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Ocean Acidification

A series of chemical reactions

Big Picture Stuff

  • The Earth exists in Harmony between plants and animals.
  • Plants breath’ in CO2 and ‘exhale’ O2
  • Animals breathe in O2 and exhale CO2

In the Beginning

  • When the Earth first formed the atmosphere was 25-50% carbon dioxide (CO2)
  • Plants emerged and converted the planet to an atmosphere of O2
  • All the CO2 created snowball Earth
  • Animals emerged and reconverted the atmosphere back to mainly CO2
  • Earth cycled between ‘tropical Earth’ and ‘ice ages’ till we reached a happy balance called the Holocene 11,000 years ago (we are in this now)
  • Humans have now started to alter the harmony between plants and animals

It All Comes Down to Carbon Dioxide (CO2)

  • Carbon Dioxide is the most important greenhouse gas, but there are others
  • Just like we saw in Earth’s cycles, more CO2 means higher temperatures
  • CO2 dissolves in the ocean like the fizz in a can of soda
  • CO2 reacts with water molecules producing carbonic acid
  • CO2 reacts with water molecules producing carbonic acid
  • The more acid in something the more acidic
  • Therefore more CO2 ends up making the ocean more acidic
  • Higher acidity = lowering the pH (the oceans pH specifically)
  • Since the Industrial Revolution, the pH of the ocean’s surface has dropped from 8.21 to 8.10
See Video

What the heck is pH?

  • pH of saltwater should be about 8.2 and freshwater is typically 6.5
  • pH of water is 7
  • When the pH is too acidic or too basic it interferes with the necessary chemical reactions
  • There is a lot more to it, but we don’t need to get into that
  • pH is a scale of how acidic or basic something is
  • 0 is a super strong acid, 7 is neutral, and 14 is the strongest base
  • Acid has lots of H+ (hydrogen ion)
  • Base or alkaline has lots of -OH (hydroxide ion) or they want a H+

What Does Carbon Have to Do With Acidification?

  • CO2 is normally in the atmosphere/air
  • CO2 dissolves in the ocean like the fizz in a can of soda
  • When CO2 is absorbed by seawater, a series of chemical reactions occur resulting in the increased concentration of hydrogen ions (H+)
  • Remember the hydrogen ions (H+) = more acidic

What Does Carbon Dioxide Have to Do With Acidification?

  • CO2 reacts with water molecules producing carbonic acid (H2CO3) a weak acid that breaks down (chemically called dissociates) into hydrogen ions (H+) and bicarbonate ions (HCO3) and therefore lowering the oceans pH (raising its acidity)
  • Think about if I threw stickers on the tables. Some would take the stickers, some would not, some would put the stickers on and then put them back….same is true of CO2
  • Since the Industrial Revolution, the pH of the ocean’s surface has dropped from 8.21 to 8.10
  • This is 30% increase in acidity (pH scale is not logarithmic)

So Where is All This Extra CO2 Coming From?

  • You may have guessed but burning fossil fuels like oil and coal
  • Fossil fuels contain are made of millions of plants and phytoplankton (plant plankton).
  • Those dead plants pulled carbon out of the atmosphere through photosynthesis over many millions of years (remember Earth’s’ warm/cool cycle)
  • When we burn them we are returning all that carbon back to the atmosphere 
  • Took millions of years to sequester and we are returning it in a few hundred

PETROLEUM & NATURAL GAS FORMATION

Tiny sea plants and animals died and were buried on the ocean floor. Over time, they were covered by layers of silt and sand.

Over millions of years, the remains were buried deeper and deeper. The enormous heat and pressure turned them into oil and gas.

Today, we drill down through layers of sand, silt, and rock to reach the rock formations that contain oil and gas deposits.

