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Skeletocutis biguttulata

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Skeletocutis biguttulata is a species of poroid fungus in the family Polyporaceae. It was first described scientifically by Swedish mycologist Lars Romell in 1932.[2] Tuomo Niemelä redescribed and illustrated the fungus in 1998, and explained that collections of this fungus had previously been attributed to the related Skeletocutis subincarnata. S. biguttulata may be distinguished from the latter fungus by its biguttulate spores (containing two oil droplets), more regularly arranged pores, and the cracking pore surface seen in older specimens.[3]

It has been collected in Fennoscandia, Estonia, France, Poland,[4] and Russia.[5]

References

  1. ^ "GSD Species Synonymy: Skeletocutis biguttulata (Romell) Niemelä". Species Fungorum. CAB International. Retrieved 2016-10-04.
  2. ^ Pilát, A. (1932). "Additamenta ad floram Sibiriae Asiaeque orientalis mycologicam. Pars prima: Polyporaceae". Bulletin de la Société Mycologique de France (in French). 48 (1): 1–52.
  3. ^ Niemelä, Tuomo (1998). "The Skeletocutis subincarnata complex (Basidiomycetes), a revision". Acta Botanica Fennica. 161: 1–35.
  4. ^ Piatek, Marcin; Cabala, Jolanta. "New and noteworthy polypores from Poland with validation of the family Phaeotrametaceae". Mycotaxon. 91: 173–183.
  5. ^ Spirin, Viacheslav (2005). "Notes on some rare polypores, found in Russia 2. Junghuhnia vitellina sp. nova, plus genera Cinereomyces and Skeletocutis". Karstenia. 45 (2): 103–113. doi:10.29203/ka.2005.409.
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Skeletocutis biguttulata: Brief Summary

provided by wikipedia EN

Skeletocutis biguttulata is a species of poroid fungus in the family Polyporaceae. It was first described scientifically by Swedish mycologist Lars Romell in 1932. Tuomo Niemelä redescribed and illustrated the fungus in 1998, and explained that collections of this fungus had previously been attributed to the related Skeletocutis subincarnata. S. biguttulata may be distinguished from the latter fungus by its biguttulate spores (containing two oil droplets), more regularly arranged pores, and the cracking pore surface seen in older specimens.

It has been collected in Fennoscandia, Estonia, France, Poland, and Russia.

license
cc-by-sa-3.0
copyright
Wikipedia authors and editors
original
visit source
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wikipedia EN