Abstract
Permineralized peat from the central Transantarctic Mountains of Antarctica has provided a wealth of information on plant and fungal diversity in Middle Triassic high-latitude forest paleoecosystems;however, there are no reports as yet of algae or cyanobacteria. The first record of a fossil filamentous cyanobacterium in this peat consists of wide, uniseriate trichomes composed of discoid cells up to 25 mu m wide, and enveloped in a distinct sheath. Filament morphology, structurally preserved by permineralization and mineral replacement., corresponds to the fossil genus Palaeolyngbya, a predominantly Precambrian equivalent of the extant Lyngbya sensu lato (Oscillatoriaceae, Oscillatoriales). Specimens occur exclusively in masses of interwoven hyphae produced by the fungus Endochaetophora antarctica, suggesting that a special micro-environmental setting was required to preserve the filaments. Whether some form of symbiotic relationship existed between the fungus and cyanobacterium remains unknown.
Dokumententyp: | Zeitschriftenartikel |
---|---|
Fakultät: | Geowissenschaften > Department für Geo- und Umweltwissenschaften |
Themengebiete: | 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie |
ISSN: | 2167-8359 |
Sprache: | Englisch |
Dokumenten ID: | 90624 |
Datum der Veröffentlichung auf Open Access LMU: | 25. Jan. 2022, 09:36 |
Letzte Änderungen: | 25. Jan. 2022, 09:36 |