Difference between revisions of "Kentiopsis pyriformis"

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[[Image:Kpyriformis2.jpg|thumb|300px|CA]]
 
[[Image:Kpyriformis2.jpg|thumb|300px|CA]]
  
 
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==Habitat==
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Kentiopsis pyriformis grows on ultramafic rocks, often on unstable steep slopes.
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==Distribution==
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Kentiopsis pyriformis ranges from along the east coast of New Caledonia south of Yate, where it occurs in a fringe of forest 20km long an 100-500m wide from Touaourou to Goro villages at 5-100m elevation.  The main population is at Goro on steep, unstable rocky slope above the mouth of the Kuebini River
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==Description==
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Subcanopy to emergent palm.  Trunk 10-18m tall.  Sometimes enlarged or buldging at the base, adventious roots visible
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==Culture==
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Flowers usually occur from November through February with a 15day delay between anthesis of staminate and pistillate flowers in the same triad; fruits mature from April through June.  Seedlings of Kentiopsis pyriformis have been found germinating on red colluvium, rich in iron oxide.  This material originates from the erosion of ultrabasic rocks (peridoite) on nearby slopes...
 
[[Category:KENTIOPSIS|pyriformis]]
 
[[Category:KENTIOPSIS|pyriformis]]

Revision as of 05:31, 16 January 2012

young container plant in CA
CA
CA

Habitat

Kentiopsis pyriformis grows on ultramafic rocks, often on unstable steep slopes.

Distribution

Kentiopsis pyriformis ranges from along the east coast of New Caledonia south of Yate, where it occurs in a fringe of forest 20km long an 100-500m wide from Touaourou to Goro villages at 5-100m elevation. The main population is at Goro on steep, unstable rocky slope above the mouth of the Kuebini River

Description

Subcanopy to emergent palm. Trunk 10-18m tall. Sometimes enlarged or buldging at the base, adventious roots visible

Culture

Flowers usually occur from November through February with a 15day delay between anthesis of staminate and pistillate flowers in the same triad; fruits mature from April through June. Seedlings of Kentiopsis pyriformis have been found germinating on red colluvium, rich in iron oxide. This material originates from the erosion of ultrabasic rocks (peridoite) on nearby slopes...