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Greening planetBy Dr J Floor Anthoni (2010) www.seafriends.org.nz/issues/global/climate5.htm (This chapter is best navigated by opening links in a new tab of your browser)
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In this chapter we will put some misunderstandings to rest, beginning by reviewing the ecology of carbon and how it recycles. Then we'll study where the carbon is found in ecosystems and how these ecosystems acquired it. Before reviewing some important findings, we'll review how scientific experiments are done and learn about their limitations.
On the Seafriends website we have quite extensively documented the geology, ecology and biology of soil and the world's ecosystems (see soil) in order to foster a thorough understanding necessary for combating soil loss (in quality and quantity), the world's foremost ecological problem. This educational resource now also serves to understand an important side of 'global warming'.
We are happy and fortunate that somewhere else exists a web site specialising in the science of CO2 fertilisation, complete with extensive data for many plant species. It is also scientifically independent and objective. So please continue your studies at www.co2science.org.
Carbon ecology
Carbondioxide is food for plants, like nothing else. While making live tissues through photosynthesis, they combine carbondioxide with water, simplistically as:: 6CO2 + 6H2O + Light => C6H12O6 (Glucose) + 6O2For making more complicated biochemical substances like proteins, also minerals are required like nitrogen (N), potassium (K), sulfur (S) and some twenty more. See the elements of life. But CO2 and water remain the most important ones. Of these two, water is the most abundant substance whereas CO2 the least abundant, by far. For instance, in the air around us, only one in 3000 molecules is CO2, and plants must be able to catch these, in competition with all other plants on Earth. No surprise then that CO2 is highly in demand, and higher concentrations of it promote plant growth like nothing else. |
To understand that plants live in a world where CO2 is scarce, these two diagrams provide an ecological explanation. The green S-curve is how a population grows in relation to its resources like food. First (on left), their world is unexploited and food is plentiful. so the population grows explosively (exponentially) until mid-way growth slows down as food becomes more scarce. As the population grows further, growth slows to a trickle until it stops for lack of food. If such a population is a warm-blooded species, the maximum population cannot reach the top of the curve because such species require much food to survive. However, cold-blooded species can survive better in the almost fully exploited world, and 'cold-blooded' species that do not even move, like plants, can survive and still grow in the grey band of an almost fully exploited resource. |
The red graph shows growth rate (horizontal) as a function of the use
of the resource (vertical). One can see that in the grey band, the growth
rate is severely limited by the scarcity of the resource. Move the black
arrow slightly down, and a large increase in growth rate follows. This
is again depicted in the diagram shown here.
The amount of fossil fuel burnt by humans has been increasing exponentially,
which means that annual emissions have been growing, and 57% of that is
consistently retained in air.
Does sequestration by
plants keep up with human emissions?
we've seen overwhelming evidence that plants sequester only 43% of human emissions, which was confirmed by a recent study of Ballantyne et al [1] who plotted the missing CO2 against total emissions. Their diagram shows CO2 emissions in red and plant sequestrations in black. Although plants capture only about half of increased emissions, they are doing so ever more progressively. Indeed, in the past 50 years, their uptake has even doubled rather than levelled off as was feared by warmists. [1] Ballantyne A P et al (2012): Increase in net carbon dioxide uptake by land and oceans during the past 50 years, Nature 488, 70-72. |
The
Carbon
Pipe concept
We've shown before that the idea of carbon reservoirs is perhaps inaccurate, and that carbon flows more like inside a pipe, where the flow is determined by pressure (concentration in air). One cannot talk about carbondioxide without looking at the full picture with all its pathways, and much of this remains unknown. Plants absorb the CO2 breathed out by animals (not much) and from decomposition (much). Most of this interchange happens nearby, in fact on the roots of land plants, and likewise for plankton. Thus carbondioxide cycles fastest outside the atmosphere. The imaginary carbon pipe also connects the land with the sea in such a way that during warm interglacials, carbon travels from sea to land and during the cold ice ages in the opposite direction. |
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Thus the main movement of carbondioxide happens as follows:
global warming => oceans expel CO2 => higher CO2 in air => CO2 absorbed by plants and soiland the man-made CO2 is just part of this very large shift in fertility. Let's just hope that it continues for a few more millennia, rather than reversing into the next ice age. The first thing to notice could well be a lowering of the CO2 concentration in the atmosphere. From there on, the world rapidly descends back into poverty and cold. In an ice age, life is brutal and short.
