THALLUS: pale to bright lemon yellow to greenish-yellow, areolate crust, underlain by thin black prothallus visible around the margins and between areolae
APOTHECIA: black inset discose apothecia, often angular like areoles
SPORES: brown, muriform, 20-36 × 10-20 µm
CHEMISTRY: cortex UV+y (rhizocarpic acid major), medulla PD+ yellow (psoromic acid major), rarely C+ fleeting pink/red (gyrophoric acid in cortex? or medulla?)
Cosmopolitan.
Common Name: Golden Map Lichen
Bright lemon-yellow to greenish-yellow tiled crustose lichen growing over a thin unlichenized black prothallus on exposed granite and other siliceous rocks, especially in mountains.
Sunny, exposed, non-calcareous rocks, generally in mountains (1000-3720 m).
There are severa other yellow Rhizocarpon species:
R. macrosporum identical except for spore size (32-60 × 15-22 µm), less common R. lecanorinum also has brown muriform spores, crescent-shaped areoles around some apothecia, epihymenium K- or K+ green instead of K+ violet or purple others spores 2-celled and medulla K/I- in section (instead of blue)Some other genera that have yellow-and-black crustose thalli:
Acarospora apothecia brownish to yellowish, many spores per ascus, areoles often round or subsquamulose, rarely angular, no black prothallus Pleopsidium apothecia brownish to yellowish, areoles elongate into distinct short lobes at margin, no prothallus Dimelaena oreina very pale, distinctly radiating lobes at margin, apothecia not black Caloplaca yellow to orange, pigment K+ wine red, apothecia not black (in orange species) Candelina apothecia orange, distinctly lobate around margin, no prothallusCommonly used in lichenometry to date exposed rock surfaces.
Rhizocarpon geographicum (the map lichen) is a species of lichen, which grows on rocks in mountainous areas of low air pollution. Each lichen is a flat patch bordered by a black line of fungal hyphae. These patches grow adjacent to each other, leading to the appearance of a map or a patchwork field.
When circular, or roughly circular, the diameter of this lichen species has been widely used to help determining the relative age of deposits, e.g. moraine systems, thus revealing evidence of glacial advances. The process is termed lichenometry. This technique is generally attributed to the work of Roland Beschel in the Alps.[1]
Lichenometry is based on the assumption that the largest lichen growing on a rock is the oldest individual. Generally, the five largest lichen thalli diameters are taken, although several statistical methods have been used. If the growth rate is known, the maximum lichen size will give a minimum age for when this rock was deposited. The growth rate curve, a graph of age of a lichen against the date of the substrate on which it is found has to be constructed for an area. Beschel originally used gravestones to produce a calibration curve. Growth rates for different areas and species can be obtained by measuring maximum lichen sizes on substrates of known age, such as gravestones, historic or prehistoric rock buildings, or moraines of known age (e.g. those deposited during the Little Ice Age).
This lichen species is broadly distributed and may be found in most cold areas with exposed rock surfaces. The North American range includes the Sierra Nevada[2] and northern Boreal forests of Canada, Greenland, Iceland, Fennoscandia and Siberia.[3] In the tropics it only occurs at high altitudes such as the Andes of Peru and Colombia. Further south the map lichen is found broadly across Patagonia,[4][5] in the Falkland Islands, the sub Antarctic islands and the Antarctic Peninsula.[6]
In Britain it can be found commonly growing on hard siliceous rocks, especially in upland regions. Its range covers virtually all of Scotland, much of North West England, and other upland areas in much of the rest of England, Wales and Ireland too.[7]
In Spain it is found primarily in siliceous mountain ranges, although occasionally it can be found near sea level, even in southern Spain, where it is known from Cabo de Gata.[8]
Rhizocarpon geographicum is a known host to the lichenicolous fungus species Muellerella pygmaea.[9]
In an experiment, this lichen species was placed in a capsule and launched into space. The capsule was opened, exposing the lichen to space conditions for 10 days before being brought back down to Earth, where it showed minimal changes or damage.[10]
Media related to Rhizocarpon geographicum at Wikimedia CommonsRhizocarpon geographicum (the map lichen) is a species of lichen, which grows on rocks in mountainous areas of low air pollution. Each lichen is a flat patch bordered by a black line of fungal hyphae. These patches grow adjacent to each other, leading to the appearance of a map or a patchwork field.
When circular, or roughly circular, the diameter of this lichen species has been widely used to help determining the relative age of deposits, e.g. moraine systems, thus revealing evidence of glacial advances. The process is termed lichenometry. This technique is generally attributed to the work of Roland Beschel in the Alps.
Lichenometry is based on the assumption that the largest lichen growing on a rock is the oldest individual. Generally, the five largest lichen thalli diameters are taken, although several statistical methods have been used. If the growth rate is known, the maximum lichen size will give a minimum age for when this rock was deposited. The growth rate curve, a graph of age of a lichen against the date of the substrate on which it is found has to be constructed for an area. Beschel originally used gravestones to produce a calibration curve. Growth rates for different areas and species can be obtained by measuring maximum lichen sizes on substrates of known age, such as gravestones, historic or prehistoric rock buildings, or moraines of known age (e.g. those deposited during the Little Ice Age).
