Giant Philippine Frog vs Oso Polar

Limnonectes macrocephalus compared with Ursus maritimus

Key Differences

• Giant Philippine Frog is Near Threatened while Oso Polar is Vulnerable.

Taxonomic Classification

Rank	Giant Philippine Frog	Oso Polar
Kingdom same	Animalia (Animals)	Animalia (Animals)
Phylum same	Chordata (cordados)	Chordata (cordados)
Class	Amphibia (Amphibians)	Mammalia (mamíferos)
Order	Anura (Frogs & Toads)	Carnivora (carnívoros)
Family	Dicroglossidae	Ursidae (Bears)
Genus	Limnonectes	Ursus (Bears)
Species	Limnonectes macrocephalus	Ursus maritimus

Evolutionary Relationship

Giant Philippine Frog and Oso Polar share a common ancestor at the Phylum level: Chordata. (cordados)

Conservation Status

Giant Philippine Frog

NT — Near Threatened

Oso Polar

VU — Vulnerable

Population: ~26.0K

Trend: Decreasing ↓

Physical Characteristics

Attribute	Giant Philippine Frog	Oso Polar
Diet	—	Carnivore
Average Lifespan	—	25 years
Average Length	—	2.4 m
Average Weight	—	450.0 kg

Habitat & Geographic Range

Giant Philippine Frog

Habitat

Typically found in freshwater habitats, moist forests, and wetlands.

Oso Polar

Habitat

Found across multiple habitat types including temperate broadleaf and mixed forests, temperate coniferous forests, and boreal forests and taiga, among 4 distinct biome types within the Palearctic biogeographic realm. Populations are also found in montane and highland environments at higher elevations.

Range

Found in Norway. Currently classified as Vulnerable on the IUCN Red List, this species faces significant conservation challenges across its range.

Oso Polar

El mayor carnivoro terrestre de la Tierra, el oso polar puede superar los 700 kg y se encuentra en el hielo marino del Artico, desde Canada hasta Rusia. Es un mamifero marino altamente especializado que depende del hielo marino para cazar focas anilladas y barbadas. Excelente nadador capaz de cubrir grandes distancias en agua abierta. Clasificado como Vulnerable, sus poblaciones soportan una presion severa por la rapida perdida de hielo marino artico debida al cambio climatico.