CHAPTER VII

MINUTE STRUCTURE OF FOSSIL PLANTS—DIFFERENCES FROM LIVING ONES

We have seen in the last chapter that the main morphological divisions,

roots, stems, leaves, and fructifications, were as distinct in the Coal

Measure period as they are now. There is one structure, however, found in

the Coal Measure fossils, which is hardly paralleled by anything similar

in the living plants, and that is the fossil known as _Stigmaria_.

_Stigmaria_ is the name given, not to a distinct species of plant, but to

the large rootlike organs which we know to have belonged to all the

species of _Lepidodendron_ and of _Sigillaria_. In the frontispiece these

organs are well seen, and branch away at the foot of the trunk, spreading

horizontally, to all appearance merely large roots. They are especially

regularly developed, however, the main trunk giving rise always to four

primary branches, these each dividing into two equal branches, and so

on—in this they are unlike the usual roots of trees. They bore numerous

rootlets, of which we know the structure very well, as they are the

commonest of all fossils, but in their internal anatomy the main “roots”

had not the structure which is characteristic of roots, but were like

_stems_. In living plants there are many examples of stems which run

underground, but they always have at least the rudiments of leaves in the

form of scales, while the fossil structures have apparently no trace of

even the smallest scales, but bear only rootlets, thus resembling true

roots. The questions of morphology these structures raise are too complex

to be discussed here, and Stigmaria is only introduced as an example, one

of the very few available, of a palæozoic structure which seems to be of

a nature not clearly determinable as either root, stem, leaf, or

fructification. Among living plants the fine rootlike rhizophores of

Selaginella bear some resemblance to Stigmaria in essentials, though so

widely different from them in many ways, and they are probably the

closest analogy to be found among the plants of to-day.

The individual cells, we have already seen, are strikingly similar in the

case of fossil and living plants. There are, of course, specific

varieties peculiar to the fossils, of which perhaps the most striking

seem to be some forms of _hair_ cells. For example, in a species of fern

from the French rocks there were multicellular hairs which looked like

little stems of Equisetum owing to regular bands of teeth at the

junctions of the cells. These hairs were quite characteristic of the

species—but hairs of all sorts have always abounded in variety, so that

such distinction has but minor significance.

[Illustration: Fig. 48.—Stele of _Lepidodendron_ W, surrounded by a

small ring of secondary wood S]

As was noted in the table (p. 58) the only cell types of prime importance

which were not evolved by the Palæozoic plants were the wood vessels,

phloem and accompanying cells which are characteristic of the flowering

plants.

Among the fossils the vascular arrangements are most interesting, and, as

well as all the types of stele development noted in the previous chapter

as common to both living and fossil plants, there are further varieties

found only among the fossils (see fig. 50).

The simple protostele described (on p. 61) is still found, particularly

in the very young stages of living ferns, but it is a type of vascular

arrangement which is not common in the mature plants of the present day.

In the Coal Measure period, however, the protostele was characteristic of

one of the two main groups of ferns. In different species of these ferns,

the protostele assumed a large variety of shapes and forms as well as the

simple cylindrical type. The central mass of wood became five-rayed in

some, star-shaped, and even very deeply lobed, with slightly irregular

arms, but in all these cases it remained fundamentally monostelic.

Frequently secondary tissue developed round the protosteles of plants

whose living relatives have no such tissue. A case of this kind is

illustrated in fig. 48, which shows a simple circular stele surrounded by

a zone of secondary woody tissue in a species of _Lepidodendron_.

[Illustration: Fig. 49.—_Lepidodendron_, showing Part of the Hollow

Ring of Primary Wood W, with a relatively large amount of Secondary

Tissue S, surrounding it]

In many species of _Lepidodendron_ the quantity of secondary wood formed

round the primary stele was very great, so that (as is the case in higher

plants) the primary wood became relatively insignificant compared with

it. In most species of _Lepidodendron_ the primary stele is a hollow ring

of wood (cf. fig. 38, p. 62) round which the secondary wood developed, as

is seen in fig. 49. These two cases illustrate a peculiarity of fossil

plants. Among living ones the solid and the simple ring stele are almost

confined to the Pteridophytes, where secondary wood does not develop, but

the palæozoic Pteridophytes, while having the simple primary types of

steles, had quantities of secondary tissue, which was correlated with

their large size and dominant position.

