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Immunology of pacific oysters experiment
This dataset has no description
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Survival log of pacific oysters experiment
This dataset has no description
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(Table 4) In situ methane concentrations (Cm), amount of dissolved methane an...
C = Core length, C AOM = core length below AOM zone, GH = gas hydrate, vol = volume, ps = pore space and cv = core volume. * This gas:water ratio of 132/1 is in between the... -
(Table 11) Shell characteristics of recent Calyptogena species
This dataset has no description
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(Table 5) Gas and gas hydrate contents in pressurized cores taken from the Ha...
SZ, sulfate zone. Proportion free gas in vol % of total gas volume (Vtg). The extent of analytical uncertainties is discussed in section 3.4.2. -
(Table 5) Unit-specific lengths (LsUx), pore fluid volumes (VpfUx), pore flui...
a assuming average sediment porosities Ø of 0.85 (Unit 1), 0.72 (Unit 2), and 0.61 (Unit 3), respectively, according to data provided by Haeckel et al. (2008) and Reitz et al.... -
Population density of mesozooplankton during POLARSTERN cruise ANT-X/6
This dataset has no description
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ICEFLUX allometric measurements of polar zooplankton and fish
This dataset summarizes allometric measurements on zooplankton and nekton species performed in the framework of the Dutch and German ICEFLUX projects. Measurements were... -
Seawater carbonate chemistry and skeletal mineralization of a marine fish
Ocean acidification and warming are known to alter, and in many cases decrease, calcification rates of shell and reef building marine invertebrates. However, to date, there are... -
Morphometry of cold-water coral mounds along the northern Moroccan Atlantic m...
Coral mounds formed by framework-forming cold-water corals pierce the seabed along most continental margins of the Atlantic Ocean and new sites are continuously being... -
Simulated leakage of high pCO2 water negatively impacts bivalve dominated inf...
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... -
Stable isotope analysis of jellyfish in Kiel Fjord, Western Baltic Sea during...
A temporal change in stable isotope (SI) composition of jellyfish in the Kiel Fjord, Western Baltic Sea, was documented by analyzing delta13C, delta15N and delta34S of bell... -
The impact of ocean acidification and warming on the skeletal mechanical prop...
Increased atmospheric CO2 concentration is leading to changes in the carbonate chemistry and the temperature of the ocean. The impact of these processes on marine organisms will... -
Temperature, length and width of Tuberculodinium vancampoae (the resting cyst...
Cyst forming dinoflagellates are useful in reconstructing past environments. For accuracy it is essential to know how environmental parameters such as salinity, temperature and... -
Laboratory measurements of food consumption and preference in Haliotis squama...
To test whether food consumption in Haliotis squamata is a function of temperature (Experiment 1), we produced agar-pellets containing Ulva lactuca powder (Xi'an XiaoCao... -
Seawater carbonate chemistry and Oikopleura dioica growth dynamics in mesocos...
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... -
Individual-based landscape and environmental factors and ranavirus epidemiolo...
This dataset has no description
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Fig. 4, Fig. S4 and Fig. S5b,c,d - Larval performance of F1 and F2 animals ex...
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... -
Seawater carbonate chemistry and fish hearing
Humans are rapidly changing the marine environment through a multitude of effects, including increased greenhouse gas emissions resulting in warmer and acidified oceans.... -
Seawater carbonate chemistry and shell morphometrics during CO2 acidified sea...
Seawater changing chemistry has consequences on coastal ecosystems and their living resources. Future projections suggest the pH could drop 0.2-0.3 pH units by the year 2100...