Marlin L. Bowles, John V. Freudenstein, Judy Hall Jacobson
Madroño 68 (2), 75-86, (17 September 2021) https://doi.org/10.3120/0024-9637-68.2.75
KEYWORDS: Alaska, climate relic, Corallorhiza maculata, Corallorhiza mertensiana, field and herbarium records, morphology, migration, rain shadow, Xerothermic Hypsithermic interval
In the Pacific Northwest, the spotted coralroot, Corallorhiza maculata (Raf.) Raf., has been recognized as occurring as far north as central British Columbia, but excluded from the flora of Alaska. The western coralroot, C. mertensiana Bong., reaches its northern range limit in Southeast Alaska, where collections of this sister species may be confused with C. maculata. In 2019-20, we conducted herbarium and field studies that verified eight C. maculata stations in northern Southeast Alaska. Two of these stations are represented by collections made in 2000 and 2007, which were identified as C. mertensiana; 14 C. mertensiana collections had been identified as C. maculata. This confusion may have resulted from nomenclatural changes, as well as rarity of actual C. maculata material. These species differ in morphological features that reflect different breeding systems, and occupy different habitats in Alaska. The Alaska stations of C. maculata represent a 650 km range extension that is disjunct from locations in central British Columbia. These stations occur in a summer-dry climate zone caused by a rainshadow from coastal mountains. We advance the hypothesis that this area provides habitat for populations of C. maculata that represent relics of a floristic migration that occurred during the Xerothermic interval 10-7500 yr BP. In contrast, C. mertensiana is widespread in humid coastal habitats in southeast Alaska, and its distribution is contiguous with more southern coastal populations. Though both species occur in Southeast Alaska, they occupy different climate zones, and their distributions are narrowly allopatric.