UPSC MainsGEOLOGY-PAPER-I201615 Marks
Q28.

Give an account of the evolutionary changes noticed in the glabella of trilobites.

How to Approach

This question requires a detailed understanding of trilobite morphology and evolutionary trends, specifically focusing on the glabella. The answer should trace the changes in glabella shape, size, and ornamentation through different trilobite orders and geological time. A chronological approach, starting with early trilobites and progressing to more advanced forms, is recommended. Mentioning key trilobite orders (e.g., Agnostida, Redlichida, Phacopida, Proetida) and their characteristic glabella features will enhance the answer.

Model Answer

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Introduction

Trilobites, an extinct group of marine arthropods, are invaluable index fossils for Paleozoic rocks. Their well-defined exoskeletons, particularly the cephalon (head), provide a rich record of evolutionary changes. The glabella, the central raised portion of the cephalon, is a crucial element in trilobite classification and understanding their phylogenetic relationships. Its morphology underwent significant transformations throughout their ~270 million-year existence, reflecting adaptations to different ecological niches and evolutionary pressures. This account will detail the evolutionary changes observed in the glabella of trilobites, tracing its development from early forms to more advanced species.

Early Trilobites: Agnostida and Redlichida

The earliest trilobites, belonging to the orders Agnostida and Redlichida (Cambrian period), exhibited relatively simple glabellae. In Agnostida, the glabella was typically small, nearly parallel-sided, and often occupied less than half the cephalon width. It lacked distinct furrows or lobes. These trilobites were generally small and likely inhabited deep-water environments.

Redlichida showed a more developed glabella, often wider than in Agnostida, and frequently displaying shallow, longitudinal furrows. The glabella in Redlichida was generally convex and expanded posteriorly. A key characteristic was the presence of genal spines, extending laterally from the cephalon. The glabella’s size and furrow development increased gradually within this order, indicating early experimentation with cephalic morphology.

Intermediate Forms: Ptychopariida and Corynexochida

During the Ordovician period, the orders Ptychopariida and Corynexochida emerged, displaying more complex glabellae. Ptychopariida exhibited a glabella that was often wider than long, with prominent lateral lobes and a distinct axial lobe. The furrows were more pronounced, creating a more sculpted appearance. These trilobites were often larger and more actively mobile than their Cambrian predecessors.

Corynexochida showed a unique glabella morphology characterized by a narrow, elongated glabella with a distinct, often deeply incised, central furrow. The glabella was typically surrounded by a broad facial suture, allowing for enrollment (rolling up) for protection. This order represents a significant step towards more specialized glabella structures.

Advanced Trilobites: Phacopida and Proetida

The Phacopida (Ordovician-Devonian) and Proetida (Ordovician-Permian) represent the most advanced trilobite orders, exhibiting the most diverse and specialized glabellae.

  • Phacopida: The glabella in Phacopida is characterized by its pronounced forward projection, forming a prominent ‘nose’ or rostrum. This projection likely served as a sensory organ or for sediment probing. The glabella also displayed well-developed furrows and often had a distinct ‘occipital ring’ at its posterior margin. The eyes were large and well-developed, contributing to their predatory lifestyle.
  • Proetida: Proetida exhibited a wide range of glabella morphologies. Early Proetids had relatively simple glabellae, but later forms developed highly complex structures. Some Proetids had a very wide, flattened glabella, while others had a narrow, elongated one. The furrows were often deeply incised and branched, creating a highly ornamented surface. The glabella’s shape and ornamentation varied significantly between different species, reflecting their diverse ecological roles.

Evolutionary Trends Summarized

The evolutionary changes in the trilobite glabella can be summarized as follows:

Order Glabella Shape Furrow Development Ornamentation Period
Agnostida Small, parallel-sided Absent or shallow Smooth Cambrian
Redlichida Wider than long, convex Shallow, longitudinal Slightly ornamented Cambrian
Ptychopariida Wide, with lateral lobes Prominent Sculpted Ordovician
Corynexochida Narrow, elongated Deeply incised central furrow Smooth Ordovician
Phacopida Projecting rostrum Well-developed Ornamented, occipital ring Ordovician-Devonian
Proetida Variable (wide, flattened, narrow) Deeply incised, branched Highly ornamented Ordovician-Permian

These changes reflect adaptations to different lifestyles, including changes in sensory perception, feeding strategies, and defensive mechanisms. The increasing complexity of the glabella is also indicative of the overall evolutionary trend towards greater specialization and diversification within the trilobite lineage.

Conclusion

The evolution of the trilobite glabella provides a compelling example of how morphological features can change over geological time in response to environmental pressures and evolutionary opportunities. From the simple, parallel-sided glabellae of early trilobites to the highly complex and ornamented structures of later forms, the glabella’s evolution reflects the remarkable adaptability and diversity of this extinct group. Studying these changes provides valuable insights into the evolutionary history of arthropods and the paleoecology of the Paleozoic seas.

Answer Length

This is a comprehensive model answer for learning purposes and may exceed the word limit. In the exam, always adhere to the prescribed word count.

Additional Resources

Key Definitions

Cephalon
The cephalon is the anterior (head) section of a trilobite's exoskeleton, containing the glabella, eyes, and facial sutures.
Facial Suture
The facial suture is a line on the cephalon of a trilobite that allows the front part of the cephalon to be shed during molting.

Key Statistics

Trilobites existed for approximately 270 million years, from the early Cambrian period (around 521 million years ago) to the end of the Permian period (around 252 million years ago).

Source: Palmer, D. (1998). The Fossil Book. New York: Facts on File.

Over 20,000 species of trilobites have been identified, representing a significant portion of the Paleozoic marine fauna.

Source: Fortey, R. A. (2000). Trilobite! Eyewitness to Evolution. New York: Alfred A. Knopf.

Examples

Elrathia kingii

Elrathia kingii, a common Middle Cambrian trilobite from Utah, USA, exhibits a well-defined glabella with three distinct lobes separated by furrows, showcasing the typical glabella structure of Redlichida.

Frequently Asked Questions

What was the function of the glabella?

The exact function of the glabella is debated, but it likely housed sensory organs, contributed to muscle attachment for cephalic movement, and played a role in hydrodynamic stability.

Topics Covered

PaleontologyGeologyFossilsTrilobitesEvolutionary Biology