Links With the Past in the Plant World — Key Ideas to Explore
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ed by the uplifting of piles of marine sediments. From Tertiary strata in the Isle of Wight, on the Hampshire coast, and in the London basin numerous fossil plants have been obtained, which afford convincing evidence of climatic conditions much more genial than those of the present day. The presence of palm leaves and of a wealth of other sub-tropical plants in Lower Tertiary beds in England reveals the existence of a flora differing considerably both from that in the uppermost Tertiary beds of Norfolk and from the modern British flora, but closely allied to the present Mediterranean flora.
The basaltic columns of the Giants' Causeway and of the Staffa Cave, and the terraced rocks which form so characteristic a feature in the contours of the Inner Hebrides, are portions of lava-flows, which in the early days of the Tertiary period were poured out over a wide area of land stretching from the north-east of Ireland, through the Western isles of Scotland, the Faroë islands, to Iceland and Greenland. While in this northern region volcanic activity was being manifested on a stupendous scale, a shallow sea extended over part of what is now the south-east of England in which was deposited a considerable thickness of sedimentary material derived from the neighbouring land. In this upraised sea-floor, known as the London clay, which is exposed in the Isle of Sheppey and in many other localities, numerous fossil fruits and fragments of wood occur in association with marine shells. The fact that many of the fruits were ripe at the time of their entombment led some eighteenth century writers to assign an autumn date to the universal deluge. One of the Sheppey fruits may be mentioned as an especially interesting sample of the early Tertiary flora, namely the genus Nipadites, so named from the very close resemblance of the fossils to the fruits of the existing tropical plant Nipa. _Nipa fruticans_, sometimes described as a stemless palm because of the absence of the erect stem which is usually a characteristic feature of palms, grows in brackish estuaries of many tropical countries (Fig. 5, A): it has long leaves not unlike those of the date-palm and bears clusters of fruits as large as a man's head; a single fruit is two or three inches long and its hard fibrous shell is characterised by four or five longitudinal ribs (Fig. 5, B). The fruits of Nipa, which may be carried a considerable distance by ocean-currents without losing the power of germination, are constantly found with other vegetable drift on the beaches of tropical islands. The discovery of fruits of Nipa (or Nipadites), hardly distinguishable from those of the existing species, in Tertiary beds in England, Belgium, in the Paris basin, and in Egypt affords a striking instance of changes in the geographical distribution of an ancient plant now restricted to warmer regions.
While the higher members of the Cretaceous system, as seen in the chalk cliffs and downs, represent the upraised calcareous accumulations on the floor of a fairly deep and clear sea, the lower members testify to shallower water within reach of river-borne sand and mud. 'During the Chalk period,' as Huxley wrote, 'not one of the present great physical features of the globe was in existence. Our great mountain ranges, Pyrenees, Alps, Himalayas, Andes, have all been upheaved since the chalk was deposited, and the Cretaceous sea flowed over the sites of Sinai and Ararat'(29).
The Wealden strata, at the base of the Cretaceous system, as seen on the Sussex coast, in parts of the Isle of Wight, in the Weald district of Kent and neighbouring counties, point to the existence of a lake over a portion of the south of England and of the English Channel. The remains of a rich Wealden flora have been collected from these Wealden sediments, notably from the plant-beds of Ecclesbourne near Hastings, in which, so far as we know, flowering plants played no part or at most occupied a very subordinate position. A few fossil leaves have been described from rocks assigned to a Wealden age,--and from the older Stonesfield Slate, of Jurassic age, a single leaf is recorded,--which seem to be those of Dicotyledons; but it is certain that even in the early days of the Cretaceous period the present dominant group in the plant kingdom was in its infancy and in many regions probably unrepresented. When we glance at the geological table and consider that in all the floras from the Wealden down to the Devonian period, flowering plants played no part, we are able to appreciate the fact of their rapid development, referred to in a previous chapter, when once this highest type had become established.
Seward opens not with a sweeping claim but with a precise question: how old are the plants we see today? He immediately anchors the discussion in observable evidence—the green, short-lived spores of Osmunda ferns, which he argues are a primitive trait that handicaps dispersal. This focus on a single, concrete detail sets the tone for a work that builds its case from the ground up, using anatomical structure and fossil comparison rather than speculation.
