Banded hare-wallaby vs

Lagostrophus fasciatus compared with Chrysosphaerella longispina

Key Differences

• Banded hare-wallaby is Vulnerable while is Not Evaluated.

Taxonomic Classification

Rank	Banded hare-wallaby
Kingdom	Animalia (動物)	Chromista (クロミスタ)
Phylum	Chordata (脊索動物)	Ochrophyta (オクロ植物)
Class	Mammalia (哺乳類)	Chrysophyceae (黄金色藻)
Order	Diprotodontia (カンガルー目)	Ochromonadales (Ochromonadales)
Family	Macropodidae (Kangaroos)	Paraphysomonadaceae
Genus	Lagostrophus	Chrysosphaerella
Species	Lagostrophus fasciatus	Chrysosphaerella longispina

Conservation Status

Banded hare-wallaby

VU — Vulnerable

NE — Not Evaluated

Physical Characteristics

Attribute	Banded hare-wallaby
Diet	—	—
Average Lifespan	—	—
Average Length	—	—
Average Weight	—	—

Habitat & Geographic Range

Banded hare-wallaby

Habitat

Typically found in diverse terrestrial and aquatic ecosystems.

Habitat

Native to Europe, inhabiting ecosystems characteristic of the region.

Range

Distributed across Denmark, Norway, and Sweden.

Banded hare-wallaby

The Banded hare-wallaby (Lagostrophus fasciatus) is a species in the genus Lagostrophus. It is currently classified as Vulnerable on the IUCN Red List. Typically found in diverse terrestrial and aquatic ecosystems.

Chrysosphaerella longispina is a colonial chrysophyte alga in the genus Chrysosphaerella, notable for the long silica spines (longispina: Latin, long spine) that project from each cell in the colony. The genus is characterized by spherical or discoid colonies of photosynthetic cells that each secrete siliceous scales and elongated spine-like appendages, making Chrysosphaerella colonies distinctively bristled and visible under light microscopy. The long spines of C. longispina likely serve as anti-predation structures that make the colonies more difficult for zooplankton to ingest. C. longispina is found in cold, oligotrophic freshwater lakes, particularly in Scandinavia, where comprehensive chrysophyte surveys have documented its presence. Chrysosphaerella colonies contribute to freshwater primary production and the cycling of biogenic silica, which upon cell dissolution is deposited in lake sediments as microscopically identifiable remains. These silica structures are widely used by paleolimnologists to reconstruct past changes in lake water chemistry, thermal stratification, and climate. The conservation status of C. longispina has not been assessed by the IUCN; the species is listed as Not Evaluated.