Betic Midwife Toad vs

Alytes dickhilleni compared with Chrysosphaerella longispina

Key Differences

• Betic Midwife Toad is Endangered while is Not Evaluated.

Taxonomic Classification

Rank	Betic Midwife Toad
Kingdom	Animalia (حيوانات)	Chromista (أسناخ صبغية)
Phylum	Chordata (حبليات)	Ochrophyta (طحالب داكنة)
Class	Amphibia (برمائيات)	Chrysophyceae (طحالب ذهبية)
Order	Anura (ضفدع)	Ochromonadales (Ochromonadales)
Family	Alytidae	Paraphysomonadaceae
Genus	Alytes	Chrysosphaerella
Species	Alytes dickhilleni	Chrysosphaerella longispina

Conservation Status

Betic Midwife Toad

EN — Endangered

NE — Not Evaluated

Physical Characteristics

Attribute	Betic Midwife Toad
Diet	—	—
Average Lifespan	—	—
Average Length	—	—
Average Weight	—	—

Habitat & Geographic Range

Betic Midwife Toad

Habitat

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

Habitat

Native to Europe, inhabiting ecosystems characteristic of the region.

Range

Distributed across Denmark, Norway, and Sweden.

Betic Midwife Toad

The Betic Midwife Toad (Alytes dickhilleni) is a species in the genus Alytes. It is currently classified as Endangered on the IUCN Red List. Typically found in freshwater habitats, moist forests, and wetlands.

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.