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CLIMATE CHANGE. CHANGE III:
from 8400-8100 BP. The atmospheric CO2
content decreases concurrent with
increased solubility in the cooling ocean.
In comparison the ice cores at Taylor Dome
demonstrate nearly flat values. (Figure 3.4,
lower curve).
Further evidence of the variability of CO2
values has been provided in a review by
Beck (2007) of some 90,000 analytical
measurements conducted before 1958 and
dating back to the nineteenth century. The
CO2 show rather large variations, in
contrast to the ice core data’s flat and
invariant CO2 proxy data. Beck’s summary
of the analytical data documents a large
increase in CO2 values co-incident with
the warming observed from 1920 to 1940
(Figure 3.5). In general, this data is
rejected by IPCC but not on grounds of
analytical accuracy, which is excellent, but
because the values did not fit their
preconceived concepts. Beck’s review is
thorough and comprehensive, and
convincingly demonstrates significant
variability in atmospheric CO2 in contrast
to ice core data.
Although a great deal has been made of
the dangers of CO2 emissions, much of it
is nothing more than fear mongering. The
truth is that CO2 is highly beneficial to
the planet. The measurements at the
Mauna Loa recording station are
demonstrating an increase in amplitude
of the seasonal CO2 cycle (high in winter,
low in summer), which indicates that CO2
fertilization is expanding the biosphere
and, in fact, creating a negative feedback.
Plants use CO2 to produce the organic
molecules which forms their tissues.
Higher levels of CO2 in the air allows
plants to grow bigger, produce more
branches and leaves, expand their root
systems, and produce more flowers and
fruit (Idso, 1989). There is an extensive
amount of published data indicating the
growth enhancement provided by a 300
ppmv increase in atmospheric CO2.
(Poorter, 1993; Ceulmans and Mousseau,
1994; Wullschleger et al., 1995 and 1997).
Fertilization by CO2 causes plants to
produce fewer stomatal pores per unit
area of leaf and the pores are narrower.
This change reduces most plants’ rate of
water loss by transpiration allowing them
to withstand drought conditions more
effectively (Tuba et al., 1998; Idso and
Quinn, 1983).
Similarly in the oceans, CO2 fertilizes the
organisms at the base of the food chain.
The high solubility of CO2 in cold water
explains the rich organic life of the cold15
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