Apulian Garlic vs

Allium apulum compared with Chrysosphaerella longispina

Key Differences

• Apulian Garlic is Least Concern while is Not Evaluated.

Taxonomic Classification

Rank	Apulian Garlic
Kingdom	Plantae (พืช)	Chromista (โครมิสตา)
Phylum	Magnoliophyta (Flowering Plants)	Ochrophyta (Ochrophyta)
Class	Liliopsida (Monocots)	Chrysophyceae (สาหร่ายสีทอง)
Order	Asparagales (อันดับหน่อไม้ฝรั่ง)	Ochromonadales (Ochromonadales)
Family	Amaryllidaceae	Paraphysomonadaceae
Genus	Allium	Chrysosphaerella
Species	Allium apulum	Chrysosphaerella longispina

Conservation Status

Apulian Garlic

LC — Least Concern

NE — Not Evaluated

Physical Characteristics

Attribute	Apulian Garlic
Diet	—	—
Average Lifespan	—	—
Average Length	—	—
Average Weight	—	—

Habitat & Geographic Range

Apulian Garlic

Habitat

Typically found in grasslands, wetlands, forests, and cultivated landscapes.

Habitat

Native to Europe, inhabiting ecosystems characteristic of the region.

Range

Distributed across Denmark, Norway, and Sweden.

Apulian Garlic

The Apulian Garlic (Allium apulum) is a species in the genus Allium. It is currently classified as Least Concern on the IUCN Red List. Typically found in grasslands, wetlands, forests, and cultivated landscapes.

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.