Bali Shortcake vs

Acropora latistella compared with Chrysosphaerella longispina

Key Differences

• Bali Shortcake is Least Concern while is Not Evaluated.

Taxonomic Classification

Rank	Bali Shortcake
Kingdom	Animalia (حيوانات)	Chromista (أسناخ صبغية)
Phylum	Cnidaria (لاسعات)	Ochrophyta (طحالب داكنة)
Class	Anthozoa	Chrysophyceae (طحالب ذهبية)
Order	Scleractinia (مرجانيات صلبة)	Ochromonadales (Ochromonadales)
Family	Acroporidae	Paraphysomonadaceae
Genus	Acropora	Chrysosphaerella
Species	Acropora latistella	Chrysosphaerella longispina

Conservation Status

Bali Shortcake

LC — Least Concern

NE — Not Evaluated

Physical Characteristics

Attribute	Bali Shortcake
Diet	—	—
Average Lifespan	—	—
Average Length	—	—
Average Weight	—	—

Habitat & Geographic Range

Bali Shortcake

Habitat

Native to Asia, inhabiting ecosystems characteristic of the region.

Range

Found in Taiwan.

Habitat

Native to Europe, inhabiting ecosystems characteristic of the region.

Range

Distributed across Denmark, Norway, and Sweden.

Bali Shortcake

The Bali Shortcake (Acropora latistella) is a species in the genus Acropora. It is currently classified as Least Concern on the IUCN Red List. Native to Asia, inhabiting ecosystems characteristic of the region.

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.