ruby said:
The Observer, your opening post did not refer to a study, it had someone’s story about some research from 2013. You might want to have a look at the page on Scripps Institution of Oceanography site about the research on coral from 2013 and get back to us about what it says.
Ruby, perhaps you would like to borrow my glasses? The OP clearly refered to a study, and nowhere in the OP is the year 2013 mentioned.
take another look dear -
From: The_observer
ID: 799816
Subject: Increase in acidity may not be harmful to coral reefs after all
Increase in acidity may not be harmful to coral reefs after all
Phys.org http://phys.org/news/2015-11-acidity-coral-reefs.html
November 10, 2015 by Bob Yirka
A combined team of researchers affiliated with the Scripps Institution of Oceanography and the Bermuda Institute of Ocean Sciences has found, via a five year study, that increased ocean acidification may not pose the threat to coral reefs that scientists have thought. In their paper published in Proceedings of the National Academy of Sciences, the team describes their study and why they now believe that an increase in green house gas emissions many not have the devastating impact on coral reefs that most in the field have assumed would occur.
To better understand what might happen with coral reefs if more carbon dioxide makes its way into the oceans due to an increase of the gas in the atmosphere caused by human emissions, the researchers set up monitoring devices along a coral reef offshore from Bermuda—information from the sensors was monitored for five years (2007 to 2012). The team also had access to data from an ocean chemistry monitoring station approximately 80 kilometers from their study site.
The combined data offered a unique perspective on coral activity.
In studying the data, the researchers noticed that spikes of phytoplankton blooms occurred during 2010 and again in 2011—those blooms made their way to the coral reef offering more food than normal for the coral. The coral responded by growing which caused them to pull more alkaline carbonate from the surrounding water, making it more acidic. Eating more also resulted in the corals emitting more carbon dioxide into the water. The result was a big increase in acidity—+to levels higher than have been predicted for the future due to human emissions+—yet, the coral continued to flourish.
These observations contrast sharply with the prevailing view that an increase in acidity is harmful to coral—leading to death if it goes too far. But the levels seen by the researchers with this new effort suggest that is not the case at all, and therefore muddles theories regarding the impact on the oceans of higher levels of carbon dioxide and warmer temperatures.
Now the study (Shifts in coral reef biogeochemistry and resulting acidification linked to offshore productivity, Proceedings of the National Academy of Sciences (2015) is paywalled, but here’s an extract from the abstract that clearly states that the reefs undergo rapid, but natural fluxuations in pH.
“Here, in a 5-y study of the Bermuda coral reef, we show evidence that variations in reef biogeochemical processes drive interannual changes in seawater pH and Ωaragonite that are partly controlled by offshore processes. Rapid acidification events driven by shifts toward increasing net calcification and net heterotrophy were observed during the summers of 2010 and 2011, with the frequency and extent of such events corresponding to increased offshore productivity. These events also coincided with a negative winter North Atlantic Oscillation (NAO) index, which historically has been associated with extensive offshore mixing and greater primary productivity at the Bermuda Atlantic Time-series Study (BATS) site. Our results reveal that coral reefs undergo natural interannual events of rapid acidification due to shifts in reef biogeochemical processes that may be linked to offshore productivity and ultimately controlled by larger-scale climatic and oceanographic processes.
Now, Ruby, forget fish tank experiments and model forcast & consider real evidence gathered on real reefs; reefs undergo daily extremes of changes in pH which are natural and equal to, if not greater than, any expected change in pH by the year 2100
eg
High-Frequency Dynamics of Ocean pH: A Multi-Ecosystem Comparison
Hofmann et al
http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0028983
some extracts from the study
The effect of Ocean Acidification (OA) on marine biota is quasi-predictable at best. While perturbation studies, in the form of incubations under elevated pCO2, reveal sensitivities and responses of individual species, one missing link in the OA story results from a chronic lack of pH data specific to a given species’ natural habitat.
Here, we present a compilation of continuous, high-resolution time series of upper ocean pH, collected using autonomous sensors, over a variety of ecosystems. These observations reveal a continuum of month-long pH variability with standard deviations from 0.004 to 0.277 and ranges spanning 0.024 to 1.430 pH units.
These biome-specific pH signatures disclose current levels of exposure to both high and low dissolved CO2, often demonstrating that resident organisms are already experiencing pH regimes that are not predicted until 2100.
the drive to forecast the effects of anthropogenic ocean acidification (OA) on marine ecosystems and their resident calcifying marine organisms has resulted in a growing body of research. However, the emerging picture of biological consequences of OA – from data gathered largely from laboratory experiments – is not currently matched by equally available environmental data that describe present-day pH exposures or the natural variation in the carbonate system experienced by most marine organisms. Although researchers have documented variability in seawater carbonate chemistry on several occasions in different marine ecosystems, this variation has been under-appreciated in these early stages of OA research.
Specifically, laboratory experiments to test tolerances are often not designed to encompass the actual habitat exposure of the organisms under study, a critical design criterion in organismal physiology that also applies to global change biology
The salient conclusions from this comparative dataset are two-fold: (1) most non-open ocean sites are indeed characterized by natural variation in seawater chemistry that can now be revealed through continuous monitoring by autonomous instrumentation, and (2) in some cases, seawater in these sites reaches extremes in pH, sometimes daily, that are often considered to only occur in open ocean systems well into the future
Now relax Mrs Ruby & enjoy the interglacial.