Notice I said coral reefs of TODAY? I mean I know you are the world's foremost expert at everything, so certainly you should understand English, right?
Coral reefs today don't die in water with a ph of 8 and no amount of our CO2 is ever going to lower the ph of the ocean more than that.
Did the scientists have names?
Of course they do and the routinely find that the models upon which your doomsday cult thrives are dead wrong. For example:
BG - Abstract - Groundwater and porewater as major sources of alkalinity to a fringing coral reef lagoon (Muri Lagoon, Cook Islands)
Natural variation, and the capacity to adapt to ocean acidification in the keystone sea urchin Strongylocentrotus purpuratus - Kelly - Global Change Biology - Wiley Online Library
Vogt, M., Steinke, M., Turner, S., Paulino, A., Meyerhofer, M., Riebesell, U., LeQuere, C. and Liss, P. 2008. Dynamics of dimethylsulphoniopropionate and dimethylsulphide under different CO2 concentrations during a mesocosm experiment. Biogeosciences 5: 407-419.
Hughes, T.P., Baird, A.H., Dinsdale, E.A., Moltschaniwskyj, N.A., Pratchett, M.S., Tanner, J.E. and Willis, B.L. 2012. Assembly rules of reef corals are flexible along a steep climatic gradient. Current Biology 22: 736-741.
What was done
To explore this subject in more detail, Hughes et al. applied a "rigorous quantitative approach to examine large-scale spatial variation in the species composition and abundance of corals on mid-shelf reefs along the length of Australia's Great Barrier Reef, a biogeographic region where species richness is high and relatively homogeneous." More specifically, they say they used "a hierarchical, nested sampling design to quantify scale-dependent patterns of coral abundances [for] five regions of the Great Barrier Reef [that they] sampled from north to south, each 250-500 km apart." Altogether, they thus identified and measured a total of 35,428 coral colonies on 33 reefs, categorizing each colony they encountered (including the majority of species that are too rare to analyze individually) into "ecologically relevant groups depending on their physiology, morphology and life history."
What was learned
The seven scientists report that the diverse pool of species they examined along the latitudinal gradient of the Great Barrier Reef "can assemble in markedly different configurations across a wide range of contemporary environments." With respect to temperature, for example, they indicate that "the geographic ranges of 93% of the 416 coral species found on the Great Barrier Reef extend northwards toward the equator (e.g., to Papua New Guinea, the Solomon Islands, and/or the Indonesian archipelago)," while "46% are also found in colder conditions further to the south." As for ocean acidification, they state that "globally, ocean surface pH has decreased by 0.1 unit since 1750 due to the uptake of atmospheric CO2, with a smaller 0.06 decline recorded for the tropics," citing Kleypas et al. (2006). In contrast, however, they report that contemporary variation in pH among various reef habitats on the Great Barrier Reef, as well as differences among short-term replicate measurements, span a range of 0.39 unit, from 8.37 to 7.98, citing Gagliano et al. (2010). And they rightfully note that this short-term and habitat-scale variability literally swamps that of latitudinal trends.
Thresher, R.E., Tilbrook, B., Fallon, S., Wilson, N.C. and Adkins, J. 2011. Effects of chronic low carbonate saturation levels on the distribution, growth and skeletal chemistry of deep-sea corals and other seamount megabenthos. Marine Ecology Progress Series 442: 87-99.
What was done
"To determine the sensitivity of corals and allied taxa to long-term exposure to very low carbonate concentrations," in the words of Thresher et al., they examined in detail "the depth distribution and life-history characteristics of corals and other shell-forming megabenthos along the slopes of deep-sea seamounts and associated structure in the SW Pacific," where the gradient of water chemistry ranged from super-saturated with respect to aragonite and high-magnesium calcite (HMC) to under-saturated, even with respect to calcite.
What was learned
The five researchers report that they "found little evidence that carbonate under-saturation to at least -30% affected the distribution, skeletal composition, or growth rates of corals and other megabenthos on Tasmanian seamounts." In fact, they found that "both solitary scleractinian corals and colonial gorgonians were abundant at depths well below their respective saturation horizons and appeared healthy," while HMC echinoderms were common to as deep as they sampled (4011 m), in water that was approximately 45% under-saturated. They also report that "for both anthozoan and non-anthozoan taxa, there was no obvious difference in species' maximum observed depths as a function of skeletal mineralogy." In other words, the community "was not obviously shifted towards taxa with either less soluble or no skeletal structure at increasing depth." And in light of these observations, they write that "it is not obvious from our data that carbonate saturation state and skeletal mineralogy have any effect on species' depth distributions to the maximum depth sampled," and they say that they also saw "little evidence of an effect of carbonate under-saturation on growth rates and skeletal features."
Commenting further on their findings, Thresher et al. write that "the observation that the distributions of deep-sea corals are not constrained by carbonate levels below saturation is broadly supported by the literature," noting that "solitary scleractinians have been reported as deep as 6 km (Fautin et al., 2009) and isidid gorgonians as deep as 4 km (Roark et al., 2005)." And they say that their own data also "provide no indication that conditions below saturation per se dictate any overall shifts in community composition."
As for why things were as they observed them to be, the researchers note, as highlighted by Cohen and Holcomb (2009), that one or more cell membranes may envelope the organisms' skeletons, largely isolating the calcification process and its associated chemistry from the bulk seawater, citing the studies of McConnaughey (1989), Adkins et al. (2003) and Cohen and McConnaughey (2003), which phenomenon could presumably protect "the skeleton itself from the threat of low carbonate dissolution." In addition, they note that "calcification is energetically expensive, consuming up to 30% of the coral's available resources, and that normal calcification rates can be sustained in relatively low-carbonate environments under elevated feeding or nutrient regimes," as described in detail by Cohen and Holcomb (2009), stating that the likelihood that "elevated food availability could compensate for the higher costs of calcification in heterotrophic deep-sea species appears plausible."
And it could go on ad nauseum...study after study after study demonstrating that the models that you warmist folks believe in so strongly are simply wrong.