic carbon speciation. Collectively, the term ocean acidification (OA) summarizes these changes. Few... -
Water chemistry data from stream, groundwater, precipitation and porewater sa...
This dataset contains data on water chemsitry and stable water isotopes for samples collected in the Two-Boat Lake catchment, Western Greenland, during the period 2015-2019. The... -
Age Model of ODP Site 145-883
Here we present a new astronomically tuned age model for the late Pliocene section of ODP site 883. The astronomically tuned age model was developed by correlation of benthic... -
Foraminifera (living) count data containing infomation about the samples volu...
To obtain the foraminifera count data sediment (stained with Rose Bengal, a solution which causes living tissue to appear pink) was washed through a 63 µm sieve and then picked... -
Stacked Artemisia and xerophyte records from the Iberian Peninsula and Morocc...
This dataset has no description
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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... -
High-resolution census data of Extinction Group species in the Late Pliocene-...
This dataset has no description
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High-resolution census data of Extinction Group species in the Late Pliocene-...
This dataset has no description
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Compilation of trophic positions of marine biota from the central and Northea...
Fractional trophic levels (i.e., trophic positions) describe the position of organisms within food webs and help define their functional roles in ecosystems (Odum & Heald,... -
Annual SST estimates from the late Marine Isotope Stage 6 (140-135 kyr) and c...
This dataset has no description
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Abundance of Globigerinita glutinata and mixed-layer species at ODP Hole 130-...
This dataset has no description
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S10. Benthic foraminifer stable carbon and oxygen isotope data of ODP Site 20...
This dataset has no description
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S9. Benthic foraminifer stable carbon and oxygen isotope data of ODP Site 208...
Species code for benthic foraminifer:CBRA Cibicidoides bradyiiCCIC Cibicidoides cicatricosusCEOCEA Cibicidoides eoceanusCGRIM Cibicidoides grimsdaleiCHAVA Cibicidoides... -
S8. Benthic foraminifer stable carbon and oxygen isotope data of ODP Site 208...
Species code for benthic foraminifer:CBRA Cibicidoides bradyiiCCIC Cibicidoides cicatricosusCEOCEA Cibicidoides eoceanusCGRIM Cibicidoides grimsdaleiCHAVA Cibicidoides... -
Maximum annual SST estimates during the early LIG (129-124 ka; 189 sites)
Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES. -
SST estimates for the Last Interglacial (129-116 ka BP) during the months of ...
Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES.
