Flat-petioled spindle
Crop

Flat-petioled spindle

Euonymus planipes

Description

Euonymus planipes, commonly known as the flat-petioled spindle, is a deciduous shrub belonging to the Celastraceae family. It is widely recognized by botanists and horticulturists for its remarkable seasonal interest, particularly its brilliant autumn foliage and unique, showy fruit capsules that appear in late summer and early autumn.

Native to East Asia, including regions of the Russian Far East, Japan, Korea, and China, this plant has adapted to temperate forest climates. In cultivation, it has proven to be a robust and reliable woody plant, suitable for inclusion in botanical collections and private gardens throughout various hardiness zones.

Botanically, it is a sturdy, multi-stemmed shrub that can reach heights of 2-3 meters. Its branches are glabrous and produce thin, flat petioles, which inspired its specific epithet. The fruit is perhaps its most distinct trait, appearing as pendulous, deep-red pods that split to reveal bright orange-covered seeds, creating a high-contrast visual display.

Agrotechnical success with this species requires well-drained, fertile soil with a neutral to slightly alkaline pH. While the shrub exhibits good shade tolerance, planting it in a location with partial or full sun exposure ensures the most vibrant leaf coloration during the fall. Maintenance includes annual mulching to retain soil moisture and light pruning to encourage denser branching.

In landscaping, Euonymus planipes is highly valued for its versatility as a specimen plant or as part of a mixed border. While generally hardy, growers should remain vigilant for common pests such as aphids or spider mites, as well as fungal issues like powdery mildew, which can be managed through proper site ventilation and timely integrated pest management practices.

  • Stunning red autumn color
  • Distinctive pendulous fruit
  • Good tolerance to partial shade
  • Low maintenance requirements
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Дмитрий Дунин · CC BY 4.0 · GBIF
Дмитрий Дунин · CC BY 4.0 · GBIF
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