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Underway physical oceanography and carbon dioxide measurements during Healy c...
Cruise QC flag: B (see further details). -
BONUS INTEGRAL WINTER cruise on RV Aranda (28.02.-11.03.2019) for monitoring ...
The dataset includes the continuous water side pCO2/fCO2 measurements made by Finnish Meteorological Institute on BONUS INTEGRAL winter cruise on RV Aranda for monitoring the... -
Seawater carbonate chemistry and gastrovascular cavity pH, calcification of M...
Coral polyps have a fluid-filled internal compartment, the gastrovascular cavity (GVC). Respiration and photosynthesis cause large daily excursions in GVC oxygen concentration... -
Seawater carbonate chemistry and herbivory rates of Lacuna vincta grazing on ...
Acidification and deoxygenation are two consequences of climate change that also co-occur in eutrophied coastal zones and can have deleterious effects on marine life. While the... -
Seawater carbonate chemistry and antioxidant defences, oxidative stress of tw...
We collected samples for oxidative stress and antioxidants in a high CO2 mesocosm experiment for two weeks, focussing on two common crustacean copepods Calanus finmarchicus and... -
Seawater carbonate chemistry and growth rate, larval attachment of edible oys...
Unprecedented rate of increased CO2 level in the ocean and the subsequent changes in carbonate system including decreased pH, known as ocean acidification (OA), is predicted to... -
Seawater carbonate chemistry and neurobiological and behavioural responses of...
Cleaning interactions are textbook examples of mutualisms. On coral reefs, most fishes engage in cooperative interactions with cleaners fishes, where they benefit from... -
Seawater carbonate chemistry and chlorophyll a, primary productioin and algal...
A mesocosm experiment was conducted in Wuyuan Bay (Xiamen), China, to investigate the effects of elevated pCO2 on bloom formation by phytoplankton species previously studied in... -
Impact of ocean acidification in the metabolism and swimming behavior of the ...
Since the industrial revolution, [CO2]atm has increased from 280 µatm to levels now exceeding 380 µatm and is expected to rise to 730-1,020 µatm by the end of this century. The... -
PeECE III - Pelagic Ecosystem CO2 Enrichment Study, Raunefjord, Bergen, Norwa...
The effects of CO2-induced seawater acidification on plankton communities were also addressed in a series of 3 mesocosm experiments, called the Pelagic Ecosystem CO2 Enrichment... -
Physicochemical water conditions during laboratory incubation of European sea...
L = larvaeJ = juvenilesC = cold conditionedW = warm conditionedA = ambientSW = ambient sea water -
Underway physical oceanography and carbon dioxide measurements during TANGARO...
Cruise QC flag: D (see further details). The Fair Data Use Statement for SOCAT can be found at hdl:10013/epic.48576.d001 -
Underway physical oceanography and carbon dioxide measurements during TANGARO...
Cruise QC flag: D (see further details) -
Underway physical oceanography and carbon dioxide measurements during Tangaro...
Detailed metadata description of each cruise doi:10.1594/PANGAEA.769638 -
Seawater carbonate chemistry and metabolic rates, bloodbased metrics in newbo...
Anthropogenic ocean acidification (OA) is a threat to coral reef fishes, but few studies have investigated responses of high-trophic-level predators, including sharks. We tested... -
Seawater carbonate chemistry and carbonate load of seagrass leaves
Seagrass meadows play a significant role in the formation of carbonate sediments, serving as a substrate for carbonate-producing epiphyte communities. The magnitude of the... -
Seawater carbonate chemistry and coral-coral competition
As carbon dioxide (CO2) levels increase, coral reefs and other marine systems will be affected by the joint stressors of ocean acidification (OA) and warming. The effects of... -
Seawater carbonate chemistry and sperm physiology in Mytilus galloprovincialis
The ongoing increase of CO2 in the atmosphere is inducing a progressive lowering of marine water pH that is predicted to decrease to 7.8 by the end of this century. In marine... -
Seawater carbonate chemistry and foraminiferal calcification
The response of the marine carbon cycle to changes in atmospheric CO2 concentrations will be determined, in part, by the relative response of calcifying and non-calcifying... -
Seawater carbonate chemistry and physiology and extrapallial fluid pH, calci...
Increasing anthropogenic carbon dioxide is predicted to cause declines in ocean pH and calcium carbonate saturation state over the coming centuries, making it potentially harder...