The Geological History of PlantsDawson, John William, Sir
Science
The Geological History of Plants
Dawson, John William, Sir
Paleobotany
has been preserved.
I am indebted to Dr. T. Sterry Hunt for the following very valuable
information, which at once places in a clear and precise light the
chemical relations of epidermal tissue and spores with coal. Dr. Hunt
says: "The outer bark of the cork-tree, and the cuticle of many if not
all other plants, consists of a highly carbonaceous matter, to which
the name of _suberin_ has been given. The spores of _Lycopodium_ also
approach to this substance in composition, as will be seen by the
following, one of two analyses by Duconi,[CJ] along with which I give
the theoretical composition of pure cellulose or woody fibre, according
to Payen and Mitscherlich, and an analysis of the suberin of cork, from
_Quercus suber_, from which the ash and 2·5 per cent of cellulose have
been deducted.[CK]
[CJ] Liebig and Kopp, "Jahresbuch," 1847-'48.
[CK] Gmelin, "Handbook," xv., 145.
---------+-----------+--------+------------
| Cellulose.| Cork. | Lycopodium.
---------+-----------+--------+------------
Carbon | 44·44 | 65·73 | 64·80
Hydrogen | 6·17 | 8·33 | 8·73
Nitrogen | .... | 1·50 | 6·18
Oxygen | 49·39 | 24·44 | 20·29
+-----------+--------+------------
Total | 100·00 | 100·00 | 100·00
---------+-----------+--------+------------
"This difference is not less striking when we reduce the above centesimal
analyses to correspond with the formula of cellulose, C{24}H{20}O{20},
and represent cork and _Lycopodium_ as containing twenty-four equivalents
of carbon. For comparison I give the composition of specimens of peat,
brown coal, lignite, and bituminous coal:[CL]
[CL] "Canadian Naturalist," vi., 253.
Cellulose C{24}H{20}O{20}
Cork C{24}H{18-2/10}O{6-7/10}
Lycopodium C{24}H{19-4/10}NO{5-6/10}
Peat (Vaux) C{24}H{14-4/10}O{10}
Brown coal (Schröther) C{24}H{14-3/10}O{10-6/10}
Lignite (Vaux) C{24}H{11-3/10}O{6-4/10}
Bituminous coal (Regnault) C{24}H{10}O{3-3/10}
"It will be seen from this comparison that, in ultimate composition, cork
and _Lycopodium_ are nearer to lignite than to woody fibre, and may be
converted into coal with far less loss of carbon and hydrogen than the
latter. They in fact approach closer in composition to resins and fats
than to wood, and, moreover, like those substances repel water, with
which they are not easily moistened, and thus are able to resist those
atmospheric influences which effect the decay of woody tissue."
Public-domain text, read in full here on John Shaqi.
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