Academic Journal
The Fossil Record of the Peronosporomycetes (Oomycota)
| العنوان: | The Fossil Record of the Peronosporomycetes (Oomycota) |
|---|---|
| المؤلفون: | Krings, Michael, Taylor, Thomas N., Dotzler, Nora |
| بيانات النشر: | Mycological Society of America |
| سنة النشر: | 2011 |
| المجموعة: | The University of Kansas: KU ScholarWorks |
| مصطلحات موضوعية: | Antheridium, Carboniferous, Chert, Coal ball, Devonian, Fossil water mold, Oogonium |
| الوصف: | This is the publisher's version, which is being shared with permission. The original may be found at the following link: http://dx.doi.org/10.3852/10-278 ; Evidence of fossil Peronosporomycetes has been slow to accumulate. In this review various fossils historically assigned to the Peronosporomycetes are discussed briefly and an explanation is provided as to why the fossil record of this group has remained inconsistent. In recent years there have been several new reports of fossil peronosporomycetes based on structurally preserved oogonium-antheridium complexes from Devonian and Carboniferous rocks that demonstrate the existence of these organisms as fossils and refute the long-standing assumption that they are too delicate to be preserved. Among these are several types characterized by oogonial surface ornamentation patterns not seen in any modern members of the group. To date at least three groups of fossil vascular plants (i.e. lycophytes, ferns and seed ferns) are known to host peronosporomycetes as endophytes; however only one form has been identified as a parasite. |
| نوع الوثيقة: | article in journal/newspaper |
| وصف الملف: | application/pdf |
| اللغة: | English |
| Relation: | Krings, M., Taylor, T., Dotzler, N. 2011. The fossil record of the Peronosporomycetes (Oomycota). Mycologia 103(3): 445-457.; http://hdl.handle.net/1808/13677 |
| DOI: | 10.3852/10-278 |
| الاتاحة: | http://hdl.handle.net/1808/13677 https://doi.org/10.3852/10-278 |
| Rights: | openAccess |
| رقم الانضمام: | edsbas.22F11280 |
| قاعدة البيانات: | BASE |
| DOI: | 10.3852/10-278 |
|---|