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Carbon Dioxide and Earth's Future Pursuing the ... - Magazooms

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www.co2science.org<br />

P a g e | 106<br />

When <strong>the</strong>se emissions estimates are transformed into reductions of oceanic pH, it can readily<br />

be seen in <strong>the</strong> following figure that Tans’ projected pH change at 2100 is far less than that of<br />

<strong>the</strong> IPCC. And Tans’ analysis indicates a pH recovery to values near those of today by <strong>the</strong> year<br />

2500, clearly suggesting that things are not <strong>the</strong> way <strong>the</strong> world’s climate alarmists make <strong>the</strong>m<br />

out to be, especially when it comes to anthropogenic CO2 emissions <strong>and</strong> <strong>the</strong>ir effects on <strong>the</strong><br />

air’s CO2 content <strong>and</strong> oceanic pH values.<br />

Ano<strong>the</strong>r reason to not jump<br />

on <strong>the</strong> ocean acidification<br />

b<strong>and</strong>wagon is <strong>the</strong> fact that,<br />

with more CO2 in <strong>the</strong> air,<br />

additional wea<strong>the</strong>ring of<br />

terrestrial carbonates likely<br />

will occur, which would<br />

increase delivery of Ca 2+ to<br />

<strong>the</strong> oceans <strong>and</strong> partially<br />

compensate for <strong>the</strong> CO2induced<br />

decrease in calcium<br />

carbonate saturation state.<br />

And as with all phenomena<br />

involving living organisms,<br />

<strong>the</strong> introduction of life into<br />

<strong>the</strong> acidification picture<br />

greatly complicates things,<br />

as several interrelated<br />

biological phenomena must<br />

also be considered; <strong>and</strong><br />

when <strong>the</strong>y are, it becomes<br />

much more difficult to draw<br />

such sweeping negative<br />

conclusions. In fact, as demonstrated in numerous reviews of <strong>the</strong> scientific literature, <strong>the</strong>se<br />

considerations even suggest that <strong>the</strong> rising CO2 content of earth’s atmosphere may well be a<br />

beneficial phenomenon with many positive consequences (Idso, 2009; Idso <strong>and</strong> Singer, 2009).<br />

As an example of this fact, <strong>the</strong> Center for <strong>the</strong> Study of <strong>Carbon</strong> <strong>Dioxide</strong> <strong>and</strong> Global Change<br />

(hereafter, <strong>the</strong> Center) maintains an online ocean acidification database that may be accessed<br />

free of charge at http://www.co2science.org/data/acidification/acidification.php, showcasing<br />

over 1100 experimental results on this topic from <strong>the</strong> peer-reviewed scientific literature (as of<br />

Jan 2011). Specifically, <strong>the</strong>ir Ocean Acidification Database is an ever-growing archive of <strong>the</strong><br />

responses of various growth <strong>and</strong> developmental parameters of marine organisms immersed in<br />

seawater at or near today’s oceanic pH level, as well as at levels lower than that of today. The<br />

measured parameters included in <strong>the</strong> database pertain to changes in calcification, metabolism,<br />

growth, fertility <strong>and</strong> survival; <strong>and</strong> <strong>the</strong> data are arranged by marine organism, accessible by<br />

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