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Differential acid-base regulation in various gills of the green crab Carcinus...
Euryhaline decapod crustaceans possess an efficient regulation apparatus located in the gill epithelia, providing a high adaptation potential to varying environmental abiotic... -
Ocean acidification mediates photosynthetic response to UV radiation and temp...
Increasing atmospheric CO2 concentration is responsible for progressive ocean acidification, ocean warming as well as decreased thickness of upper mixing layer (UML), thus... -
Seawater carbonate chemistry and early development of the sea urchin Lytechin...
Land-based aquaculture facilities often utilize additional bicarbonate sources such as commercial sea salts that are designed to boost alkalinity in order to buffer seawater... -
Growth and photosynthesis of a diatom Cylindrotheca closterium grown under el...
The combination of elevated CO2 and the increased acidity in surface oceans is likely to have an impact on photosynthesis via its effects on inorganic carbon speciation and on... -
Metabolic costs of larval settlement and metamorphosis in the coral Seriatopo...
We tested the effects of pCO2 on Seriatopora caliendrum recruits over the first 5.3 d of post-settlement existence. In March 2011, 11-20 larvae were settled in glass vials (3.2... -
Seawater carbonate chemistry and calcification rates of Porites rus and Hydro...
Central to evaluating the effects of ocean acidification (OA) on coral reefs is understanding how calcification is affected by the dissolution of CO2 in sea water, which causes... -
The synergistic effects of increasing temperature and CO2 levels on activity ...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used to compute a complete and consistent... -
Rising CO2 and increased light exposure synergistically reduce marine primary...
Carbon dioxide and light are two major prerequisites of photosynthesis. Rising CO2 levels in oceanic surface waters in combination with ample light supply are therefore often... -
Reduced calcification decreases photoprotective capability in the Coccolithop...
Intracellular calcification of coccolithophores generates CO2 and consumes additional energy for acquisition of calcium and bicarbonate ions; therefore, it may correlate with... -
Future CO2-induced ocean acidification mediates the physiological performance...
The oceans take up more than 1 million tons of CO2 from the air per hour, about one-quarter of the anthropogenically released amount, leading to disrupted seawater chemistry due... -
Seawater carbonate chemistry and biological processes in experiments of the N...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used to compute a complete and consistent... -
Short-term metabolic and growth responses of the cold-water coral lophelia pe...
Cold-water corals are amongst the most three-dimensionally complex deep-sea habitats known and are associated with high local biodiversity. Despite their importance as ecosystem... -
Seawater carbonate chemistry and phytoplankton and eubacterial community comp...
On-deck CO2-Fe-manipulated incubation experiments were conducted using surface seawater collected from the Western Subarctic Gyre of the NW Pacific in the summer of 2008 to... -
(Table 1) 40Ar-39Ar incremental heating ages for ODP Hole 163-988A basalt and...
Results of 40Ar-39Ar Ar dating constrain the age of the submerged volcanic succession, part of the seaward-dipping reflector sequence of the Southeast Greenland volcanic rifted... -
Seawater carbonate chemistry and pteropod Limacina helicina antarctica shell ...
Anthropogenic ocean acidification is likely to have negative effects on marine calcifying organisms, such as shelled pteropods, by promoting dissolution of aragonite shells.... -
U-Th, 14C and d11B results for Holocene North Atlantic deep sea corals (Lophe...
Sediment Core MD01-2454G SW Rockall BANK 747m water depth on Logatechev Mounds (Core was taken during Marion Dufresne Cruise Geosciences 2001 at 55°31'N and 15°39'W)ENAM corals... -
Seawater carbonate chemistry and brown dottyback (Pseudochromis fuscus) movem...
Changes in olfactory-mediated behaviour caused by elevated CO2 levels in the ocean could affect recruitment to reef fish populations because larval fish become more vulnerable... -
Seawater carbonate chemistry and expression of hsp70, hsp90 and hsf1 in the r...
Ocean acidification is an ongoing threat for marine organisms due to the increasing atmospheric CO2 concentration. Seawater acidification has a serious impact on physiologic... -
Seawater carbonate chemistry and resource allocation and extracellular acid-b...
Anthropogenic CO2 emission will lead to an increase in seawater pCO2 of up to 80-100 Pa (800-1000 µatm) within this century and to an acidification of the oceans. Green sea... -
Seawater carbonate chemistry and crab Necora puber size and elements in tissu...
Ocean acidification (OA) is predicted to play a major role in shaping species biogeography and marine biodiversity over the next century. We tested the effect of medium-term...