Syllabus topics (official RTMNU)
- Palaeobotany: Concept and Importance. Geological Time Scale.
- Contributions of Birbal Sahni
- Types of fossils: Impression, Compression, Petrifaction, Cast, Mold and Amber.
- Fossil plants: Glossopteris (Leaf, Scutum).
Palaeobotany: Concept and Importance. Geological Time Scale.
Palaeobotany (Gk. palaios = ancient, botane = plant) is the branch of botany that deals with the study of fossil plants of past geological ages. A fossil is any remains, trace or impression of an organism preserved in rocks of the earth's crust. The term was popularised by the study of plant remains in sedimentary rocks.
Concept: When plants die, most of them decay. But if a plant part is quickly buried in fine sediments (mud, silt, volcanic ash) under water, decay is slowed because oxygen and microbes are less. Over millions of years the sediment becomes rock and the plant part is preserved as a fossil. Fossils are found mostly in sedimentary rocks.
Importance of Palaeobotany:
- Evolution: gives direct evidence of plant evolution, e.g. origin of vascular plants (Rhynia), origin of seed habit (seed ferns).
- Connecting links: reveals extinct groups such as Pteridospermales (seed ferns), Cycadeoidales and Glossopteridales.
- Stratigraphy: index fossils help in dating and correlating rock layers.
- Fuel exploration: coal is formed from Carboniferous and Permian plants; fossil spores and pollen (palynology) help locate coal and petroleum.
- Palaeoclimate and palaeogeography: fossils tell about past climates; Glossopteris flora supports the theory of continental drift (Gondwanaland).
- Phylogeny and classification: helps in arranging plant groups in a natural order.
Geological Time Scale: The history of the earth (about 4.6 billion years) is divided into Eras โ Periods โ Epochs. Each era has a characteristic flora.
| Era | Period | Approx. age (million years ago) | Dominant plant life |
|---|---|---|---|
| Cenozoic | Quaternary | 2.6 โ present | Modern herbs, man appears |
| Cenozoic | Tertiary | 66 โ 2.6 | Dominance of angiosperms |
| Mesozoic | Cretaceous | 145 โ 66 | Rise of angiosperms; gymnosperms decline |
| Mesozoic | Jurassic | 201 โ 145 | Age of cycads, Bennettitales, conifers |
| Mesozoic | Triassic | 252 โ 201 | Gymnosperms dominant; seed ferns decline |
| Palaeozoic | Permian | 299 โ 252 | Glossopteris flora (Gondwana), conifers |
| Palaeozoic | Carboniferous | 359 โ 299 | Age of pteridophytes and seed ferns; coal forests (Lepidodendron, Calamites) |
| Palaeozoic | Devonian | 419 โ 359 | Early land vascular plants (Rhynia), first seeds late |
| Palaeozoic | Silurian | 444 โ 419 | First vascular land plants (Cooksonia) |
| Palaeozoic | Ordovician & Cambrian | 541 โ 444 | Marine algae |
| Precambrian | โ | 4600 โ 541 | Bacteria, blue-green algae (stromatolites) |
Contributions of Birbal Sahni
Prof. Birbal Sahni (1891โ1949) is known as the Father of Indian Palaeobotany. He was born at Bhera (now in Pakistan), studied at Lahore and at Cambridge under Prof. A.C. Seward.
- Worked as Professor of Botany at Lucknow University; founded the Birbal Sahni Institute of Palaeobotany (BSIP), Lucknow in 1946 (foundation stone laid by Pt. Jawaharlal Nehru in 1949).
- Studied the Glossopteris flora of the Gondwana rocks of India and supported continental drift.
- Described the Rajmahal Hills (Jharkhand) Jurassic flora; discovered and named Pentoxylon (Pentoxylales), a new group of gymnosperms, and Williamsonia sewardiana.
- Worked on Homoxylon (a vesselless angiosperm-like wood) and on fossils of the Deccan Intertrappean beds (e.g. Enigmocarpon).
- Studied the age of the Saline Series of the Salt Range (Punjab) using microfossils.
- Also contributed to archaeology โ studied coin moulds of Rohtak.
- Elected Fellow of the Royal Society (FRS) in 1936 โ first Indian botanist to receive it; President of the Indian Science Congress (1940).
Types of fossils: Impression, Compression, Petrifaction, Cast, Mold and Amber.
| Type | How formed | What is preserved |
|---|---|---|
| Impression | Plant part pressed on soft mud; organic matter lost completely | Only a print/outline of the surface (e.g. leaf venation). No organic matter. |
| Compression | Plant part flattened by weight of sediments; water and gases removed | A thin carbonaceous film; cuticle can be peeled and studied (e.g. Glossopteris leaves in coal shales) |
| Petrifaction (Petrification) | Minerals (silica, calcium carbonate, pyrites) dissolved in water infiltrate cells and replace/fill them | Internal cellular anatomy in 3-D; studied by thin sections or peel method (e.g. Rhynia in Rhynie chert) |
| Mold (Mould) | Plant part buried and later decays, leaving a hollow cavity in rock | External shape as a cavity |
| Cast | The cavity of a mould gets filled with minerals/sediment that harden | A solid replica of the external form (e.g. pith casts of Calamites) |
| Amber | Small organisms or plant parts trapped in sticky resin of conifers; resin hardens into amber | Very fine details, even cells; pollen, flowers, insects |
Fossil plants: Glossopteris (Leaf, Scutum).
Systematic position: Gymnosperms โ Pteridospermales (Glossopteridales). Glossopteris (Gk. glossa = tongue) is a form-genus for tongue-shaped leaves of Permian age found in the Gondwana rocks of India, Africa, South America, Australia and Antarctica. Its wide distribution supports the idea of a single southern continent, Gondwanaland.
Leaf:
- Simple, tongue-shaped (lingulate) to spathulate, 2โ40 cm long, margin entire, apex obtuse or acute.
- Prominent midrib made of several parallel veins.
- Lateral veins arise from the midrib at acute angles, arch towards the margin and form a reticulate (net) venation with elongated meshes.
- Leaves borne in spirals or pseudo-whorls on woody stems; the fossil roots of this plant are called Vertebraria (they look jointed in cross section); the wood is Araucarioxylon-type.
- Stomata on lower surface (hypostomatic), sunken.
Scutum (fertile structure):
- The scutum is a female (ovulate) fructification of Glossopteridales.
- It is attached to the midrib of a fertile leaf by a stalk (adnate pedicel).
- It is made of two halves: a sterile cap/scale half and a fertile half bearing many ovules (seeds) on the inner surface; the margin is often fringed.
- Examples of related fructifications: Scutum, Ottokaria, Lidgettonia (female); Eretmonia and Glossotheca (male, bearing pollen sacs).
5 likely exam questions
Long answer
- What is palaeobotany? Explain its importance and give an outline of the Geological Time Scale with dominant plant groups.
- Describe the different types of fossils and the process of their formation. Add a note on Glossopteris.
Short answer / short notes
- Write the contributions of Prof. Birbal Sahni to palaeobotany.
- Differentiate between impression and compression fossils.
- Describe the leaf and scutum of Glossopteris.