-
Seawater carbonate chemistry and boron incorporation of planktic foraminifer ...
Culture experiments with living planktic foraminifers reveal that the ratio of boron to calcium (B/Ca) in Orbulina universa increases from 56 to 92 µmol mol-1 when pH is raised... -
Seawater carbonate chemistry and biological processes of oysters Crassostrea ...
Estuarine organisms are exposed to periodic strong fluctuations in seawater pH driven by biological carbon dioxide (CO2) production, which may in the future be further... -
Seawater carbonate chemistry and shell weights of Laternula elliptica, Yoldia...
Antarctic calcified macroorganisms are particularly vulnerable to ocean acidification because many are weakly calcified, the dissolution rates of calcium carbonate are inversely... -
Seawater carbonate chemistry and calcification, mass and shed rate of tropica...
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... -
Seawater carbonate chemistry, the abiotic conditions in the fluid surrounding...
This study investigated the effects of seawater pH (i.e., 8.10, 7.85 and 7.60) and temperature (16 and 19 °C) on (a) the abiotic conditions in the fluid surrounding the embryo... -
Seawater carbonate chemistry and benthic foraminifera Ammonia sp. mass, size,...
About 30% of the anthropogenically released CO2 is taken up by the oceans; such uptake causes surface ocean pH to decrease and is commonly referred to as ocean acidification... -
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... -
Neogloboquadrina pachyderma sinistralis shell weight and sediment age from Ei...
Sediment core ID GS06-144 09MC-D -
Seawater carbonate chemistry and Astrangia poculata mass and zooxanthellate d...
The effects of nutrients and pCO2 on zooxanthellate and azooxanthellate colonies of the temperate scleractinian coral Astrangia poculata (Ellis and Solander, 1786) were... -
Seawater carbonate chemistry, Acropora digitifera growth and skeletal U/Ca ra...
The impact of ocean acidification caused by the increasing atmospheric CO2 has been studied in marine calcifiers, including hermatypic corals. However, the effect of elevated... -
Seawater carbonate chemistry and biological processes of Amphisorus hemprichi...
Ocean acidification, which like global warming is an outcome of anthropogenic CO2emissions, severely impacts marine calcifying organisms, especially those living in coral reef... -
Seawater carbonate chemistry and weight of two Atlantic corals Favia fragum a...
Rising concentrations of atmospheric CO2 are changing the carbonate chemistry of the oceans, a process known as ocean acidification (OA). Absorption of this CO2 by the surface... -
Seawater carbonate chemistry and Emiliania huxleyi mass and size, 2011
About one-third of the carbon dioxide (CO2) released into the atmosphere as a result of human activity has been absorbed by the oceans, where it partitions into the constituent... -
Seawater carbonate chemistry, length, mass and otholith development of spiny ...
Determining which marine species are sensitive to elevated CO2 and reduced pH, and which species tolerate these changes, is critical for predicting the impacts of ocean... -
Seawater carbonate chemistry and biological processes of foraminifera, Globig...
Specimens of two species of planktic foraminifera, Globigerinoides ruber and Globigerinella siphonifera, were grown under controlled laboratory conditions at a range of... -
Seawater carbonate chemistry and biological processes during experiments with...
The effect of short-term (5 days) exposure to CO2-acidified seawater (year 2100 predicted values, ocean pH = 7.6) on key aspects of the function of the intertidal common limpet... -
Seawater carbonate chemistry and Bathymodiolus brevior shell variables near E...
Increasing atmospheric carbon dioxide levels are causing ocean acidification, compromising the ability of some marine organisms to build and maintain support structures as the... -
Seawater carbonate chemistry and Ruditapes decussatus biological processes du...
We investigated the effects of ocean acidification on juvenile clams Ruditapes decussatus (average shell length 10.24 mm) in a controlled CO2 perturbation experiment. The... -
Seawater carbonate chemistry and Globigerinoides sacculifer biological proces...
The effect of carbonate ion concentration ([CO3]) on calcification rates estimated from shell size and weight was investigated in the planktonic foraminifera Orbulina universa... -
Planktonic foraminifera shell counts and weights from Labrador Sea in the upp...
Counts of planktonic foraminifera shells in the upper samples of three sediment cores from the Labrador Sea: HU2008-029-004TWC, HU91-045-93BX and MD99-2227. Foraminifera shells...
