by Elio
For the next four posts we'll cover the fungi in what we are calling »Fungomania«.
Figure 1. Devonian landscape, 417 − 354 million years ago. Source
"The fossil record of life's earliest steps onto land is profoundly incomplete." So starts a paper by Cambridge University's Martin Smith that helps shed light on this momentous happening. The climb ashore took place about 500 million years ago, give or take (no one seems to be quite sure of the date). These successful adventurers were plants, but still far from the highly-evolved plants we know today. They were small, simple in structure, and non-flowering. Not yet vascular plants, they were spore formers, possibly akin to the liverworts. On land, they faced the vicissitudes of novel and harsh environments. Their survival was probably helped by association with fungi, which could have pioneered on land to make the soil needed for plant growth. In time, symbioses like mycorrhizae were established. Anyhow, the earliest association of fungi and plants is revealed in fossils some 460 million-years-old. Keep in mind that fungi are much older than that.
Figure 2. When Fungi ruled the landscape. Credit: Mary Parrish, National Museum of Natural History.
An aside. Although not directly relevant to today's plant-fungus story, fungi have some interesting bragging rights. For some time, fungi managed to reign supreme on land. From approximately 420 to 350 million years ago (the Silurian-Devonian eras), the landscape was dominated by imposing rocket-like structures some 8 meters tall and 1 meter in diameter. Known as Prototaxites, these giants are thought to have been fungal in nature or maybe lichens, (although not everyone agrees).
Figure 3. Tortotubus from the Burgsvik Formation, Gotland, Sweden (SEM). Left: surface texture of Tortotubus closely resembles surface texture of hyphae in Leccinum scabrum (a basidiomycete mushroom on the right. Source.
But back to fungi and terrestrial plants. Smith reports that a fungus by the evocative name of Tortotubus protuberans is found in some manageable fossil rocks from the Silurian-Devonian. This makes them the oldest fossils of land creatures. This fungus' morphological features are striking: the fungal filaments show perforations in the septa, bilateral cell walls, and intertwined hyphae in the shape of cords. Smith concludes: "This morphology and pattern of growth together indicate an affinity with the ‘higher’ fungi (Dikarya) and document the formation of differentiated mycelium. The presence of complex mycelial fossils in the earliest Silurian corroborates the likely contribution of fungi to the colonization of land and the establishment of modern sedimentological systems; their rise seemingly accompanied the diversification of early embryophytes and the vegetation of the terrestrial biosphere".
Figure 4. Development of cords in T. protuberans. Presumed growth direction to top of page. A Simple filament, with nascent secondary branches near base of primary branches. B secondary branch growing towards main filament; C secondary branch commencing retrograde growth alongside main filament. Source.
Morphological comparisons are in order: "The pattern of growth in Tortotubus finds a vivid analogue among mushroom-forming members of Basidiomycota and Ascomycota that produce coherent threads of entwined hyphae–termed mycelial cords, mycelial strands or syrrotia".
But here's a question: what did these pioneer fungi use for food? Being saprophytes, and plant material not being available, they must have lived off other consumable organisms. Photosynthetic bacteria come to mind and, if not them, then other organisms that lived off them.
The implications of these findings are tantalizing. Fungal mycelia may have played a key role in stabilizing the soil, which would have been important for plants, being that early on they lacked roots. In other words, fungi may have been responsible for the earliest stage of agriculture, that is, making the ground suitable for plants to grow. Now you know why we indulge in Fungomania in these pages.
Front page: 440 million years old fossil of Tortotubus protuberans from Gotland, Sweden, showing stages in development of filamentous envelope. Image credit: Martin R. Smith. Source
Comments