Shell-Shocked Presentations
Causes of Ocean Acidification
Google Definition: “absorption of excess atmospheric carbon dioxide by the ocean”
Lead to lower PH levels,Carbonate Depletion,ocean warming, and nutrient pollution
When CO2 dissolves in seawater (H2O), it forms carbonic acid (H2CO3). This compound breaks apart, releasing hydrogen ions (H+) and bicarbonate ions (HCO3-)
Increasing carbon emissions have caused a jump in ocean acidification over the last few decades
Primary causes include burning of fossil fuels, deforestation and land use changes, and industrial production like cement production.
CO2 + H20= H2CO3
Past and Current Trends in CO2
Carbon dioxide have increased drastically due to large burning of fossil fuels, since 1700s
CO2 has fluctuated between 200 to 8,000 ppm in last 550 million years. Early to middle Paleozoic, late Triassic, early Jurassic: highest
Dropped after Cretacious and have not been as high as today in last 800,000 years
The current carbon dioxide levels in our atmosphere is currently about 385 ppm
Creatures Responding Well to Increased CO2
Creatures Not Responding Well to Increased CO2
Conches and Quahogs are fine up to 900 ppm but then have a very negative response
Mollusks- (oysters, clams, bay scallops) fared the worst under increased CO2 conditions
Organisms that live in warm-water environments are not as adapted to acidic conditions, so they tend to fare worse
Temperate Corals
Pencil Urchins
Predictions for Future
There will be a decrease in population of shelled creatures like crabs, snails, and clams.
Clams and snails will have weaker shells which will make it easier for them to be hunted by crabs.
Crab population will increase then decrease
Critical points in carbon dioxide levels causes a rapid decline in the calcification of temperate corals, pencil urchins, quahogs, and bay scallops.
Increased ocean acidification would make it harder for the ocean to absorb carbon, making it less effective as a carbon sink
It is still unsure exactly what would happen however, due to a poor understanding of how sea organisms make their shells and skeletons.