Apple Blotch vs Oso Polar

Phyllosticta arbutifolia compared with Ursus maritimus

Key Differences

Apple Blotch is Not Evaluated while Oso Polar is Vulnerable.

Taxonomic Classification

Rank	Apple Blotch	Oso Polar
Kingdom	Fungi (Fungi)	Animalia (Animals)
Phylum	Ascomycota (Sac Fungi)	Chordata (cordados)
Class	Dothideomycetes (Dothideomycetes)	Mammalia (mamíferos)
Order	Botryosphaeriales (Botryosphaeriales)	Carnivora (carnívoros)
Family	Phyllostictaceae	Ursidae (Bears)
Genus	Phyllosticta	Ursus (Bears)
Species	Phyllosticta arbutifolia	Ursus maritimus

Conservation Status

Apple Blotch

NE — Not Evaluated

Oso Polar

VU — Vulnerable

Population: ~26.0K

Trend: Decreasing ↓

Physical Characteristics

Attribute	Apple Blotch	Oso Polar
Diet	—	Carnivore
Average Lifespan	—	25 years
Average Length	—	2.4 m
Average Weight	—	450.0 kg

Habitat & Geographic Range

Apple Blotch

Habitat

Native to Europe, inhabiting ecosystems characteristic of the region.

Range

Found in Sweden.

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.

Apple Blotch

The Apple Blotch (Phyllosticta arbutifolia) is a species in the genus Phyllosticta. Native to Europe, inhabiting ecosystems characteristic of the region.

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.