Broad-muzzled Bat vs

Submyotodon latirostris compared with Chrysosphaerella longispina

Key Differences

• Broad-muzzled Bat is Least Concern while is Not Evaluated.

Taxonomic Classification

Rank	Broad-muzzled Bat
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	Chiroptera (翼手目)	Ochromonadales (Ochromonadales)
Family	Vespertilionidae	Paraphysomonadaceae
Genus	Submyotodon	Chrysosphaerella
Species	Submyotodon latirostris	Chrysosphaerella longispina

Conservation Status

Broad-muzzled Bat

LC — Least Concern

NE — Not Evaluated

Physical Characteristics

Attribute	Broad-muzzled Bat
Diet	—	—
Average Lifespan	—	—
Average Length	—	—
Average Weight	—	—

Habitat & Geographic Range

Broad-muzzled Bat

Habitat

Typically found in diverse terrestrial and aquatic ecosystems.

Range

Found in Taiwan.

Habitat

Native to Europe, inhabiting ecosystems characteristic of the region.

Range

Distributed across Denmark, Norway, and Sweden.

Broad-muzzled Bat

The Broad-Muzzled Bat (Submyotodon latirostris) is a species in the genus Submyotodon. It is currently classified as Least Concern 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.