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Nighttime dissolution in a temperate coastal ocean ecosystem increases under ...
Anthropogenic emissions of carbon dioxide (CO2) are causing ocean acidification, lowering seawater aragonite (CaCO3) saturation state (Omega arag), with potentially substantial... -
Antarctic crustacean grazer assemblages exhibit resistance following exposure...
Anthropogenic atmospheric CO2 concentrations are increasing rapidly, resulting in declining seawater pH (ocean acidification). The majority of ocean acidification research to... -
Persistent natural acidification drives major distribution shifts in marine b...
This dataset has no description
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Effects of elevated CO2 and temperature on an intertidal meiobenthic community
In the near future, the marine environment is likely to be subjected to simultaneous increases in temperature and decreased pH. The potential effects of these changes on... -
Seawater carbonate chemistry and calcification rate in flume experiment
Ocean acidification (OA) poses a severe threat to tropical coral reefs, yet much of what is know about these effects comes from individual corals and algae incubated in... -
Reefs shift from net accretion to net erosion along a natural environmental g...
Coral reefs persist in an accretion-erosion balance and ocean acidification resulting from anthropogenic CO2 emissions threatens to shift this balance in favor of net reef... -
Secondary calcification and dissolution respond differently to future ocean c...
Climate change threatens both the accretion and erosion processes that sustain coral reefs. Secondary calcification, bioerosion, and reef dissolution are integral to the... -
Seaweed fails to prevent ocean acidification impact on foraminifera along a s...
Ocean acidification causes biodiversity loss, alters ecosystems, and may impact food security, as shells of small organisms dissolve easily in corrosive waters. There is a... -
Seasonality affects macroalgal community response to increases in pCO2
Ocean acidification is expected to alter marine systems, but there is uncertainty about its effects due to the logistical difficulties of testing its large-scale and long-term... -
Permeable coral reef sediment dissolution driven by elevated pCO2 and pore wa...
Ocean acidification (OA) is expected to drive the transition of coral reef ecosystems from net calcium carbonate (CaCO3) precipitating to net dissolving within the next century.... -
Growth response of an early successional assemblage of coralline algae and be...
The sustained absorption of anthropogenically released atmospheric CO2 by the oceans is modifying seawater carbonate chemistry, a process termed ocean acidification (OA). By the... -
Structural and functional vulnerability to elevated pCO2 in marine benthic co...
The effect of elevated pCO2/low pH on marine invertebrate benthic biodiversity, community structure and selected functional responses which underpin ecosystem services (such as... -
Seawater carbonate chemistry and net dissolution rate for experiment of Shira...
Acidification of the oceans by increasing anthropogenic CO2 emissions will cause a decrease in biogenic calcification and an increase in carbonate dissolution. Previous studies... -
Seawater carbonate chemistry and net ecosystem calcification and production i...
Net ecosystem calcification rates (NEC) and net photosynthesis (NP) were determined from CO2 seawater parameters on the barrier coral reef of Kaneohe Bay, Oahu, Hawaii.... -
Seawater carbonate chemistry, calcification and dissolution of a coral reef i...
In this study we investigated the relations between community calcification of an entire coral reef in the northern Red Sea and annual changes in temperature, aragonite... -
Seawater carbonate chemistry and community calcification near Lizar Island, 2011
It is predicted that surface ocean pH will reach 7.9, possibly 7.8 by the end of this century due to increased carbon dioxide (CO2) in the atmosphere and in the surface ocean.... -
Seawater carbonate chemistry and calcification during experiments with coral ...
Previous studies have demonstrated that coral and algal calcification is tightly regulated by the calcium carbonate saturation state of seawater. This parameter is likely to... -
Seawater carbonate chemistry and dissolution rates by boring microflora durin...
Eight-month-old blocks of the coral Porites lobata colonized by natural Hawaiian euendolithic and epilithic communities were experimentally exposed to two different aqueous pCO2... -
Seawater carbonate chemistry and community calcification during Miyako Island...
Coral reefs are characterized by enormous carbonate production of the organisms. It is known that rapid calcification is linked to photosynthesis under control of the carbonate... -
Seawater carbonate chemistry and community calcification during Shiraha coral...
Only about half of all the CO_2 that has been produced by the burning of fossil fuels now remains in the atmosphere. The CO_2 "missing" from the atmosphere is the subject of an...
