Since the beginning
of the industrial revolution, the ocean has absorbed about 1/3 of CO2
emitted to the atmosphere from human activities. The ocean plays a vital role
to alleviate global warming caused by this greenhouse gas. However, as CO2
concentrations increase continuously in atmosphere, the absorptive amount of CO2
in ocean goes up dramatically. When CO2 dissolves in seawater, it
forms carbonic acid and increases the acidity of ocean. Ocean acidification and
its effects on marine biodiversity have been largely overlooked by mainstream
medias during the debate of climate change. In addition, the concern about
ocean acidification has often focused on its negative effects on coral reefs. However,
the broader impacts of acidic sea on marine organisms and ecosystems may be
much more significant.
The basic chemistry
of how an ocean becomes acidic is well understood. When CO2 dissolves
in
http://www.pmel.noaa.gov/co2/story/Ocean+Acidification |
seawater, it forms carbonic acid, which dissociates to bicarbonate and
hydrogen ions. Bicarbonate ions can further dissociate to carbonate and
hydrogen ions. According to NOAA, the more CO2 in the atmosphere,
the more CO2 is in the ocean. The increasing quantities of CO2
in seawater will drive the equilibrium of this chemical process to produce more
hydrogen ions and greatly decrease the pH in the ocean. This changing chemistry
in the ocean will put a great threat on marine plants or animals, whose shells
or skeletons are made up of calcium carbonate (CaCO3), since CaCO3
dissolves at certain lower pH level. What is more, it is much more difficult
for organisms to construct calcium carbonate shells under acidic condition.
Currently, the ocean tends to be corrosive to numerous marine organisms with
calcium carbonate covers.
The impacts of acidic ocean on
coral reefs have been studied thoroughly. Corals are composed of coral polyps,
which are covered by calcium carbonate secreted over time. Corals live with
algae (Zooxanthellae)
symbiotically, relying on the nutrients photosynthesized by the algae and
provide stable habitats for the algae. Corals face two threats from
acidification: First, coral reefs are very sensitive to temperature change. A
1-2℃ warmer maximum summer
temperature will lead to a phenomenon called “bleaching” which refers to the expelling
of symbiotic algae by coral which makes itself become translucent(Jones et al.,
2008). Secondly, increasing acidity decreases calcification rates of coral reefs,
which makes it grow slower and vulnerable to erosion. Both threats lead host
coral to decline or even die. However, the threats to coral reefs are not the
whole story. Coral reef ecosystems are one of the most biologically diverse
hotspots. They are also called the rainforests of the sea, since they cover only
2% of global surface but provide habitat for almost 25% of all marine species
and contain almost 40% of the whole world’s productivity (John et al.). Many
species such as sponges, mollusks, crustaceans are interconnected with coral
reefs. Any fluctuation-declining of corals will influence the abundance of
other species, especially who rely on coral for food and habitat.
https://web.duke.edu/nicholas/bio217/aer9/effects.htm
Ocean acidification will trigger a chain
reaction and alter the marine food web. Calcifying organisms that are protected
by carbonate shell or skeleton span the entire marine food web. Specifically,
many microscopic phytoplankton and zooplankton species form the base of this
food web. Phytoplankton have calcium carbonate shells outside to protect
themselves from predators such as ciliate protozoa. In recent studies, almost
all calcifying organisms decrease their ability to construct shells under
acidic seawater (Endo et al.,2013). These two photos compare the calcifying
rate of one phytoplankton called Gephyrocapsa
under current CO2 conditions and the expected higher CO2
conditions by the end of this century. Under the higher CO2
conditions, the calcifying rate decreases significantly by about 25% and shows clear
structural damage (Endo et al.,2013).
Nature 407, 364-367
Without protective
shells, phytoplankton will lose their physical function and be easily captured
by predators. Ciliate protozoa gorging on these weekened phytoplankton will flourish
at the expense of loss of other organisms in the food chain (Endo et al.,2013).
What is more, as the primary producer of marine system, unprotected phytoplankton
will lower the nutritional content available for organisms higher up in the
food chain due to their loss of organic carbon cover. Reduced primary
production quality leads to lower nutritional availability for zooplankton,
thereby lowering growth and reproduction rates of other organisms in the food
chain as there is less energy input for higher organisms (Potera, 2010).
