Zoology

Theories of continental drift and plate tectonics
Theory of Continental Drift: Proposed by: Alfred Wegener (1912)Wegener, a German meteorologist and geophysicist, proposed that continents were once a single landmass that drifted apart over geological time.The Supercontinent – Pangaea. Around 300 million years ago, all landmasses were joined
Palaeogeography
Palaeogeography is the branch of geology that reconstructs the historical geography of Earth’s surface. It seeks to understand how continents, oceans, mountain ranges, and other geographic features have changed position and form over geological time. By combining data from sedimentology,
Neotropical Realm, Ethiopian Realm, Oriental Realm & Australian Realm
Neotropical Realm A. Geographical Boundaries:The Neotropical Realm includes South and Central America, the lower part of Mexico, and the West Indies. It is connected to the Nearctic Realm via the Central American Isthmus, while its other boundaries are defined by

Map work for identification of various zoogeographical regions of the world
Zoogeography is the branch of biogeography that deals with the distribution of animal species and populations across geographical areas of the Earth. The world is traditionally divided into six major zoogeographical (faunal) regions, each with its unique assemblage of fauna
Study of Vertebrate Fossils: Horse, Elephant, Camel, and Bovids
Vertebrate paleontology involves the study of fossilized bones, teeth, and traces of animals with backbones. Fossils of large mammals such as horses, elephants, camels, and bovids (cattle-like animals) are key to understanding evolutionary processes, climatic shifts, and faunal dispersal across
Study of invertebrate fossils of coelenterates, trilobites, ammonite, brachiopods, mollusks and echinoderms
Invertebrate fossils form a substantial part of the fossil record and are key indicators in the fields of paleontology, biostratigraphy, and evolutionary biology. These organisms, lacking vertebral columns, often had hard shells or exoskeletons which fossilized well. Their abundance and