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Seawater carbonate chemistry and processes during experiments with phytoplank...
This dataset has no description
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Seawater carbonate chemistry and physiological data of the diatom Thalassiosi...
We comparatively investigated the physiological and transcriptional performances of a diatom Thalassiosira weissflogii acclimated to OA (pHt drop of 0.35–0.41) between day and... -
Seawater carbonate chemistry and skeletal isotopic composition and calcifying...
The Tara Pacifc expedition (2016–2018) provided an opportunity to investigate calcifcation patterns in extant corals throughout thePacifc Ocean. Cores from colonies of the... -
Seawater carbonate chemistry and coccolithophores and diatoms resilient to oc...
Here, we investigatethe impacts of moderate (~700 μmol/kg) and high (~2700 μmol/kg) limestone-inspired alkalinity additionson two biogeochemically and ecologically important... -
Seawater carbonate chemistry and kelp densities and coral coverages at three ...
Ocean warming is altering the biogeographical distribution of marine organisms. In the tropics, rising sea surface temperatures are restructuring coral reef communities with... -
Seawater carbonate chemistry and food web composition, productivity, and trop...
As human activities intensify, the structures of ecosystems and their food webs often reorganize. Through the study of mesocosms harboring a diverse benthic coastal community,... -
Effects of in situ CO2 enrichment on structural characteristics, photosynthes...
Seagrass is expected to benefit from increased carbon availability under future ocean acidification. This hypothesis has been little tested by in situ manipulation. To test for... -
Vanishing coccolith vital effects with alleviated carbon limitation
By recreating a range of geologically relevant concentrations of dissolved inorganic carbon (DIC) in the laboratory, we demonstrate that the magnitude of the vital effects in... -
The potential of ocean acidifi cation on suppressing larval development in th...
We evaluated the effect of pH on larval development in larval Pacific oyster (Crassostrea gigas) and blood cockle ( Arca inflata Reeve). The larvae were reared at pH 8.2... -
Seawater carbonate chemistry, length and survival of Inland silverside, Menid...
Absorption of anthropogenic carbon dioxide by the world's oceans is causing mankind's 'other CO2 problem', ocean acidification. Although this process will challenge marine... -
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 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 diatom Phaeodactylum tricornutum (CCMA 106) ...
CO2/pH perturbation experiments were carried out under two different pCO2 levels (39.3 and 101.3 Pa) to evaluate effects of CO2-induced ocean acidification on the marine diatom... -
Seawater carbonate chemistry and morphometric coordinates and morphology of t...
The world's oceans are slowly becoming more acidic. In the last 150 yr, the pH of the oceans has dropped by ~0.1 units, which is equivalent to a 25% increase in acidity.... -
Seawater carbonate chemistry and biological processes during experiments with...
Ocean acidification (OA) is believed to be a major threat for near-future marine ecosystems, and that the most sensitive organisms will be calcifying organisms and the... -
Seawater carbonate chemistry and biological processes during experiments with...
Anthropogenic elevation of atmospheric pCO2 is predicted to cause the pH of surface seawater to decline by 0.3-0.4 units by 2100 AD, causing a 50% reduction in seawater [CO3]... -
Seawater carbonate chemistry and processes during experiments with cyanobacte...
We investigated carbon acquisition by the N2-fixing cyanobacterium Trichodesmium IMS101 in response to CO2 levels of 15.1, 37.5, and 101.3 Pa (equivalent to 150, 370, and 1000... -
Seawater carbonate chemistry, pigments and biological processes during experi...
Previous studies have shown that increasing atmospheric CO2 concentrations affect calcification in some planktonic and macroalgal calcifiers due to the changed carbonate... -
Seawater carbonate chemistry and processes during experiments with coccolitho...
The formation of calcareous skeletons by marine planktonic organisms and their subsequent sinking to depth generates a continuous rain of calcium carbonate to the deep ocean and...
