vs Lesson's Saddle-back Tamarin

Chrysosphaerella longispina compared with Leontocebus fuscus

Key Differences

is Not Evaluated while Lesson's Saddle-back Tamarin is Least Concern.

Taxonomic Classification

Rank		Lesson's Saddle-back Tamarin
Kingdom	Chromista (хромисты)	Animalia (животные)
Phylum	Ochrophyta (охрофитовые водоросли)	Chordata (хордовые)
Class	Chrysophyceae (Золотистые водоросли)	Mammalia (млекопитающие)
Order	Ochromonadales (Ochromonadales)	Primates (приматы)
Family	Paraphysomonadaceae	Callitrichidae
Genus	Chrysosphaerella	Leontocebus
Species	Chrysosphaerella longispina	Leontocebus fuscus

Conservation Status

NE — Not Evaluated

Lesson's Saddle-back Tamarin

LC — Least Concern

Physical Characteristics

Attribute		Lesson's Saddle-back Tamarin
Diet	—	—
Average Lifespan	—	—
Average Length	—	—
Average Weight	—	—

Habitat & Geographic Range

Habitat

Native to Europe, inhabiting ecosystems characteristic of the region.

Range

Distributed across Denmark, Norway, and Sweden.

Lesson's Saddle-back Tamarin

Habitat

Typically found in diverse terrestrial and aquatic ecosystems.

Range

Found in Colombia.

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.