Balkan Maple vs Oso Polar

Acer hyrcanum compared with Ursus maritimus

Key Differences

  • Balkan Maple is Least Concern while Oso Polar is Vulnerable.

Taxonomic Classification

Rank Balkan Maple Oso Polar
Kingdom Plantae (planta) Animalia (Animals)
Phylum Magnoliophyta (Flowering Plants) Chordata (cordados)
Class Magnoliopsida (Dicots) Mammalia (mamíferos)
Order Sapindales (Sapindales) Carnivora (carnívoros)
Family Sapindaceae Ursidae (Bears)
Genus Acer Ursus (Bears)
Species Acer hyrcanum Ursus maritimus

Conservation Status

Balkan Maple

LC — Least Concern

Oso Polar

VU — Vulnerable

Population: ~26.0K

Trend: Decreasing ↓

Physical Characteristics

Attribute Balkan Maple Oso Polar
Diet Carnivore
Average Lifespan 25 years
Average Length 2.4 m
Average Weight 450.0 kg

Habitat & Geographic Range

Balkan Maple

Habitat

Typically found in diverse terrestrial habitats from tropical forests to temperate regions.

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.

Balkan Maple

The Balkan Maple (Acer hyrcanum) is a species in the genus Acer. It is currently classified as Least Concern on the IUCN Red List. Typically found in diverse terrestrial habitats from tropical forests to temperate regions.

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.

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