Our Planet Can Store Excess Carbon

  • Sinks are places that absorb CO2 from the atmosphere. 
  • Forests, soils, and the ocean are the largest sinks
  • Forest: The plants in forests absorb a lot of CO2 (about 16% annually)
  • Soil: CO2 is by plants sequestering the carbon in the soil. Peatland, wetlands, and permafrost are the best. (about 30% annually) 
  • Scientists lump forest and soils into the ‘land sink’
  • Ocean: this is the largest carbon sink (30-50% annually). This is mainly due to phytoplankton (the plant plankton that gave us oil in the first place)
  • They are developing technologies to capture carbon

Our Body, Our pH

  • Sometimes thinking about the big picture makes it harder, let’s be selfish 
  • Our human body has a natural pH of 7.34 to 7.4
  • If your body gets to 6.9, you go into a coma! That’s only a change of 0.44-0.5!
  • Remember the Oceans has changed it acidity from 8.21 to 8.10 over the past 260-150 years . That is a change of 0.11.
  • CO2 is a natural byproduct of our body 
  • Just like our planet we can become ‘sick’ from too much CO2
  • The main ways your body gets rid of excess CO2: lungs and kidneys 
  • Our body can store excess carbon dioxide in the bones aka carbon sinks. This is called our carbon sink. When we have chronic illnesses or certain types of diseases our body will slowly release from this carbon sink. Making you sicker.
  • When we get a virus like the flu, our body heats us to burn out the virus. Increases in heat lead to decreases in pH. The most obvious form of this is stomach gets more acidic aka you get a tummy ache 
  • So increase in heat = increase in acidity (decrease in pH)

Effects on Shell Builders in the Ocean

  • Floating in the ocean is a seawater soup of dissolved chemicals, ions, and other substances
  • Shelled animals like clams, crabs, snails, etc. ‘gobble up’ available carbonate ions (CO32-) and calcium ions (Ca+2) to create their strong shells (CaCO3)
  • When CO2 dissolved in the water it reacts with water to form carbonic acid (H2CO3). Which in turn generates bicarbonate (HCO3), carbonate (CO32-), and hydrogen ions (H+)
  • The hydrogen ions (H+) ‘steal’ and bond with the carbonate ions (CO32-), preventing the shellfish was creating CaCO3 needed for their shells
  • The more CO2 the more H+ in the water
  • Without CaCO3 shellfish are not able to grow as big and if they are larger they cannot maintain their ‘hard’ shells (interactive link)

Effects on Zooplankton

  • Zooplankton as a major link in the marine food chain
  • There are two major zooplankton that build shells of CaCO3
  • Their shells (and layers of dead shells) fall to the ocean floor and neutralize a lot of excess acid in the ocean
  • The pteropod or ‘sea butterfly’ is a tiny sea snail about the size of  small pea. 
  • They are critical in the marine food web being eaten by everything from krill to whales.
  • They have already been in severe levels in the Southern Ocean

Jellyfish Will Kill Us All

  • It is suspected that jellyfish will not be harmed by acidification
  • Jellyfish compete with fish and other predators for plankton (zoo and phyto)
  • Research has shown that warming ocean temperatures has increased their populations
  • Jellyfish may come to dominate ecosystems

Effects of Coral Reefs

  • Corals have a calcium carbonate skeleton that slowly grows every year.
  • The same way that shell are created using calcium carbonate (CaCO3) and obstructed by H+ ions is also occurring in corals
  • Corals are having stunted growth and difficulty maintain their skeleton
  • Coral larvae found difficulty finding a home (btw coral larvae can move)

Impact of Fish

  • The extra carbonic acid in the water is absorbed into the fishes blood resulting in acidosis
  • Acidosis (in humans) result in rapid, shallow breathing, confusion, fatigue, headaches, sleepiness, lack of appetite, jaundice, and increased heart rate. 
  • Fish have been seen not avoiding noisy predators, decreased swimming speed, confusion finding their home, and grow larger otoliths (responsible for balance), and decrease in smell

Effects on Plants and Algae

  • Ocean plants and algae may thrive under acidic conditions 
  • Coralline algae though has had a 92% drop
  • Coccolithophores had had an interesting study. A short term study found they were harmed. A long term 12 month study found they adapted and thrived
  • Kelp and algae farming absorb large amounts of carbon and may be used to mitigate OA

Impacts of Starfish and Urchins

  • These animals use the same CaCO3 to build their shell but the chemical mechanism is slightly different. Their skeleton is dissolved even more rapidly
  • Urchins have difficulty digesting food in high acidity

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