This rather complicated diagram brings together the main types of world vegetation (colours), their extents (vertical scale), their biomass above and under the ground (left columns; soil leftmost; canopy rightmost), and their productivities (righthand column). The quantities are expressed in petagram PgC which is identical to gigaton GtC. It can be seen that some ecosystems store more carbon underground than above (tundra, taiga, grassland), whereas others store more above than below (conifers, humid broad-leaved forests). Amazingly, their productivities are roughly equal once temperature suffices (tundra is too cold). The humid broad-leaved forest is the tropical rainforest, which eclipses all others. |
Finally, to show where the world's ecosystems are found, together with their soils, this diagram brings together the climate variables of temperature, rainfall and potential evapotranspiration. Starting from the left in the Arctic, the tundra's growth is severely hindered by permafrost. But as one goes southward, the temperature (red curve) rises quickly to allow for productivity in the taiga boreal forests. It crosses the rainfall curve (blue) where soils are deepest and agricultural productivity highest. This is also the most sustainable area on the planet. But from here on, rainfall quickly becomes insufficient for evapotranspiration, resulting first in dry grasslands (steppe) and then the desert. In desert soils, rainfall is even insufficient to wash out calcium compounds and other salts, which results in strata ('horizons') of salts, limestone and gypsum. |
Later came the conifers, now found naturally in the very cold regions of the boreal forests. They too react well.
Then came the leafy trees, shrubs and weeds with their wide leaves optimised for photosynthesis, together with their ability to drop leaves in response to frost or drought. All of these are powered by the C3 photosynthesis, which consists of three biochemical steps. They too react well.
Then arrived the most recent grasses (maize, sorghum, sugarcane, bamboo) powered by a new method of photosynthesis, the C4 process which happens in 4 steps, and which is able to capture CO2 more efficiently. They are about twice as efficient in converting sunlight, while needing four times less water. Photosynthesis in C3 plants converts 0.1-0.4 g CO2 with 1 kg water, whereas C4 plants convert 0.4-0.8 gram. However, a higher temperature is also needed. Thus C4 plants are found mainly in warm areas, even though plant breeding has extended their temperature range. Not surprisingly, they do not react as well, because they are already better than others at capturing CO2.
To complete the list, there are also plants powered by the Crassulean
Acid Metabolism CAM photosynthesis (cacti, succulents, agaves,
lilies, bromeliads, orchids, euphorbia, geraniums) which enables them to
store CO2 at night for delayed photosynthesis by day. In this manner they
can close their water pores during the day, while opening up at night.
Such plants grow rather slowly but resist dry climates.
During the night, CO2 is absorbed and converted into chemical storage
as oxaloacetic acid and then as malate. During the day, these compounds
are converted and normal C3 photosynthesis takes place, with the
plant's leaf pores closed to prevent unnecessary evaporation. They use
a minimum of water.
Read more in soil/fertility.
But before we do so, a general comment of disenchantment. All these experiments look only at INCREASED carbondioxide levels, and NONE have looked at DECREASED levels, which is entirely unscientific. Thus ALL carbondioxide enrichment experiments so far are POLITICALLY or INDUSTRIALLY driven. Real science would have studied the whole gamut (reach) of CO2.
We can now split plant growth experiments into separate categories:
This
graph shows the results of one of the few experiments carried out over
a long time period, with sour orange trees at ambient CO2 and enriched
by +300ppm. The trees growing in nearly twice the concentration, consistently
outperform the controls at ambient CO2 by almost 100%, particularly towards
the end of the series. The graph does little justice to the visual side
of the experiment, because if one increases its wood consistently twice
each year, the difference with their controls becomes very large over time.
Location: Maricopa, Arizona.
Paradoxically, the authors state that "Carbon dioxide fertilization increases plant water use efficiency, which may help explain why the desert ecosystems responded more dramatically than other ecosystems." http://ag.arizona.edu/pubs/natresources/az1395.pdf |
The plant growth experiments unanimously agree that:
Whereas
plants cultivated in optimum conditions benefit substantially from elevated
levels of CO2 (blue curve), an overwhelming number of studies have shown
that stressed plants which are limited in one or more resources (water,
temperature, nutrients, light, herbicides, etc), benefit even more so (red
curve). Their growth rates indeed double for a doubling in CO2. Reader
please note that this is paradoxical because CO2 effects on growth do not
simply follow Liebig’s law of the minimum (Walter Larcher), and that these
studies confirm our exponential growth
paradigm above. What this means, is that elevated levels of CO2 have proved
to be extremely beneficial for the world. "Increasing atmospheric CO2 is
an unmixed blessing – it will bring currently unproductive land into use
and bring greater yield from existing land without additional fertilizer
use. This is a wonderful benefit in being able to feed an increasing world
population."
