Liverworts of the South Kamchatka Nature Park: Survival in Active Volcanism Land

• Published in: Diversity
• Main Authors: Vadim A. Bakalin, Ksenia G. Klimova, Eugeniy A. Karpov, Daniil A. Bakalin, Seung Se Choi
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2022
• Subjects: liverworts; Kamchatka Peninsula; Northeast Asia; Pacific Ring of Fire; distribution patterns; nonvascular plants; Biology (General); QH301-705.5; Pacific; Kamchatka
• Online Access: https://doi.org/10.3390/d14090722; https://doaj.org/article/ef03cde64b5241abb76178a3c7feebf0

Kamchatka, due to its position in hemiarctic northeast Asia on the migration pathways of taxa from Asia to America and vice versa, which has an insular geographical position and provides numerous pieces of evidence regarding current active volcanism, has a peculiar flora. The study of the liverwort flora of the southeastern part of the Kamchatka Peninsula (South Kamchatka Nature Park), which, until now, has been very poorly explored, showed high taxonomic richness and some specificity due to volcanic evidence. In total, 132 species have been recorded in this sector of the “Pacific Ring of Fire”. This number is quite high compared to other floras of hemiarctic Asia. The influence of volcanism on flora formation is prominent due to the regular renewal of substrates, the appearance of specific habitats (for example, thermal water outlets), the displacement of vegetation belts, and ashfalls leading to the presence of extended spaces free of vegetation cover and is an area that is open for invaders. The altitudinal zonality, despite the difference of 2000 m in elevation, is not clearly expressed in the flora of the liverworts: arctomontane species descend far down the altitudinal profile, reaching the Betula ermanii forests. The “plantless” uppermost belt in the mountains, commonly described in floristic studies of vascular plants, is not actually free of plants if liverwort occurrences are considered. A number of species normally occupy unusual habitats in the studied flora due to contemporary volcanism evidence, e.g., sulfur-rich substrates.