Amphibians are cold-blooded vertebrates that typically have a moist, permeable skin, and spend at least part of their life cycle in water. They are known for their ability to live both in water and on land, making them unique among vertebrates.
Characteristics of Amphibians
Amphibians have several key characteristics that distinguish them from other vertebrates:
Moist, Permeable Skin: Amphibians have skin that allows for the exchange of gases and water, making them sensitive to environmental changes.
Metamorphosis: Most amphibians undergo a metamorphosis from a water-dwelling larval stage to a land-dwelling adult stage.
Frogs and Toads: These are the most diverse group of amphibians, with over 6,000 species. They have strong hind legs for jumping and often have a semi-aquatic lifestyle.
Salamanders and Newts: These amphibians have long bodies and tails, and are typically found in moist environments such as forests and streams.
Caecilians: These amphibians resemble earthworms or snakes and are found in tropical regions, often living underground or in water.
Life Cycle of Amphibians
Amphibians typically go through a complex life cycle that involves both aquatic and terrestrial stages:
Egg: Most amphibians lay eggs in water, which hatch into aquatic larvae.
Larval Stage: The larvae, such as tadpoles in frogs, live in water and undergo dramatic changes as they grow and develop.
Metamorphosis: The larvae undergo metamorphosis, developing legs and lungs to become terrestrial adults.
Adult Stage: The adult amphibians live on land, but often return to water to breed and lay eggs, completing the cycle.
Importance of Amphibians
Amphibians play crucial roles in ecosystems as both predators and prey. They also serve as indicators of environmental health, as their sensitive skin makes them vulnerable to pollution and habitat destruction.
Study Guide
Here are some key topics to study when learning about amphibians:
Use models (e.g., diagrams, maps, globes, digital representations) to explain how the rotation of Earth and unequal heating of its surface create patterns of atmospheric and oceanic circulation that determine regional climates.