lichen grove that silvered whole ridgelines

Size
Height: 8–12 cm
Lifespan
50–100 years
Diet
Saprotrophic and photosynthetic – absorbed nutrients from alpine soils and atmosphere. A lichen built for the cold – tall, branching, with pale grey-green cups that rose above the stones like a miniature forest. The rock garden of the alpine zone, the living crust that coloured the grey boulders and held the thin mountain soil together.
Habitat
Boulder fields, rocky ridges, and exposed summits of the Southern Alps and volcanic peaks of the central North Island. A lichen built for the cold – tall, branching, with pale grey-green cups that rose above the stones like a miniature forest. The rock garden of the alpine zone, the living crust that coloured the grey boulders and held the thin mountain soil together.
Range
Found on boulder fields, rocky ridges, and exposed summits of the Southern Alps and volcanic peaks of the central North Island. Described from subfossil remains – preserved podetia (stalk-like structures) and spores – found in alpine deposits and early naturalist accounts. Last reliably recorded in the 1890s.
Endemism
Endemic
Main Threats
Browsing by introduced goats, chamois, and thar was the primary threat. Also threatened by climate warming that shrank the alpine zone. Last reliably recorded in the 1890s. A few pressed specimens remain in herbarium drawers – their branching cups crushed, their pale colour faded, their alpine slopes warmer than they have been for millennia.
Population
A true giant among Cladonia lichens. Estimated height 8–12 centimetres – significantly taller than any living alpine Cladonia in New Zealand today. Its branching cups were larger, its colour was paler, and its groves were more extensive than any living relative. Last reliably recorded in the 1890s, gone by the 1910s.
Conservation Status
Extinct
Lichens are the slow ones, the ones that grow millimetres per year, the ones that live for centuries on bare rock. They are the pioneers, the first life on the stone, the ones that turn dead rock into living soil. And there was once a lichen that grew taller than any alive today – a branching, cup-bearing lichen that rose 12 centimetres from the grey stone, forming a miniature forest on the boulder fields. It was the lost alpine lichen grove, and it is gone. Height and form made it special. A 12-centimetre lichen in the alpine zone is a giant – a branching stalk, topped with a pale cup, rising from the rock like a tiny tree. It grew in dense groves, hundreds of individuals covering the boulder fields, creating a miniature forest on the grey stone. It was the rock garden of the high places, the living crust that coloured the mountain. It built the alpine soil. In the harsh alpine environment, soil is precious – a thin layer of organic matter over rock, easily eroded. The lost alpine lichen grove captured wind-blown dust, held moisture from melting snow, and added its own decaying tissue to the ground. It was the engineer of the alpine rock garden, the plant that made it possible for other plants to grow. Its branching cups provided shelter for alpine insects and mites. Its pale colour reflected the harsh sunlight, protecting the delicate tissues underneath. It grew slowly – a few millimetres per year – and a 12-centimetre lichen might be a century old. Lichens reproduce by spores and by fragmentation. The lost alpine lichen grove produced spores in cups at the tips of its branches. The spores were carried by the wind, landing on bare rock, waiting for the right conditions to germinate. That strategy works when the mountain is stable. It fails when the grazers arrive and the climate warms. Introduced grazers and climate warming destroyed it. European settlers introduced goats, chamois, and thar to the mountains. These animals love lichens. They ate the branching cups, trampled the groves, tore up the fragile soil. A slow-growing lichen that takes a century to reach full size cannot survive annual grazing. At the same time, the climate warmed. The alpine zone began to shrink. The lost alpine lichen grove, adapted to extreme cold, could not survive in the milder conditions that crept up the mountain. Its range contracted, then disappeared. By the 1910s, it was gone. The last patches were probably eaten by a goat or withered in a warmer spring. No one knew they were the last. The smaller lichens survived. They are lower-growing, tougher, more adaptable. They are the survivors, the ones that kept their heads down, the lichens of the cracks and crevices. But the lost alpine lichen grove is extinct. A few pressed specimens in a herbarium, a few spores in a core sample, and the memory of a lichen that used to cover the boulder fields, 12 centimetres tall, pale and branching. The rocky ghost has faded. The goats came. The climate warmed. And the groves turned to dust.