[1] CO2 Enrichment and Plant Nutrition. http://buythetruth.wordpress.com/2009/08/15/co2-enrichment-and-plant-nutrition/ |
There has been and still remains, a great reluctance on the part of many climatologists and ecologists, and especially environmentalists, to accept the concept that the rising level of atmospheric CO2 could be more beneficial than harmful for plant growth, food production, and the overall biosphere…Yet the scientific evidence is overwhelming. - Sylvan Wittwer
ancient species
Sago Palm Cycas revoluta Water Fern Azolla pinnata Fern, Tropical Pyrrosia piloselloides . |
+300ppm enriched
+172% +54% +78% . |
comments
. +90% at +600ppm . . |
conifer species
European larch Larix decidua Douglas Fir Pseudotsuga menziesii Spruce various Picea spp Pine various Pinus spp |
+300ppm enriched
+140% +10% +38% +22 to +38% |
comments
. . no reaction to higher CO2 P.eldarica +150%; P.mercus +200% |
broadleaf tree species (C3)
Various Acacia spp Aspen Populus spp Beech Fagus spp Birch Betula spp Gum trees Eucalyptus spp Ash species Fraxinus spp Tropical Savanna Tree Kielmeyera coriacea Maple various Acer spp Oak various Quercus spp |
+300ppm enriched
+71 to +100% +29 to 58% +24 to +88% +15 to 34% +46 to 130% +13 to 33% +88% +30 to +95% +38 to 110% |
comments
. . American beech responds better . . . . . large variation between species |
grain species (C3)
Oats Avene spp Barley Hordeum vulgare Rice Oryza sativa Common Wheat Triticum aestivum |
+300ppm enriched
+23 to +33% +38% +34% +32% |
comments
. . +141% at +600ppm. Most important food crop reacts little to higher CO2 |
C4 grasses species
various permanent grassland species Johnsongrass Sorghum halepense Sugarcane Saccharum officinarum Corn Zea mays |
+300ppm enriched
+20 to +65% 0 to +13% +34% +21% |
comments
. reacts poorly . 33% at +600ppm |
fruit species
orange trees Citrus spp Grapevine, Common Vitis vinifera Olive Tree Olea europaea Peach Tree Prunus persica |
+300ppm enriched
+30 to +60% +29% +35% +28% |
comments
. . . . |
vegetable (leaf) species
Peanut Arachis hypogaea Various beans Phaseolus spp Mustard, oilseed, broccoli Brassica spp Cucumber cucumis spp Soybean Glycine max Garden Lettuce Lactuca sativa Cultivated Tobacco Nicotiana tabacum Tomato Solanum lycopersicum |
+300ppm enriched
+60% +50 to 70% +28 to 56% +50% +47% +18% +60% +150% |
comments
. do not respond to higher CO2 do not respond to higher CO2 . +61% at +900ppm +115% at +900ppm . +53% at +600ppm! |
root crop species
Carrot Daucus carota Cassava Manihot spp Sweet Potato Ipomoea batatas Potato, White Solanum tuberosum |
+300ppm enriched
+78% +88% +33% +30% |
comments
. . +148% at +600ppm!! +71% at +900ppm |
desert species
various Agave spp . |
+300ppm enriched
+30 to +35% . |
comments
. . |
Most annual 'weeds' react vigorously, up to +460%. Weeds are species
that grow fast, reproduce profusely but live short lives.
Most human food crops react very positively, a huge benefit for growing
populations.
Water Fern Azolla pinnata +54%. Reacts vigorously to higher
concentrations. Azolla is an important fertiliser of rice paddies.
White Clover Trifolium repens +65%. An important fertiliser
of grasslands.
Water Hyacinth, Common Eichhornia crassipes +50%. A pest growing
in waterways.
Wild Spikenard Hyptis suaveolens +1700%. The winner? Pignut
or bushmint, a tropical noxious plant with antibacterial properties.
In glasshouses, flowers are grown in very high CO2 concentrations of
+900ppm, with medium response.
http://co2science.org/data/plant_growth/dry/dry_subject.php
for more data and details
Various notes
Finally various notes as a 'rats and mice' selection. |
From the literature
Hundreds of studies and extensive research conclusively show the link between CO2 levels and plant growth. Using a conservative estimate for the range of the recent atmosphere, for every 10 ppm (parts per million) that CO2 increases, plant growth increases roughly 1%. This varies from species to species and with other conditions/nutrients needed for growth. With CO2 levels rising from 280 ppm to 390 ppm (+110 ppm) since the Industrial Revolution, this equates to an 11% increase in plant growth. [Note. Since the beginning of the Green Revolution (1960), CO2 increased by 60ppm, accounting for 6% increase in plant growth and crop productivity. It could well be that new crops, more fertilisation and more irrigation did little compared to the concurrent increase in CO2] The carbon:nitrogen ratio of leaves of plants is usually increased under CO2 enrichment. Plants may acclimate to elevated CO2 by requiring less rubisco and photo-synthetic apparatus, which would lead to lower nitrogen contents. The overall change in C:N ratios is governed both by increases in structural and non-structural carbohydrates, and by decreases in protein content. However, seed nitrogen content is little affected (Allen et al., 1988). Water-use efficiency (WUE) (ratio of CO2 uptake to evapotranspiration) will increase under higher CO2 conditions. This increase is caused more by increased photosynthesis than it is by a reduction of water loss through partially closed stomata. Thus, more biomass can be produced per unit of water used, although a crop would still require almost as much water from sowing to final harvest. If temperatures rise, however, the increased WUE caused by the CO2 fertilization effect could be diminished or negated, unless planting dates can be changed to more favourable seasons. The direct effect of increasing temperatures across the range of 28 to 35°C appears to increase transpiration rate about 4 to 5% per °C, based on both experimental and modelling studies (Allen, 1991). This is in close agreement with the rise in saturation vapour pressure of about 6% per °C. Allen et al. (1985) |
For extensive documentation of scientific articles and experimental
data, please refer to the excellent and objective web site co2science.org.