NUTRIENT GASES. Gl 



tlie iiinleeules of carbon-dioxide in the air, we should oliserve how much faster they 

 are impelled towards the leaves and other green parts of plants, where the intense 

 craving for carbon is localized, than are the other constituent particles of the air. 

 This impulsion and influx lasts so long as the green cells are under the influence of 

 daylight. The flrst thing in the morning when the first ray of sunshine falls upon 

 a plant the protoplasts begin work in their little lalioratories decomposing carbonic 

 acid, and producing from it sugar, starch, and other similar organic compounds. 

 And it is not till the sun sets that this work is suspended, and the influx of carbon- 

 dioxide stopped till the following morning. 



The green plants that spenil all their lives under water are supplied with car- 

 bonic acid by the water surrounding their cells, which alwaj^s contains some of that 

 material. In the case of unicellular plants of this class, absorption of carlionic acid 

 takes place thi'ough the whole surface of the cell-membrane. Multicellular plants, 

 with their cells arranged in filameuts or plates, only take in carbonic acid through 

 those parts of the walls of their cells which are in iunnediate contact M'ith the 

 water. This applies also to submerged plants composed of several layers of cells 

 and of considerable dimensions. Thus, in plants of this kind, the cells in contact 

 with the water constitute the skin. They are always pressed closely togethei' 

 and squeezeil flat, are not thickened on the side e.xposed to the water, and are 

 united everywhere edge to edge leaving no gaps. But in the interior of these 

 water-plants large lacun;e and cavities are formed from earliest youth, owing to 

 the detachment of single rows of cells: and the spaces so formed are filled with 

 a quantity of nitrogen, oxygen, and carbon-dioxide, that is to say, with a gaseous 

 mixture not essentially diflerent from atmospheric air. Although this oi'ganiza- 

 tion may have as its primary object the reduction of the plant's weight as a 

 whole, it cannot be without a further importance inasmuch as carbonic acid can 

 be taken up from the air-spaces into ailjacent cells. But there is no doubt that, 

 even in this case (of water-plants provided with large internal air-ca\ities), 

 the chief absorption of carbonic acid is through the epidermis, or more precisely 

 through those walls of the epidermal cells which are in immediate contact with 

 the water. 



The carbonic acid taken up liy cells, wholl}' or partially immersed in water, 

 is either contained as such dissolved in the water3' medium, or occurs in com- 

 bination with calcium as bicarbonate of lime. Part of the carbonic acid in this 

 bicarbonate in aqueous solution is susceptible of being withdrawn by water-plants, 

 mono-carbonate of lime, which is insoluble in water, being then precipitated on 

 the cell-wall through which the re.st of the carbonic acid has passed into the 

 cell-interior. Accordingly, a large number of water-plants are foiind incrusted 

 with lime in both fresh and salt water. We shall return to this important pheno- 

 menon when we treat of the influence of living plants on that part of the environ- 

 ment which comes within their sphere of action for purposes of nutrition. 



Lithophytes obtain carbonic acid from the moisture deposited upon them from 

 the aqueous vapour in the atmosphere, and attract carbon-dioxide direct from the 



