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Sneak Peek: Future of Coral Reefs in an Acidifying Ocean

Thu, 08/02/2012 - 4:37pm
Laetitia Plaisance is a marine biologist who received her doctor of philosophy degree from the university of Perpignan in France.…

Carbon Dioxide Volcanic Seep

Intense volcanic CO2 vents in Ili Ili Bua Bua, Normanby Island, Papua New Guinea.

MV Chertain Lab Boat

For three weeks, the MV Chertan is home-base for the scientific team and will be transformed in a laboratory to study the effect of the CO2 seeps on reefs.

A Healthy Coral Reef

A healthy coral reef far away from CO2 seeps where the pH is still unaffected

Monoculture of Boulder Corals

But closer to the CO2 seeps, the complex reef has been replaced by a “monoculture” of boulder corals.

Fragile Branching Corals in Acidic Water

Branching corals, because of their more fragile structure, struggle to live in acidified waters

Lonely Seagrass in Acidic Waters

Where the pH is the lowest, corals can no longer grow - sand, rubble and seagrasses replace the reef.

Dissolving Shell

The acidic waters from the CO2 seeps can dissolve shells and also make it harder for shells to grow in the first place.

Dissolving Coral Skeleton in Acidic Waters

Acidic waters are also able to completely dissolve coral skeletons.
Where the pH is the lowest, corals can no longer grow - sand, rubble and seagrasses replace the reef.
Where the pH is the lowest, corals can no longer grow - sand, rubble and seagrasses replace the reef.
Laetitia Plaisance

Scientists don’t often get the opportunity to travel through time. But nestled among the beautiful coral reefs of Papua New Guinea (PNG) is a place that provides a glimpse today of what could be the biggest future threat to coral reef survival: Ocean Acidification. Ocean acidification is occurring because the ocean has absorbed about a third of the carbon dioxide (CO2) released into the atmosphere from the burning of fossil fuels. That carbon is changing the chemistry of the ocean, making seawater more acidic. Reef biologists expect this to be a bigger and bigger problem as more and more CO2 enters the atmosphere.

Normanby Island is a kind of “time vortex” where we can witness how reefs might respond to acidifying oceans. Here cool carbon dioxide naturally bubbles out of volcanic cracks in the shallow sea floor. Away from the CO2 seeps the water has a pH that is normal for modern day oceans, but as you swim closer to the seeps the water gets more and more acidic. I was fortunate to join scientists from the Australian Institute of Marine Science who are using this natural pH gradient to peer into the future.

As I first plunge into this bubble bath I understand why they named the nearby village Ili Ili Bua Bua (Water Water Bubble Bubble in the local dialect). On the shallow seafloor, I am struck by the lunar underwater landscape- the coral reef looks like none other I have seen. Instead of the usually beautiful, lively, colorful and complex scenery that I have seen in other parts of the world, massive brownish boulder corals have colonized the sea floor as far as the eye can see. There is almost no trace of the fragile branching corals that are home to so many underwater creatures elsewhere. Even the abundant and colorful fish seem to have abandoned the place. Closer to the most intense vents where water is most acidic, corals have stopped growing altogether; they have been replaced by sand, rubble and algae beds.

Where have all the beautiful corals and fish gone? When the ocean absorbs all that CO2, either from seeps like the ones in PNG or from the atmosphere, it dissolves and combines with water molecules to form carbonic acid. Ocean acidification directly harms many species with a calcareous shell or skeleton, such as mollusks and corals, by lowering the availability of calcium carbonate that they need to build their homes and structures. But other organisms that shelter in corals reefs are also threatened. Think of the coral reef as an apartment block made of chalk and the acidifying seawater as vinegar -- when you pour vinegar over chalk, it dissolves away the walls of your apartment block, providing less and less livable area for the resident species. The result, especially when combined with bleaching from warming waters, could mean the collapse of coral reefs.

Here at Water Water Bubble Bubble, we can travel through time -- in a five minute swim we see the steps of reef acidification expected for the twenty-first century. These reefs beg the question - will we be able to control our CO2 emissions before the point of no return?

To see larger pictures check out the full slideshow

Editors note: Read more about coral reefs and how you can help them.

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Comments

pH

I am curious about the pH range. How much of a range exists? As a physician, I know a small decrease in blood pH from 7.4 to 7.1, can cause substantial problems in physiology. I would be surprised if it did not affect seas life in a similar manner.

re: pH

Hi Stephen,

According to a paper I found, surface ocean pH is estimated to have dropped from near pH 8.25 to near 8.14 between 1751 and 2004, representing an increase of almost 30% in "acidity" (H+ ion concentration).

It might not seem like a lot but, as you said, a small change in pH can mean a lot. Scientists are still working out how acidic the ocean has to be before corals, mollusks, and other shell-building organisms are no longer compatible with the ocean's chemistry.

Thanks for your comment and for visiting!

Normanby Island Seeps

Hello Bob,

Thank you for your comment.

It's indeed an amazing place to dive. The pictures in the slideshow were actually taken at Normanby Island (not Dobu) where two other seep sites have been discovered. Conditions are a little different there because there is no extremely intense vents like in Dobu. However, even if the Dobu vents close to the shores in very shallow water are indeed hot, the reef that we studied (3-4 meter depth) in the three different sites show NO elevation in temperature but do show a clear pH gradient. I invite you to read the following article with the first scientific results here: http://www.nature.com/nclimate/journal/v1/n3/full/nclimate1122.html
As you can see, data show clear correlation between reef framework degradation/modification, coral diversity, and pH.

I hope you enjoy it.

All the best,

Laetitia

Dobu Island Seeps

I know this site well and have dived it for 25 years. The reason corals do not grow close to the big vents is that the sea bed is HOT. There is a healthy and diverse coral reef growing, complete with a complement of fishes and other marine life with CO2 seeps bubbling through it a few metres from the big hot vents.

This story is pure alarmism, has no scientific merit and convinces me that the "scientists" working there are frauds.

Dobu Island Seeps

Cool. I wish some day I would visit the site.

Hi Bob, Thanks for reading

Hi Bob,

Thanks for reading and the comment. We'll check in with the author about your argument, although we suspect that the scientists also know about the heat and took that into account during their research.

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