[Illustration: Fig. 50.—Diagram of Steles of the English _Medullosa_,

showing three irregular, solid, steles A, with secondary thickenings S,

all round each. _a_, Small accessory steles]

Among _polystelic_ types (see p. 63) we find interesting examples in the

fossil group of the _Medulloseæ_, which are much more complex than any

known at present, both owing to their primary structure and also to the

peculiar fact that all the steles developed secondary tissue towards the

inner as well as the outer side. One of the simpler members of this

family found in the English Coal Measures is illustrated in fig. 50. Here

there are three principal protosteles (and several irregular minor ones)

each of which has a considerable quantity of secondary tissue all round

it, so that a portion of the secondary wood is growing in towards the

actual centre of the stem as a whole—a very anomalous state of affairs.

In the more complex Continental type of _Medullosa_ there are _very_

large numbers of steles. In the one figured from the Continent in fig. 51

but a few are represented. There is a large outer double-ring stele, with

secondary wood on both sides of it, and within these a number of small

steles, all scattered through the ground tissue, and each surrounded by

secondary wood. In actual specimens the number of these central steles is

much greater than that indicated in the diagram.

No plant exists to-day which has such an arrangement of its vascular

cylinder. It almost appears as though at the early period, when the

Medulloseæ flourished, steles were experimenting in various directions.

Such types as are illustrated in figs. 50 and 51 are obviously wasteful

(for secondary wood developing towards the centre of a stem is bound to

finally meet), and complex, but apparently inefficient, which may partly

account for the fact that this type of structure has not survived to the

present, though simpler and equally ancient types have done so.

[Illustration: Fig. 51.—Continental _Medullosa_, showing R, outer

double-ring stele with secondary wood all round it; S, inner stellate

steles, also surrounded in each case by secondary tissue]

Further details of the anatomy of fossils will be mentioned when we come

to consider the individual families; those now illustrated suffice to

show that in the Coal Measures very different arrangements of steles were

to be found, as well as those which were similar to those existing now.

The significance of these differences will become apparent when their

relation to the other characters of the plants is considered.

The fructifications, always the most important parts of the plant, offer

a wide field, and the divergence between the commoner palæozoic and

recent types seems at first to be very great. Indeed, when palæozoic

reproductive bodies have to be described, it is often necessary to use

the common descriptive terms in an altered and wider sense.

Among the plants of to-day there are many varieties of the simple

single-celled reproductive masses which are called _spores_, and which

are usually formed in large numbers inside a spore case or sporangium.

Among the higher plants _seeds_ are also known in endless variety, all of

which, compared with spores, are very complex, for they are many-celled

structures, consisting essentially of an embryo or young plant enclosed

in various protective coats. The distinction between the two is sharp and

well defined, and for the student of living plants there exists no

difficulty in separating and describing seeds and spores.

But when we look back through the past eras to palæozoic plants the

subject is not so easy, and the two main types of potentially

reproductive masses are not sharply distinct. The seed, as we know it

among recent plants, and as it is generally defined, had not fully

evolved; while the spores were of great variety and had evolved in

several directions, some of which seem to have been intermediate stages

between simple spores and true seeds. These seedlike spores served to

reproduce the plants of the period, but their type has since died out and

left but two main methods among living plants, namely the essentially

simple spores, the very simplicity of whose organization gives them a

secure position, and the complex seeds with their infinite variety of

methods for protecting and scattering the young embryos they contain.

Among the Coal Measure fossils we can pick up some of the early stages in

the evolution of the seed from the spore, or at least we can examine

intermediate stages between them which give some idea of the possible

course of events. Hence, though the differences from our modern

reproductive structures are so noticeable a feature of the palæozoic

ones, it will be seen that they are really such differences as exist

between the members at the two ends of a series, not such as exist

between unrelated objects.

Very few types can be mentioned here, and to make their relations clear a

short series of diagrams with explanations will be found more helpful

than a detailed account of the structures.

[Illustration: Fig. 52.—Spores

Each spore a single cell which develops with three others in tetrads

(groups of four). Very numerous tetrads enclosed in a spore case or

sporangium which develops on a leaflike segment called the sporophyll.

Each spore germinates independently of the others after being

scattered, all being of the same size. Common in fossils and living

Pteridophytes.]

[Illustration: Fig. 53.—Spores

Each a single cell like the preceding, but here only one tetrad in a

sporangium ripens, so that each contains only four spores. Compared

with the preceding types these spores are very large. Otherwise details

similar to above. Some fossils have such sporangia with eight spores,

or some other small number; living Selaginellas have four. In the same

cone sporangia with small spores are developed and give rise to the

male organs.]

[Illustration: Fig. 54.—“Spores” of Seedlike Structure

Out of a tetrad in each sporangium only one spore ripens, S in figure,

the others, _s_, abort. The wall of the sporangium, _w_, is more

massive than in the preceding cases, and from the sporophyll, flaps,

_sp f_, grow up on each side and enclose and protect the sporangium.