Spore Colour as a Clue to Antiquity
Seward draws attention to a seemingly minor feature: the spores of Osmunda are green and lack the durability of the brown spores typical of most ferns. He cites Professor Campbell’s work on liverworts to argue that such delicate reproductive cells imply slow, difficult dispersal over geological time. If a plant with fragile spores is nonetheless widespread, its distribution likely reflects great age rather than recent migration. This reasoning is typical of Seward’s method—he treats a physiological detail as a historical document.
The argument is reinforced by fossil evidence. Seward notes that Permian rocks in Russia contain fern stems with anatomical features linking them to modern Osmundas, and Jurassic strata in Yorkshire yield fertile fronds with spores “practically identical” to those of living species. A petrified stem from New Zealand, Osmundites Dunlopi, is described as “almost identical in structure” to surviving forms. By stacking these observations, Seward builds a case for the Royal Fern’s lineage extending into the Palaeozoic.
Forked Fronds and Fossil Imprints
The genus Gleichenia offers another example of Seward’s reliance on visual and structural cues. He describes its fronds as “repeatedly forked” with a small bud between the divergent branches, and notes that the leaflets resemble “the teeth of a comb.” Such morphological precision allows him to identify fossil fragments from the Wealden strata near Brussels—the same beds that yielded Iguanodon skeletons. The co-occurrence of plant and dinosaur fossils is not sensationalised; Seward simply records it as a stratigraphic marker.
He also points to the anatomy of the creeping stem as a “ready means of identification,” showing that even fragmentary fossils can be assigned to genus when the observer knows what to look for. This section demonstrates how Seward trains his reader to see plants as composite records—each fork, bud, and cell wall a potential clue to evolutionary history.
Discontinuous Ranges as Evidence of Relict Status
Seward repeatedly invokes the concept of discontinuous geographical distribution as an indicator of antiquity. The Osmunda family, for example, appears in scattered locations—Ireland, New Zealand, and elsewhere—suggesting a once-continuous range broken by climatic shifts and continental changes. He treats this pattern not as a curiosity but as a logical inference: if a plant group is found in widely separated regions but has poor dispersal abilities, its current distribution must be a remnant of a former, larger range.
This argument is applied to other groups as well. The redwoods of California, the araucarias of the Southern Hemisphere, and the maidenhair tree (Ginkgo) are each presented as living fossils whose present-day isolation mirrors their ancient lineage. Seward avoids dramatic language; instead, he lets the geographic data speak. The reader is left to connect the dots between a fern in Killarney and a fossil in Yorkshire, building a picture of deep time through accumulated detail.
The Authority of Anatomical Detail
Throughout the book, Seward privileges internal anatomy over external form. He notes that stems are “constructed on very different plans” and that the structural peculiarities of primitive types can be recognised even in fragmentary fossils. This emphasis on wood anatomy, spore structure, and cellular organisation reflects his training as a botanist and his conviction that the most reliable evidence of relationship lies beneath the surface.
He cites the work of Kidston and Gwynne-Vaughan on Permian fern stems, which revealed “Osmundaceous characters” in plants too ancient to be placed in the same family. Such careful qualification—acknowledging difference while asserting connection—is characteristic of Seward’s prose. He does not overstate his case; he lets the anatomical facts accumulate until the reader is persuaded by weight of evidence rather than rhetorical flourish.
Seward’s book is best read as a series of linked case studies rather than a continuous narrative. Each chapter examines a different plant group, and the reader may profitably dip into any section. Pay attention to the footnotes and the bibliography at the end; Seward frequently directs the curious to primary sources. The photographs and diagrams, though few, are carefully chosen to illustrate the points made in the text. Approach the work as a companion to a herbarium or a museum collection—it rewards slow, patient reading alongside the specimens it describes.
The rain drummed on the windowsill that afternoon, and I kept returning to the ginkgo’s stubborn leaf, a fossil made flesh. It made me think of patience, of things waiting. Later, drying my hands on a towel, I picked up another old volume, Crimson Clover [1947] — Inside the Classic, and found the same quiet persistence in its faded pages, a different kind of ancient pattern holding its ground.
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