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Interstitial water geochemistry results of IODP Hole 381-M0078A
= value greater than highest calibration point. Type: IWRH = Rhizon, IWSQ = squeezed, IWrefMl = drilling mud residues from the core liner after core arrival on deck, IWrefDW =... -
Pore water and solid-phase depth profiles of manganese and alkalinity from se...
Porewater depth profiles of dissolved manganese and alkalinity from cores that were sliced and subsamples under a nitrogen atmosphere. Total Mn sediment concentrations from... -
Seawater carbonate chemistry and dry weight of 5 and 15 days-post-hatch Atlan...
Ocean acidification (OA), a direct consequence of increasing atmospheric CO2 concentration dissolving in ocean waters, is impacting many fish species. Little is known about the... -
Seawater carbonate chemistry and reproductive characteristics, Oxidative stre...
Fishes are currently facing novel types of anthropogenic stressors that have never experienced in their evolutionary history, such as ocean acidification. Under these stressful... -
Environmental and chemical measurements, and coral calcification rates in Ber...
Modern reef-building corals sustain a wide range of ecosystem services because of their ability to build calcium carbonate reef systems. The influence of environmental variables... -
Seawater pH predicted for the year 2100 affects the metabolic response to fee...
Widespread ocean acidification (OA) is transforming the chemistry of the global ocean, and the Arctic is recognised as a region where the earliest and strongest impacts of OA... -
Long-term acclimation to elevated pCO2 alters carbon metabolism and reduces g...
Increasing atmospheric CO2 levels are driving changes in the seawater carbonate system, resulting in higher pCO2 and reduced pH (ocean acidification). Many studies on marine... -
Hidden impacts of ocean acidification to live and dead coral framework
Cold-water corals, such as Lophelia pertusa, are key habitat-forming organisms found throughout the world's oceans to 3000 m deep. The complex three-dimensional framework made... -
Temperature dependence of CO2-enhanced primary production in the European Arc...
The Arctic Ocean is warming at two to three times the global rate and is perceived to be a bellwether for ocean acidification. Increased CO2 concentrations are expected to have... -
Performance of the Arctic calanoid copepods Calanus glacialis and C. hyperbor...
The sensitivity of copepods to ocean acidification (OA) and warming may increase with time, however, studies >10 days and on synergistic effects are rare. We therefore... -
Geochemistry at BIGO station AL355_376 on given timesteps
Iodide data need to be multiplied by factor 1.142 -
Geochemistry at BIGO station AL355_369 on given timesteps
Iodide data need to be multiplied by factor 1.142 -
Geochemistry at BIGO station AL355_358 on given timesteps
Iodide data need to be multiplied by factor 1.142 -
Geochemistry at BIGO station AL355_352 on given timesteps
Iodide data need to be multiplied by factor 1.142 -
Geochemistry at BIGO station AL355_348 on given timesteps
Iodide data need to be multiplied by factor 1.142 -
Geochemistry at BIGO station AL355_340 on given timesteps
Iodide data need to be multiplied by factor 1.142 -
Geochemistry at BIGO station AL355_337 on given timesteps
Iodide data need to be multiplied by factor 1.142 -
Geochemistry at BIGO station AL355_320 on given timesteps
Iodide data need to be multiplied by factor 1.142 -
Geochemistry at BIGO station AL355_376
Iodide data need to be multiplied by factor 1.142