Pteropods (a kind of zooplankton), also
called “sea butterflies” are important prey for many commercial fish species
such as the North Pacific salmon. A recent study shows that when a peteropod’s
shell is placed in seawater with the pH predicted for the year 2100, the shell
dissolves and disappears after just 45 days (Holland, 2007). Without a
protective shell, other non-calcifying organisms will out-compete the peteropods
for food and lead to change of prey-predator relationships. Some species may go
extinct without enough nutrition, others may become flourishing and invasive in
local environments. Current research shows that ocean acidification even
negatively affects commercial fisheries and shellfish industries. Due to lack
of nutrition, North Pacific salmons are smaller in size, and due to erosion of
acidic sea, west coast oysters have failed in both aquaculture and natural
development (Holland, 2007). The change of the marine food chain will
eventually affect the food security of humanity.
Ocean acidification not only indirectly
affects food web of marine organisms, but also directly affects their
physiological function. Acidic seawater disrupts normal biological mechanisms
that are vital for marine species survival and causes internal damage. For
marine animals in general, such as invertebrates or fish, lower pH may result
in acidosis or acidification of body fluids. These internal damages will lead
to reduced resistance to diseases, metabolic disorders, decreased reproductive
rates and depression in physical activity (Poertner etal.,2005). For instance,
squids require large amounts of
energy when they swim. Their energy-demanding
way of survival requires abundant supply of oxygen in the blood. However
acidosis negatively affects the transport of oxygen and leads to behavior
depression of squid. In another study from the University of Bristol, ocean
acidification can cause deafness in juvenile clownfish. Baby clownfish use both
hearing and olfactory senses to detect predator-rich coral reefs in order to
avoid capture. The researchers put clownfish in current seawater (390 ppmCO2)
and seawater with higher CO2 (900ppmCO2) to mimic emission
levels projected by 2100 if the emission rate is constant (Mundaya, 2009). In both
the hearing and olfactory sense tests, clownfish can detect and subsequently
swim away from the predator-rich coral reefs in current seawater, but baby fish
in 2100 seawater have no response to predator noise and cannot tell which
direction they should swim (Mundaya, 2009). According to this study, if we continue to
emit CO2 at current rate, the entire sensory system of clownfish
will lose effectiveness, making them more susceptible to predators and face
possible extinction. These disrupted physiological processes may
occur in other marine organisms and lead to a subsequent loss of biodiversity.
Podcast: Losing Nemo from CBC radio
Ocean acidification has great
impacts on marine biodiversity. These potential effects are not only limited in
erosion of coral reefs by dissolving their calcium carbonate shells, but have
broader impacts on disruption of biodiversity in the ocean. Acidic oceans will
directly alter the physiological function of certain marine species, disrupt
their sensory systems and depress behaviors; It will indirectly influence the
food resources in the ocean by altering marine food chain. However, these known
impacts are just one piece of the big puzzle of ocean acidification effects. More
experiment-related research is needed in order to fill the knowledge gap. At
the same time, everybody should be aware of the severe results that acidic
ocean will bring and change our lifestyle to reduce CO2 emission
daily. Go green with our transportation by using buses or bikes; Turn off the
lights when leaving an empty room; Save water by taking short showers instead
of baths… So start small and start now!
Citations:
Popular Media:
1. John Sibbick, Ocean Acidification
2. Jennifer S. Holland (November 2007)
Acid Threat. National Geographic.
Primary Literature:
1. Endo, H, T Yoshimura, T Kataoka, K Suzuki, BV
ELSEVIER SCIENCE, and Koji Suzuki.
"Effects of CO2 and Iron Availability on Phytoplankton and Eubacterial Community Compositions in the Northwest Subarctic Pacific."Journal of Experimental Marine Biology and Ecology, 439 (2013): 160-175.
2. Jones, A, R
Berkelmans, M. J. H. van Oppen, J Mieog, and W Sinclair. "A Community
Change
in the Algal Endosymbionts of a Scleractinian Coral Following a Natural Bleaching Event: Field Evidence of Acclimatization." Proceedings: Biological Sciences, 275.1641 (2008): 1359-1365.
3. Mundaya, Philip L. "Ocean
acidification impairs olfactory discrimination and homing ability of a marine
fish." Proceedings of the National Academy of Science. 106.6 (2009):
1848–1852 .
4. Potera, Carol. "MARINE and
COASTAL SCIENCE: Will Ocean Acidification Erode the Base of the Food
Web?."Environmental Health Perspectives, 118.4 (2010): A157.
5. Poertner, H.O., M. Langenbuch, and B. Michaelidis “
Synergistic effects of temperature extremes, hypoxia, and increases in Co2 on
marine animals” From earth history to
global change, Journal of
Geophysical Research-Oceans (2005): 110, C09S10, doi:10.1029/2004JC002561.
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