The one big spore appears to germinate inside these protective coats,

and not to be scattered separately from them. Only found in fossils,

one of the methods of reproduction in _Lepidodendron_. Other sporangia

with small spores were developed which gave rise to the male organs.]

[Illustration: Fig. 55.—“Seed”

In appearance this is like a seed, but differs from a true seed in

having no embryo, and is like the preceding structure in having a very

large spore, S, though there is no trace of the three aborting ones.

The spore develops in a special mass of tissue known as the nucellus,

_n_, which partly corresponds to the sporangium wall of the previous

types. In it a cavity, _p c_, the pollen chamber, receives the pollen

grains which enter at the apex of the “seed”. There is a complex coat,

C, which stands round the nucellus but is not joined to it, leaving the

space _l_ between them. Only in fossils; _Trigonocarpus_ (see p. 122)

is similarly organized. Small spores in fern-like sporangia, called

pollen grains.]

[Illustration: Fig. 56.—“Seed”

Very similarly organized to the above, but the coat is joined to the

nucellus about two-thirds of its extent, and up to the level _l_. In

the pollen chamber, _p c_, a cone of nucellar tissue projects, and the

upper part of the coat is fluted, but these complexities are not of

primary importance. The large spore S germinated and was fertilized

within the “seed”, but apparently produced no embryo before it ripened.

Small “spores” in fern-like sporangia form the pollen grains. Only in

fossils, _e.g._ Lagenostoma. (See p. 119.)]

[Illustration: Fig. 57.—Seed

Essentially similar to the preceding, except in the possession of an

embryo _e_, which is, however, small in comparison with the endosperm

which fills the spore S. The whole organization is simpler than in the

fossil _Lagenostoma_, but the coat is fused to the nucellus further up

(see _l_). Small “spores” form the pollen grains. Living and fossil

type, Cycads and Ginkgo.]

[Illustration: Fig. 58.—Seed

In the ripe seed the large embryo _e_ practically fills up all the

space within the two seed coats _c^1_ and _c^2_; endosperm, pollen

chamber, &c., have been eliminated, and the young ovule is very simple

and small as a result of the protection and active service of the

carpels in which it is enclosed. Small “spores” form the pollen grains.

Typical of living Dicotyledons.]

These few illustrations represent only the main divisions of an army of

structures with an almost unimaginable wealth of variety which must be

left out of consideration.

For the structures illustrated in figs. 54, 55, and 56 we have no name,

for their possible existence was not conceived of when our terminology

was invented, and no one has yet christened them anew with distinct

names. They are evidently too complex in organization and too similar to

seeds in several ways to be called spores, yet they lack the essential

element in a seed, namely, an embryo. The term “ovule” (usually given to

the young seed which has not yet developed an embryo) does not fit them

any better, for their tissues are ripened and hard, and they were of

large size and apparently fully grown and mature.

For the present a name is not essential; the one thing that is important

is to recognize their intermediate character and the light they throw on

the possible evolution of modern seeds.

A further point of great interest is the manner in which these “seeds”

were borne on the plant. To-day seeds are always developed (with the

exception of Cycas) in cones or flowers, or at least special

inflorescences. But the “seed” of _Lagenostoma_ (fig. 56), as well as a

number of others in the group it represents, were not borne on a special

structure, but directly on the green foliage leaves. They were in this on

a level with the simple sporangia of ferns which appear on the backs of

the fronds, a fact which is of great significance both for our views on

the evolution of seeds as such, and for the bearing it has on the

relationships of the various groups of allied plants. This will be

referred to subsequently (Chapter XI), and is mentioned now only as an

example of the difference between some of the characters of early fossils

and those of the present day.

It is true that botanists have long recognized the organ which bears

seeds as a modified leaf. The carpels of all the higher plants are looked

on as _homologous_ with leaves, although they do not appear to be like

them externally. Sometimes among living plants curious diseases cause the

carpels to become foliar, and when this happens the diseased carpel

reverts more or less to the supposed ancestral leaf-like condition. It is

only among the ancient (but recently discovered) fossils, however, that

seeds are known to be borne normally on foliage leaves.

From Mesozoic plants we shall learn new conceptions about flowers and

reproductive inflorescences in general, but these must be deferred to the

consideration of the family as a whole (Chapter XIII).

Enough has been illustrated to show that though the individual cells, the

bricks, so to speak, of plant construction, were so similar in the past

and present, yet the organs built up by them have been continually

varying, as a child builds increasingly ambitious palaces with the same

set of bricks.

Ancient Plants Being a Simple Account of the past Vegetation of the Earth and of the Recent Important Discoveries Made in This Realm of Nature · 第 3 / 15 章